79 results on '"Batista, M. J."'
Search Results
2. Olive-Oil Waste for the Removal of Heavy Metals from Wastewater
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Martín-Lara, M. A., Muñoz-Batista, M. J., Blázquez, G., Pérez, A., Calero, M., Lichtfouse, Eric, Series Editor, Schwarzbauer, Jan, Series Editor, Robert, Didier, Series Editor, Inamuddin, editor, Ahamed, Mohd Imran, editor, and Altalhi, Tariq, editor
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- 2021
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3. Olive-Oil Waste for the Removal of Heavy Metals from Wastewater
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Martín-Lara, M. A., primary, Muñoz-Batista, M. J., additional, Blázquez, G., additional, Pérez, A., additional, and Calero, M., additional
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- 2021
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4. Introduction and Geological Setting of the Iberian Pyrite Belt
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Inverno, C., Díez-Montes, A., Rosa, C., García-Crespo, J., Matos, J., García-Lobón, J. L., Carvalho, J., Bellido, F., Castello-Branco, J. M., Ayala, C., Batista, M. J., Rubio, F., Granado, I., Tornos, F., Oliveira, J. T., Rey, C., Araújo, Vítor, Sánchez-García, T., Pereira, Z., Represas, P., Solá, A. R., Sousa, P., Slack, John, Series editor, and Weihed, Pär, editor
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- 2015
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5. Modelling of the Neves Corvo Area
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Inverno, C., Rosa, C., Matos, J., Carvalho, J., Castello-Branco, J. M., Batista, M. J., Granado, I., Oliveira, J. T., Araújo, V., Pereira, Z., Represas, P., Solá, A. R., Sousa, P., Slack, John, Series editor, and Weihed, Pär, editor
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- 2015
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6. Uranium distribution and mobility in the weathering zone of the Nisa deposit, Portugal
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Prazeres, C. M., Batista, M. J., Pinto, A. J., and Gonçalves, M. A.
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- 2018
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7. Time-space evolution of Iberian Pyrite Belt igneous activity: volcanic and plutonic lineaments, geochronology, ore horizons and stratigraphic constraints
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European Commission, Laboratório Nacional de Energia e Geologia (Portugal), Albardeiro, Luís [0000-0002-3826-260X], Pereira, Z. [0000-0003-3056-6219], Mendes, Márcia [0000-0003-2290-891X], Díez Montes, Alejandro [0000-0003-3215-9174], Inverno, C. [0000-0002-0806-5330], Albardeiro, Luís, Morais, I., Matos, J. X., Sola, Rita, Salgueiro, R., Pereira, Z., Mendes, Márcia, Batista, M. J., Oliveira, D. de, Díez Montes, Alejandro, Inverno, C., Pacheco, Nelson, Araújo, Vítor, European Commission, Laboratório Nacional de Energia e Geologia (Portugal), Albardeiro, Luís [0000-0002-3826-260X], Pereira, Z. [0000-0003-3056-6219], Mendes, Márcia [0000-0003-2290-891X], Díez Montes, Alejandro [0000-0003-3215-9174], Inverno, C. [0000-0002-0806-5330], Albardeiro, Luís, Morais, I., Matos, J. X., Sola, Rita, Salgueiro, R., Pereira, Z., Mendes, Márcia, Batista, M. J., Oliveira, D. de, Díez Montes, Alejandro, Inverno, C., Pacheco, Nelson, and Araújo, Vítor
- Abstract
[EN] The volcanism in the Iberian Pyrite Belt migrated from the present day west/southwest to the east/northeast during Devonian/Carboniferous times. Evidence is here discussed based in U-Pb zircon ages of felsic volcanic and plutonic rocks, bounded by enclosed sediments and their biostratigraphic ages, together with hosted massive sulphides deposits and associated plutonic counterparts. Volcano-Sedimentary Complex rocks define several volcanic axes, or lineaments, with the general NW-SE to WNW-ESE belt trending orientation. The usage of all the available data from high-resolution stratigraphy, geology and geophysics lead to establishment of eleven main volcanic axes, nine with zircon U-Pb radiometric ages (166 samples). In this research, we reinforce a previous inter-axes volcanic evolutionary trend, but we also suggest an intra-axis evolutionary trend of the IPB igneous activity with time. This means the basin igneous activity also evolved along most of the volcanic and plutonic lineaments, from west/northwest to east/southeast. Successive weighted average ages for each axis (SW to NE) and opposite end-point sample ages for each axis (NW/W to SE/E) are presented. Similar trends are found with felsic volcanic rocks, subvolcanic and plutonic rocks and even massive sulphide ages correspond to the regional trend corroborating the proposed geological framework. Siliciclastic sediments and lower VSC sequences (sediments, felsic volcanic rocks and massive sulphides) show a comparable age trending evolution although upper VSC sediments seem to be contemporaneous across the province. Older ages, from zircon U-Pb and from associated reworked palynomorph in the sediments, show a long-lasting age distribution along most Devonian times, suggesting the IPB evolved since Lochkovian times (Lower Devonian). Therefore, we propose the IPB inter-axes evolution could be related with a NE-direction plate motion (present-day location) over a heat source, while intra-axes are probably du
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- 2023
8. Manual de metodologías geoquímicas de países iberoamericanos : información geoquímica para la sociedad
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Batista, M. J., Prieto Rincón, Gloria, Turel, Andrea, Martín Méndez, Iván, Pérez, Adrián, Asociación de Servicios de Geología y Minería Iberoamericanos, Batista, M. J., Prieto Rincón, Gloria, Turel, Andrea, Martín Méndez, Iván, Pérez, Adrián, and Asociación de Servicios de Geología y Minería Iberoamericanos
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- 2023
9. Mineral resources and geochemical exploration in PLANAGEO (Angola)
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Martín Méndez, Iván, Feria Martín, María del Carmen, Batista, M. J., Merino Martínez, E., Prazeres, Cátia, Martín Méndez, Iván, Feria Martín, María del Carmen, Batista, M. J., Merino Martínez, E., and Prazeres, Cátia
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[EN] PLANAGEO is an international Project developed by the Spanish Geological Survey (IGME), Portugal Geological Survey (LNEG) and Asturian company (IMPULSO) for 8 years (2014-2022) in the south part of Angola (476.500 Km2). This project has four main activities: 1) Aerogeophysical surveys, 2) Geological mapping, 3) Geochemical exploration and 4) Specific studies (Mineral resources exploration, hydrogeological studies and ornamental rock and industrial mineral exploration).
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- 2022
10. Identification of the co-existence of low total organic carbon contents and low pH values in agricultural soil in north-central Europe using hot spot analysis based on GEMAS project data
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Xu, Haofan, Demetriades, Alecos, Reimann, Clemens, Jimenez, Juan J., Filser, Juliane, Zhang, Chaosheng, Albanese, S., Andersson, M., Baritz, R., Batista, M. J., Bel-lan, A., Birke, M., Cicchella, D., De Vivo, B., De Vos, W., Dinelli, E., Duris, M., Dusza-Dobek, A., Eklund, M., Ernstsen, V, Filzmoser, P., Flem, B., Flight, D. M. A., Forrester, S., Fuchs, M., Fugedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V, De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kirby, J., Klos, V, Krone, F., Kwecko, P., Kuti, L., Ladenberger, A., Lima, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., McLaughlin, M., Malyuk, B., I, Maquil, R., Matschullat, J., Meuli, R. G., Mol, G., Negrel, P., O'Connor, P., Oorts, K., Pasieczna, A., Petersell, V, Pfleiderer, S., Ponavic, M., Prazeres, C., Rauch, U., Radusinovic, S., Sadeghi, M., Salpeteur, I, Scanlon, R., Schedl, A., Scheib, A., Schoeters, I, Sellersjo, E., Slaninka, I, Soriano-Disla, J. M., Sorsa, A., Svrkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V, Valera, P., Verougstraete, V., Vidojevi, D., Zissimos, A., Zomeni, Z., Xu H., Demetriades A., Reimann C., Jimenez J.J., Filser J., Zhang C., GEMAS Project Team: Albanese S., Andersson M., Baritz R., Batista M.J., Bel-lan A., Birke M., Cicchella D., De Vivo B., De Vos W., Dinelli E., Ďuriš M., Dusza-Dobek A., Eklund M., Ernstsen V., Filzmoser P., Flem B., Flight D.M.A., Forrester S., Fuchs M., Fügedi U., Gilucis A., Gosar M., Gregorauskiene V., De Groot W., Gulan A., Halamić J., Haslinger E., Hayoz P., Hoffmann R., Hoogewerff J., Hrvatovic H., Husnjak S., Janik L., Jordan G., Kirby J., Klos V., Krone F., Kwecko P., Kuti L., Ladenberger A., Lima A., Locutura J., Lucivjansky P., Mann A., Mackovych D., McLaughlin M., Malyuk B.I., Maquil R., Matschullat J., Meuli R.G., Mol G., Négrel P., O'Connor P., Oorts K., Pasieczna A., Petersell V., Pfleiderer S., Poňavič M., Prazeres C., Rauch U., Radusinović S., Sadeghi M., Salpeteur I., Scanlon R., Schedl A., Scheib A., Schoeters I., Sellersjö E., Slaninka I., Soriano-Disla J.M., Šorša A., Svrkota R., Stafilov T., Tarvainen T., Trendavilov V., Valera P., Verougstraete V., Vidojević D., Zissimos A., Zomeni Z., Haofan, Xu, Alecos, Demetriade, Clemens, Reimann, Juan J, Jiménez, Juliane, Filser, Chaosheng, Zhang, Albanese, S., Andersson, M., Baritz, R., Batista, M. J., Bel-lan, A., Birke, M., Cicchella, D., De Vivo, B., De Vos, W., Dinelli, E., Ďuriš, M., Dusza-Dobek, A., Eklund, M., Ernstsen, V., Filzmoser, P., Flem, B., Flight, D. M. A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kirby, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Ladenberger, A., Lima, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Matschullat, J., Meuli, R. G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Pasieczna, A., Petersell, V., Pfleiderer, S., Poňavič, M., Prazeres, C., Rauch, U., Radusinović, S., Sadeghi, M., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sellersjö, E., Slaninka, I., Soriano-Disla, J. M., Šorša, A., Svrkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojević, D., Zissimos, A., and Zomeni, Z.
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Pollution ,Environmental Engineering ,010504 meteorology & atmospheric sciences ,Hot spot analysis ,Hot spot analysi ,media_common.quotation_subject ,Hot spot (veterinary medicine) ,010501 environmental sciences ,01 natural sciences ,GEMAS ,chemistry.chemical_compound ,Environmental Chemistry ,European agricultural soil ,TOC ,pH ,Waste Management and Disposal ,0105 earth and related environmental sciences ,media_common ,Total organic carbon ,North central ,business.industry ,chemistry ,Agriculture ,Environmental chemistry ,Carbon dioxide ,Spatial ecology ,Environmental science ,Soil fertility ,business - Abstract
Total organic carbon (TOC) contents in agricultural soil are presently receiving increased attention, not only because of their relationship to soil fertility, but also due to the sequestration of organic carbon in soil to reduce carbon dioxide emissions. In this research, the spatial patterns of TOC and its relationship with pH at the European scale were studied using hot spot analysis based on the agricultural soil results of the Geochemical Mapping of Agricultural Soil (GEMAS) project. The hot and cold spot maps revealed the overall spatial patterns showing a negative correlation between TOC contents and pH values in European agricultural soil. High TOC contents accompanying low pH values in the north-eastern part of Europe (e.g., Fennoscandia), and low TOC with high pH values in the southern part (e.g., Spain. Italy, Balkan countries). A special feature of co-existence of comparatively low TOC contents and low pH values in north-central Europe was also identified on hot and cold spot analysis maps. It has been found that these patterns are strongly related to the high concentration of SiO2 (quartz) in the coarse-textured glacial sediments in north-central Europe. The hot spot analysis was effective, therefore, in highlighting the spatial patterns of TOC in European agricultural soil and helpful to identify hidden patterns. (C) 2019 Elsevier B.V. All rights reserved.
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- 2019
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11. Multispectral and hyperspectral remote sensing as a source of knowledge in the Portuguese sector of the Iberian Pyrite Belt
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de Oliveira, D., Batista, M. J., Matos, J. X., Sousa, A. J., Marsh, S., Carreiras, J., and Dias, R.
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Multispectral, Hyperspectral, Portuguese sector of the Iberian Pyrite Belt (PSIPB), Multi-source data, Spectral information - Abstract
Remote sensing is an invaluable tool to increase geological and mining knowledge, due to its screening view and variable discrimination and identification capabilities of the target materials. In this study an overview of remote sensing research developed and ongoing within the Portuguese sector of the Iberian Pyrite Belt (PSIPB) since 2000 is given. Multispectral and hyperspectral datasets were processed using hybrid methods, related both to general and detailed characterization, to: 1) support geological, mineral and hydrothermal mapping, 2) generate products derived from multivariate analysis and band ratios, 3) enhance correlation with radiometric data, 4) provide elements for environmental assessment concerning mining activity, 5) map Acid Mine Drainage (AMD) based on spectral field signatures, 6) quantify AMD based on high correlation mineralogical mapping, and 7) monitor AMD. The results highlight the importance of the quantitative digital support given by remote sensing tools within the Portuguese Sector of the Iberian Pyrite Belt (PSIPB), ruled by georesource exploitation in different stages of the Mine Lyfe Cycle.RESUMO: A deteção remota é uma ferramenta valiosa para aumentar o conhecimento geológico e mineiro, devido à visão sinótica e à capacidade variável de discriminação e identificação dos materiais-alvo. Neste trabalho dá-se uma visão geral da investigação através dos trabalhos de deteção remota desenvolvidos e em curso no Setor Português da Faixa Piritosa Ibérica (SPFPI) desde 2000. Os dados multiespectrais e hiperespectrais foram processados usando métodos híbridos quer para a sua caracterização geral quer detalhada para: 1) apoiar a cartografia geológica, de mineralizações e sistemas hidrotermais, 2) gerar produtos de análise multivariada e rácios de bandas, 3) melhorar a correlação com dados radiométricos 4) fornecer elementos para avaliação ambiental em áreas mineiras, 5) cartografar a drenagem ácida de mina (DAM) com assinaturas espectrais de campo, 6) quantificar a DAM através de cartografia mineralógica de alta correlação, e 7) monitorizar a DAM. Destaca-se a importância do suporte digital quantitativo dado por ferramentas de deteção remota no SPFPI, regido pela exploração de georrecursos em diferentes fases do Ciclo de Vida das Minas.
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- 2020
12. Use of GEMAS data for risk assessment of cadmium in European agricultural and grazing land soil under the REACH Regulation
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Birke, M., Reimann, C., Oorts, K., Uwe, R., Alecos, D., Dinelli, E., Ladenberger, A., Halamić, J., Mateja, G., Jähne Klingberg, F., Andersson, M., Baritz, R., Batista, M. J., Bel Ian, A., Cicchella, D., De Vos, W., Duris, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernsten, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fügedi, U., Gilcucis, A., Gregorauskiene, V., De Groot, W., Gulan, A., Haslinger, E., Hayoz, P., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Kwecko, P., Kuti, L., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Negrel, P., ’Connor, P. O, Ottesen, R. T., Pasnieczna, A., Petersell, V., Pfleiderer, S., Ponavi c, M., Prazeres, C., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sefcik, P., Sellersjo, E., Slaninka, I., Soriano Disla, J. M., Sorsa, A., Svrkota, R., Stafilov, T., Tarvainen, T., Tendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zomeni, Z., Zissimos, A., ALBANESE, STEFANO, DE VIVO, BENEDETTO, LIMA, ANNAMARIA, Birke, M., Reimann, C., Oorts, K., Uwe, R., Alecos, D., Dinelli, E., Ladenberger, A., Halamić, J., Mateja, G., Jähne Klingberg, F., Albanese, Stefano, Andersson, M., Baritz, R., Batista, M. J., Bel Ian, A., Cicchella, D., DE VIVO, Benedetto, De Vos, W., Duris, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernsten, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fügedi, U., Gilcucis, A., Gregorauskiene, V., De Groot, W., Gulan, A., Haslinger, E., Hayoz, P., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Kwecko, P., Kuti, L., Lima, Annamaria, Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Negrel, P., ’Connor, P. O, Ottesen, R. T., Pasnieczna, A., Petersell, V., Pfleiderer, S., Ponavi c, M., Prazeres, C., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sefcik, P., Sellersjo, E., Slaninka, I., Soriano Disla, J. M., Sorsa, A., Svrkota, R., Stafilov, T., Tarvainen, T., Tendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zomeni, Z., Zissimos, A., Birke, Manfred, Reimann, Clemen, Oorts, Koen, Rauch, Uwe, Demetriades, Aleco, Dinelli, Enrico, Ladenberger, Anna, Halamić, Josip, Gosar, Mateja, and Jähne-Klingberg, Fabian
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Pollution ,agricultural soil ,grazing land soil ,risk assessment ,REACH ,cadmium ,Soil test ,media_common.quotation_subject ,chemistry.chemical_element ,010501 environmental sciences ,010502 geochemistry & geophysics ,Agricultural soil ,01 natural sciences ,Ecology and Environment ,Geochemistry and Petrology ,Grazing ,Environmental Chemistry ,Risk assessment ,0105 earth and related environmental sciences ,media_common ,Hydrology ,Cadmium ,business.industry ,Forestry ,Expert group ,Chemistry ,chemistry ,Agriculture ,Soil water ,Earth Sciences ,business ,Grazing land soil - Abstract
Over 4000 soil samples were collected for the “Geochemical Mapping of Agricultural and Grazing Land Soil of Europe” (GEMAS) project carried out by the EuroGeoSurveys Geochemistry Expert Group. Cadmium concentrations are reported for the
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- 2016
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13. Health literacy and associated factors in patients with chronic diseases, Brazil
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Tenani, C F, primary, Sousa, M L R, additional, and Batista, M J, additional
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- 2020
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14. GEMAS: Cobalt, Cr, Cu and Ni distribution in agricultural and grazing land soil of Europe
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ALBANESE, STEFANO, LIMA, ANNAMARIA, DE VIVO, BENEDETTO, Sadeghi, M., Cicchella, D., Dinelli, E., Valera, P., Falconi, M., Demetriades, A., Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Birke, M., De Vos, W., Ďuriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Ladenberger, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Ottesen, R. T., Pasieczna, A., Petersell, V., Pfleiderer, S., Poňavič, M., Prazeres, C., Rauch, U., Radusinović, S., Reimann, C., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sellersjö, E., Slaninka, I., Soriano Disla, J. M., Šorša, A., Svrkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Verougstraete, V., Vidojević, D., Zomeni, Z., Albanese, Stefano, Sadeghi, M., Lima, Annamaria, Cicchella, D., Dinelli, E., Valera, P., Falconi, M., Demetriades, A., DE VIVO, Benedetto, Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Birke, M., De Vos, W., Ďuriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Ladenberger, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Ottesen, R. T., Pasieczna, A., Petersell, V., Pfleiderer, S., Poňavič, M., Prazeres, C., Rauch, U., Radusinović, S., Reimann, C., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sellersjö, E., Slaninka, I., Soriano Disla, J. M., Šorša, A., Svrkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Verougstraete, V., Vidojević, D., Zomeni, Z., Albanese, S., Lima, A., De Vivo, B., Batista, M.J., Bel-lan, A., Duris, M., Dusza-Dobek, A., Eggen, O.A., Flight, D.M.A., Fugedi, U., Halamic, J., Malyuk, B.I., Meuli, R.G., Negrel, P., Ottesen, R.T., Ponavic, M., Radusinovic, S., Sellersjo, E., Soriano-Disla, J.M., Sorsa, A., and Vidojevic, D.
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Mediterranean climate ,Soil test ,Metal ,Mafic-ultramafic rocks ,Soil guidelines ,Earth science ,European soil ,Mineralogy ,cobalt ,crom ,distribution ,Ni ,Cu ,Ophiolite ,Metals ,Geochemistry and Petrology ,Ultramafic rock ,Grazing ,Geochemical mapping ,Economic Geology ,Glacial period ,Mafic ,European soil Mafic–ultramafic rocks Metals Geochemical mapping Soil guidelines ,Scale (map) ,Geology ,Mafic-ultramafic rock - Abstract
In the framework of the GEMAS project, 2211 samples of agricultural soil (Ap, 0-20cm, regularly ploughed fields), and 2118 samples from land under permanent grass cover (Gr, 0-10cm, grazing land soil) were collected across almost the whole European continent, at a density of 1 sample site/2500km2, in accordance with a common sampling protocol.Among many other elements, the concentrations of Co, Cr, Cu and Ni in European soil were determined by ICP-MS after a hot aqua extraction, and WD-XRFS analytical methods, and their spatial distribution patterns generated by means of a GIS software.The presence of mafic and ultramafic rocks, ophiolite complexes and mineralisation, is widespread across the European continent, and seems to explain most of the variability of the elements studied in this paper. A large belt, north of the last glaciation maximum limit, is generally dominated by lower concentrations compared with central European and Mediterranean areas and to some areas in Northern Europe where higher Co, Cr, Cu and Ni values also occur.The application of the guideline value set for Cu and Ni by the EU Directive 86/278/EEC to the Ap soil samples of the GEMAS data set highlighted that at the continental scale the use of a unique reference interval is a tool of limited effectiveness; the lithological variation, occurring across a whole continent, generates changes in the geochemistry of soil, which cannot be accommodated by using a single reference interval even if it is very wide. The GEMAS data set should form the sound basis to set at the European scale the geochemical background reference intervals, at least, for regions sharing common lithological settings and a common geological history. •Geochemistry of Co, Cr, Cu and Ni•Mineral deposits in Europe with Co, Cr, Cu and Ni•Distribution of Co, Cr, Cu and Ni in European agricultural and grazing land soil•Comparison of aqua regia extractable and total element concentrations in soil•Comparison of Cu and Ni concentrations with European guideline values. © 2015 Elsevier B.V.
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- 2015
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15. Bioavailable 87Sr/86Sr in European soils:A baseline for provenancing studies
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Hoogewerff, Jurian A., Reimann, Clemens, Ueckermann, Enriette, Frei, Robert, Frei, Karin M., van Aswegen, Thalita, Stirling, Claudine, Reid, Malcolm, Clayton, Aaron, Ladenberger, Anna, Albanese, S., Andersson, M., Baritz, R., Batista, M. J., Bel-Ian, A., Birke, M., Cicchella, D., Demetriades, A., De Vivo, B., De Vos, W., Dinelli, E., Duris, M., Dusza-Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fugedi, U., Gilucis, A., Gregorauskiene, V, De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V, Krone, F., Kwecko, F., Kuti, L., Lima, A., Locutura, J., Lucivjansky, D. P., Mann, A., Mackovych, D., Matschullat, J., McLaughlin, M., Malyuk, B., I, Maquil, R., Meuli, R. G., Mol, G., Negrel, P., Connor, O., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Ponavic, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinovic, S., Reimann, C., Sadeghi, M., Salpeteur, I, Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I, Sefcik, P., Sellersjo, E., Skopijak, F., Slaninka, I, Soriano-Disla, J. M., Sorsa, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V, Valera, P., Verougstraete, V., Vidojevic, D., Zissimos, A., Zomeni, Z., Hoogewerff, Jurian A., Reimann, Clemens, Ueckermann, Enriette, Frei, Robert, Frei, Karin M., van Aswegen, Thalita, Stirling, Claudine, Reid, Malcolm, Clayton, Aaron, Ladenberger, Anna, Albanese, S., Andersson, M., Baritz, R., Batista, M. J., Bel-Ian, A., Birke, M., Cicchella, D., Demetriades, A., De Vivo, B., De Vos, W., Dinelli, E., Duris, M., Dusza-Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fugedi, U., Gilucis, A., Gregorauskiene, V, De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V, Krone, F., Kwecko, F., Kuti, L., Lima, A., Locutura, J., Lucivjansky, D. P., Mann, A., Mackovych, D., Matschullat, J., McLaughlin, M., Malyuk, B., I, Maquil, R., Meuli, R. G., Mol, G., Negrel, P., Connor, O., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Ponavic, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinovic, S., Reimann, C., Sadeghi, M., Salpeteur, I, Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I, Sefcik, P., Sellersjo, E., Skopijak, F., Slaninka, I, Soriano-Disla, J. M., Sorsa, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V, Valera, P., Verougstraete, V., Vidojevic, D., Zissimos, A., and Zomeni, Z.
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- 2019
16. GEMAS: Cadmium distribution and its sources in agricultural and grazing land soil of Europe - Original data versus clr-transformed data
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BIRKE M., REIMANN C, RAUCH U., LADENBERGER A., DEMETRIADES A., JÄHNEKLINGBERG F., OORTS K, GOSAR M., DINELLI D., HALAMIĆ J., ALBANESE S., ANDERSSON M., BARITZ R., BATISTA M. J., BEL-IAN A., CICCHELLA D., DE VIVO B., DE VOS W., ĎURIŠ M., DUSZA-DOBEK A., EGGEN O. A., EKLUND M., ERNSTEN V., FILZMOSER, FLIGHT D. M. A., FORRESTER S., FÜGEDI U., GILCUCIS A., GREGORAUSKIENE V., DE GROOT W., GULAN A., HASLINGER E., HAYOZ P., HOOGEWERFF J., HRVATOVIC H., HUSNJAK S., JANIK L., JORDAN G., KAMINARI M., KIRBY J., KLOS V., KWEĆKO P., KUTI L., LIMA A., LOCUTURA J., LUCIVJANSKY P., MANN A., MACKOVYCH D., MCLAUGHLIN M., MALYUK B. I., MAQUIL R., MEULI R. G., MOL G., NÉGREL P., O’CONNOR P., OTTESEN R. T., PASNIECZNA A., PETERSELL V., PFLEIDERER S., POŇAVIČ M., PRAZERES C., RADUSINOVIĆ S., SALPETEUR I., SADEGHI M., SCANLON R., SCHEDL A., SCHEIB A., SCHOETERS I., ŠEFČIK P., SELLERSJÖ E., SLANINKA I., SORIANO-DISLA J. M., ŠORŠA A., SVRKOTA R., STAFILOV T., TARVAINEN T., TENDAVILOV V., VALERA P., VEROUGSTRAETE V., VIDOJEVIĆ D., ZOMENI Z., ZISSIMOS A., Birke, Manfred, Reimann, Clemen, Rauch, Uwe, Ladenberger, Anna, Demetriades, Aleco, Jähne-Klingberg, Fabian, Oorts, Koen, Gosar, Mateja, Dinelli, Enrico, Halamić, Josip, Birke, M., Reimann, C, Rauch, U., Ladenberger, A., Demetriades, A., Jähneklingberg, F., Oorts, K, Gosar, M., Dinelli, D., Halamić, J., Albanese, S., Andersson, M., Baritz, R., Batista, M. J., BEL-IAN, A., Cicchella, D., DE VIVO, B., DE VOS, W., Ďuriš, M., DUSZA-DOBEK, A., Eggen, O. A., Eklund, M., Ernsten, V., Filzmoser, Flight, D. M. A., Forrester, S., Fügedi, U., Gilcucis, A., Gregorauskiene, V., DE GROOT, W., Gulan, A., Haslinger, E., Hayoz, P., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Kwećko, P., Kuti, L., Lima, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Négrel, P., O’Connor, P., Ottesen, R. T., Pasnieczna, A., Petersell, V., Pfleiderer, S., Poňavič, M., Prazeres, C., Radusinović, S., Salpeteur, I., Sadeghi, M., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Šefčik, P., Sellersjö, E., Slaninka, I., SORIANO-DISLA, J. M., Šorša, A., Svrkota, R., Stafilov, T., Tarvainen, T., Tendavilov, V., Valera, P., Verougstraete, V., Vidojević, D., Zomeni, Z., and Zissimos, A.
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Cadmium ,Agricultural soil ,Compositional data analysis ,PCA ,Continental-scale geochemical mapping ,Europe ,Soil test ,Weathering ,010501 environmental sciences ,010502 geochemistry & geophysics ,01 natural sciences ,Compositional data analysi ,chemistry.chemical_compound ,Geochemistry and Petrology ,Grazing ,Aqua regia ,Glacial period ,0105 earth and related environmental sciences ,Hydrology ,business.industry ,Anomaly (natural sciences) ,chemistry ,Agriculture ,Economic Geology ,Quaternary ,business ,Geology - Abstract
Over 4000 agricultural and grazing land soil samples were collected for the “Geochemical Mapping of Agricultural and Grazing Land Soil of Europe” (GEMAS) project carried out by the EuroGeoSurveys Geochemistry Expert Group. The samples were collected in 33 European countries, covering 5.6 million km 2 at a density of 1 sample site per 2500 km 2 . All samples were analysed by ICP-MS following an aqua regia extraction. The European median Cd concentration is 0.182 mg/kg in agricultural soil and 0.197 mg/kg in grazing land soil (including eastern Ukraine). The Cd map demonstrates the existence of two different geochemical background regimes in northern and southern Europe, separated by the southern limit of the Quaternary glaciation. Cadmium shows two times higher background concentrations in the older and more weathered southern European soil than in northern European soil. The spatial distribution patterns of Cd in the collected soil samples are mainly governed by geology (parent material and mineralisation), as well as weathering, soil formation and climate since the last glaciation period. Locally, in several areas, the natural anomaly pattern is overprinted by anthropogenic emissions from former mining, ore processing and related metal industries. Some Cd anomalies can be attributed to urbanisation and the use of fertilisers. A comparison of the raw data Cd concentration map with its clr-transformed counterpart and selected single element ratio maps demonstrates that substantial additional information about sources and processes governing the distribution of Cd in agricultural soil at the European scale can be obtained. Results of a PCA, carried out following the classical approach (standardised) versus a PCA based on the statistically acceptable approach, using clr-transformed data, are quite comparable.
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- 2017
17. GEMAS : Indium in agricultural and grazing land soil of Europe - Its source and geochemical distribution patterns
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Ladenberger, Anna, Demetriades, Alecos, Reimann, Clemens, Birke, Manfred, Sadeghi, Martiya, Uhlbäck, Jo, Andersson, Madelen, Jonsson, Erik, Albanese, S., Baritz, R., Batista, M. J., Bel-lan, A., Cicchella, D., De Vivo, B., De Vos, W., Dinelli, E., uri?, M., Dusza-Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M A, Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Lima, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., McLaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Ottesen, R. T., Pasieczna, A., Petersell, V., Pfleiderer, S., Ponavic, M., Prazeres, C., Rauch, U., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sellersjö, E., Slaninka, I., Soriano-Disla, J. M., or?a, A., Svrkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zomeni, Z., Ladenberger, A., Demetriades, A., Reimann, C., Birke, M., Sadeghi, M., Uhlbäck, J., Andersson, M., Jonsson, E., Albanese, S., Baritz, R., Batista, M.J., Bel-lan, A., Cicchella, D., De Vivo, B., De Vos, W., Dinelli, E., Ďuriš, M., Dusza-Dobek, A., Eggen, O.A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D.M.A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Lima, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B.I., Maquil, R., Meuli, R.G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Ottesen, R.T., Pasieczna, A., Petersell, V., Pfleiderer, S., Ponavic, M., Prazeres, C., Rauch, U., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A., Schoeters, I., Sellersjö, E., Slaninka, I., Soriano-Disla, J.M., Šorša, A., Svrkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zomeni, Z., Uhlback, J., Albanese, Stefano, Batista, M. J., Bel lan, A., DE VIVO, Benedetto, Dusza Dobek, A., Eggen, O. A., Falconi, M., Flight, D. M. A., Halami ć, J., Lima, Annamaria, Malyuk, B. I., Meuli, R. G., Ottesen, R. T., Pfleiderer, S., Poňavič, M., Radusinović, S., Soriano Disla, J. M., Stafilov, T., and Vidojević, D.
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Mediterranean climate ,Hydrology ,geography ,geography.geographical_feature_category ,Land use ,Lithology ,Iindium ,Geochemistry ,Agricultural soil ,Grazing land soil ,Continental-scale ,Europe ,Weathering ,Soil science ,Spatial distribution ,Karst ,Indium ,Soil series ,Geochemistry and Petrology ,Grazing ,Economic Geology ,Geology - Abstract
Indium is a very rare element, which is usually not reported in geochemical data sets. It is classified as a critical metal, with important applications in the electronics industry, especially in the production of solar panels and liquid-crystal displays (LCDs).Over 4000 samples of agricultural and grazing land soil have been collected for the "Geochemical Mapping of Agricultural and Grazing Land Soil of Europe" (GEMAS) project, carried out by the EuroGeoSurveys Geochemistry Expert Group. Indium concentrations in soil have been analysed using aqua regia extraction followed by ICP-MS. Median values of In for both land use types are nearly identical, 0.0176. mg/kg for agricultural soil and 0.0177. mg/kg for grazing land soil.The spatial distribution patterns of In in European soil are mainly controlled by geology and the presence of Zn and Sn mineralisation. The preference of In to accumulate in the fine-grained fraction of soil with high clay content dominates the major anomaly patterns on the geochemical maps. In the Mediterranean region, secondary In enrichment is visible in karst areas. A notable feature of the In spatial distribution is the large difference between northern and southern Europe, with median values of 0.012 and 0.021. mg. In/kg, respectively, suggesting that, in addition to lithology, weathering and climate are important factors influencing In soil enrichment over time. © 2015 Elsevier B.V.
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- 2015
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18. Geochemical fingerprinting and sources discrimination in soils and sediments at continental scale
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Négrel, P., Sadeghi, M., Ladenberger, A., Reimann, C., Birke, M., ALBANESE, STEFANO, Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Cicchella, D., Demetriades, A., DE VIVO, BENEDETTO, De Vos, W., Dinelli, E., Ďuriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Fabian, K., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., de Caritat, P., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwećko, P., Kuti, L., LIMA, ANNAMARIA, Locutura, J., Lucivjansky, D. P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., O’Connor, P., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Poňavič, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinović, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., Šefčik, P., Sellersjö, E, Skopljak, F., Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Turner, N., Valera, P., Verougstraete, V., Vidojević, D., Zissimos, Z. Zomeni, A. Zissimos, Z. Zomeni, Négrel, P., Sadeghi, M., Ladenberger, A., Reimann, C., Birke, M., Albanese, Stefano, Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Cicchella, D., Demetriades, A., DE VIVO, Benedetto, De Vos, W., Dinelli, E., Ďuriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Fabian, K., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., de Caritat, P., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwećko, P., Kuti, L., Lima, Annamaria, Locutura, J., Lucivjansky, D. P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., O’Connor, P., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Poňavič, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinović, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., Šefčik, P., Sellersjö, E, Skopljak, F., Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Turner, N., Valera, P., Verougstraete, V., Vidojević, D., Zissimos, Z. Zomeni, A. Zissimo, and Z., Zomeni
- Abstract
2108 agricultural soil samples (Ap-horizon, 0-20 cm) were collected in Europe (33 countries, area 5.6 million km(2)) as part of the recently completed GEMAS (GEochemical Mapping of Agricultural and grazing land Soil) soil mapping project. GEMAS soil data have been used to provide a general view of element origin and mobility with a main focus on source parent material (and source rocks) at the continental scale, either by reference to average crustal abundances or to normalized patterns of element mobility during weathering processes. The survey area covers a large territory with diverse types of soil parent materials, with distinct geological history and a wide range of climate zones, and landscapes. To normalize the chemical composition of European agricultural soil, mean values and standard deviation of the selected elements have been compared to model compositions of the upper continental crust (UCC) and mean European river suspended sediment. Some elements are enriched relative to the UCC (Al, P, Pb, Zr,) whereas others, such as Mg, Na and Sr are depleted. The concept of the UCC extended normalization pattern has been applied to selected elements. The mean values of Rb, K, Y, Ti, Al, Si, Zr, Ce and Fe are very similar to the values from the UCC model, even when standard deviations indicate slight enrichment or depletion. Zirconium has the best fit to the UCC model using both mean value and standard deviation. Lead and Cr are enriched in European soil when compared to the UCC model, but their standard deviation values span a large, particularly towards very low values, which can be interpreted as a lithological effect. GEMAS soil data have been normalized to Al and Na, taking into account themain lithologies of the UCC, in order to discriminate provenance sources. Additionally, sodium normalization highlights variations related to the soluble and insoluble behavior of some elements (e.g., K, Rb versus Ti, Al, Si, V, Y, Zr, Ba, and La, respectively), their reactivity (e.g, Fe, Mn, Zn) and association with carbonates (e.g., Ca and Sr). Maps of Europe showing the spatial distribution of normalized compositions and element ratios reveal difficulties with the use of classical element ratios because of the large lithological differences in compositions of soil parent material. The ratio maps and color composite images extracted from the GEMAS data can help to discriminate the main lithologies in Europe at the regional scale but need to be used with caution due to the complexity of superimposed processes responsible for the soil chemical composition.
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- 2015
19. Mobile Metal Ion analysis of European agricultural soils : bioavailability, weathering, geogenic patterns and antrhropogenic anomalies
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Mann, A., Reimann, C., De Caritat, P., Turner, N., Birke, M., Albanese, S., Andersson, M., Baritz, R., Batista, M. J., Bel-Lan, A., Cicchella, D., Demetriades, A., De Vivo, B., De Vos, W., Dinelli, E., uri?, M., Dusza-Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Fabian, K., Filzmoser, P., Flight, D., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halami?, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwe?ko, P., Kuti, L., Ladenberger, A., Lima, A., Locutura, J., Lucivjansky, D. P., Mackovych, D., McLaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Negrel, P., O'Connor, P., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Po?avi?, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinovi?, S., Sadeghi, M., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., ef?ik, P., Sellersjö, E., Skopljak, F., Slaninka, I., or?a, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojevi?, D., Zissimos, A., Zomeni, Z., Mann, A., Reimann, C., De Caritat, P., Turner, N., Birke, M., Albanese, S., Andersson, M., Baritz, R., Batista, M.J., Bel-Lan, A., Cicchella, D., Demetriades, A., De Vivo, B., De Vos, W., Dinelli, E., Ďuriš, M., Dusza-Dobek, A., Eggen, O.A., Eklund, M., Ernstsen, V., Fabian, K., Filzmoser, P., Flight, D., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwećko, P., Kuti, L., Ladenberger, A., Lima, A., Locutura, J., Lucivjansky, D.P., Mackovych, D., Mclaughlin, M., Malyuk, B.I., Maquil, R., Meuli, R.G., Mol, G., Negrel, P., O’Connor, P., Oorts, R.K., Ottesen, R.T., Pasieczna, A., Petersell, W., Pfleiderer, S., Poňavič, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinović, S., Sadeghi, M., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A.J., Schoeters, I., Šefčik, P., Sellersjö, E., Skopljak, F., Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojević, D., Zissimos, A., Zomeni, Z., de Caritat, P., Albanese, Stefano, Batista, M. J., Bel lan, A., DE VIVO, Benedetto, Dusza Dobek, A., Eggen, O. A., Flight, D. M. A., Lima, Annamaria, Lucivjansky, D. P., Malyuk, B. I., Meuli, R. G., Oorts, R. K., Ottesen, R. T., Scheib, A. J., Sellersjö, E, Zissimos, Z. Zomeni, A. Zissimo, and Z., Zomeni
- Subjects
Lithology ,Mineralogy ,Weathering ,GEMAS ,Metal ,chemistry.chemical_compound ,Geochemistry and Petrology ,Aqua regia ,ICP-MS ,geogenic pattern ,anthropogenic anomalie ,General Environmental Science ,geochemical mapping ,business.industry ,Geogenic patterns ,MMI (R) extraction ,General Chemistry ,mobile ,metal ,ion ,Bioavailability ,chemistry ,Agriculture ,visual_art ,Environmental chemistry ,Anthropogenic anomalies ,Soil water ,visual_art.visual_art_medium ,General Earth and Planetary Sciences ,MMI® extraction ,business ,bioavailability ,Geology - Abstract
Two thousand one hundred and eight agricultural soils (0–20 cm depth) collected at a density of one sample per 2500 km2 under the auspices of the Geochemical Mapping of Agricultural Soils (GEMAS) project over most of the European continent have been analysed using the Mobile Metal Ion (MMI®) partial extraction technique with ICP-MS finish. For a number of elements, notably Ce, Ni, and Ca, coherent geogenic patterns have been observed which relate to underlying lithology. For Fe and Al, coherent patterns are also observed but the effects of weathering are evident, and provide a mechanism to explain the acidity of soils in high rainfall areas. Individual anomalies, many related to anthropogenic activity (mining, metallurgy, agriculture) have been observed for Ag, Au, Cu, Pb, Cd and Zn. Comparison of the results with aqua regia digestion and the equivalent National Geochemistry Survey of Australia (NGSA) provides insights into weathering processes and the concept of bioavailability. © 2015 AAG/The Geological Society of London.
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- 2015
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20. GEMAS: Prediction of solid-solution partitioning coefficients (Kd) for cationic metals in soils using mid-infrared diffuse reflectance spectroscopy
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Janik, L. J., Forrester, S. T., Soriano Disla, J. M., Kirby, J. K., McLaughlin, M. J., Reimann, C., Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Birke, M., Cicchella, D., Demetriades, A., De Vos, W., Dinelli, E., Ďuriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Jordan, G., Kaminari, M., Klos, V., Krone, F., Kwećko, P., Kuti, L., Ladenberger, A., Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Poňavič, M., Prazeres, C., Rauch, U., Radusinović, S., Sadeghi, M., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., Sellersjö, E, Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojević, D., Zomeni, Z., ALBANESE, STEFANO, DE VIVO, BENEDETTO, LIMA, ANNAMARIA, Janik, L. J., Forrester, S. T., Soriano Disla, J. M., Kirby, J. K., Mclaughlin, M. J., Reimann, C., Albanese, Stefano, Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Birke, M., Cicchella, D., Demetriades, A., DE VIVO, Benedetto, De Vos, W., Dinelli, E., Ďuriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamić, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Jordan, G., Kaminari, M., Klos, V., Krone, F., Kwećko, P., Kuti, L., Ladenberger, A., Lima, Annamaria, Locutura, J., Lucivjansky, P., Mann, A., Mackovych, D., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Négrel, P., O'Connor, P., Oorts, K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Poňavič, M., Prazeres, C., Rauch, U., Radusinović, S., Sadeghi, M., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., Sellersjö, E, Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojević, D., and Zomeni, Z.
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Cations Solid-solution partitioning coefficients (Kd) Mid-infrared spectroscopy Partial least squares regression Soil - Abstract
Partial least squares regression (PLSR) models, using mid-infrared (MIR) diffuse reflectance Fourier-transformed (DRIFT) spectra,wereusedtopredictdistributioncoefficient(Kd)valuesforselectedaddedsolublemetalcations(Agþ,Co 2þ,Cu 2þ,Mn 2þ,Ni 2þ, Pb2þ, Sn 4þ, and Zn2þ) in 4813 soils of the Geochemical Mapping of Agricultural Soils (GEMAS) program. For the development of the PLSR models, approximately 500 representative soils were selected based on the spectra, and Kd values were determined using a singlepointsolublemetal orradioactiveisotopespike.Theoptimummodels, usingacombinationofMIR–DRIFTspectra andsoilpH,resulted ingoodpredictionsforlogKdþ1forCo,Mn,Ni,Pb,andZn(R20.83)butpoorpredictionsforAg,Cu,andSn(R2
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- 2015
21. Multispectral and hyperspectral remote sensing as a source of knowledge in the Portuguese sector of the Iberian Pyrite Belt.
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Quental, L., Gonçalves, P., de Oliveira, D., Batista, M. J., Matos, J. X., Sousa, A. J., Marsh, S., Carreiras, J., and Dias, R.
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REMOTE sensing ,MINES & mineral resources ,DISCRIMINATION (Sociology) ,RESEARCH & development - Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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- 2020
22. Geophysical surveys in the Portuguese sector of the Iberian Pyrite Belt: a global overview focused on the massive sulphide exploration and geologic interpretation.
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Matos, J. X., Carvalho, J., Represas, P., Batista, M. J., Sousa, P., Ramalho, E. C., Marques, F., Morais, I., Albardeiro, L., Gonçalves, P., and Dias, P.
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GEOPHYSICS ,SULFIDES ,ACQUISITION of data ,ELECTROMAGNETISM - Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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- 2020
23. Geochemical exploration and assessment of environmental impacts in the Portuguese sector of the Iberian Pyrite Belt.
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Batista, M. J., Mateus, A., Matos, J. X., Gonçalves, M. A., Figueiras, J., Abreu, M. M., and Luz, F.
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ENVIRONMENTAL impact analysis ,GEOPHYSICS ,GEOCHEMISTRY ,INFORMATION storage & retrieval systems - Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2020
24. Mineral sustainability of the Portuguese sector of the Iberian Pyrite Belt.
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de Oliveira, D. P. S., Batista, M. J., Matos, J. X., and Silva, T. P.
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SUSTAINABILITY ,MINERALS ,SULFIDE minerals ,CEMENTATION (Metallurgy) - Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2020
25. Portable X-ray fluorescence and clustering methods applied to mineral exploration: the significance and nature of Batigelas anomaly (Ossa-Morena Zone - Cabeço de Vide, Portugal).
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Nogueira, P., Afonso, P., Roseiro, J., Maia, M., São Pedro, D., Moreira, N., Matos, J. X., and Batista, M. J.
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X-ray fluorescence ,PROSPECTING ,DRILLING & boring ,GEOCHEMISTRY ,K-means clustering - Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2020
26. Pioneer Mediterranean Shrub Species Revegetating Soils Developed on Mining Soils/Spoils
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Fundação para a Ciência e a Tecnologia (Portugal), Batista, M. J., González-Fernández, Oscar, Abreu, M. M., Queralt Mitjans, Ignacio, Carvalho, M. L., Fundação para a Ciência e a Tecnologia (Portugal), Batista, M. J., González-Fernández, Oscar, Abreu, M. M., Queralt Mitjans, Ignacio, and Carvalho, M. L.
- Abstract
Spontaneous and autochthonous species of plants growing on degraded and contaminated soils/spoils that survive in such environments show, in general, no symptoms of toxicity. This study compares concentrations of chemical elements in different leaves maturation and in different seasons of several native species in a massive sulphide in an abandoned mine area. The objective is to evaluate if these species can play an important role on the stabilization of degraded soils and mine spoils. Total concentrations of chemical elements were great in soils. However, in general, only <1% of the total concentration was extracted by DTPA or ammonium acetate solutions. Total and available fraction of the chemical elements has similar behaviour between soil sites. Mature leaves have higher concentrations of As, Cu, Fe, Mn, Pb and Zn than younger ones. An opposite behaviour occurs with S. Winter and spring variations in most chemical elements concentrations in the plant leaves are not significantly different, except for As. Elemental concentrations of plant leaves are independent of the same elements concentrations (total and available fraction) in soils where plants have grown. The concentrations of As, Cu and Pb in plant leaves were below the level of risk to be ingested by grazing animals, although soils are above the reported thresholds. Therefore, all studied plant species can be considered for phytostabilization programmes, but the use of the land for pasture may not be a solution considering that animals ingest soil along with herbage. Copyright © 2016 John Wiley & Sons, Ltd.
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- 2017
27. GEMAS: Spatial distribution of the pH of European agricultural and grazing land soils
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Fabian C., Reimann C., Fabian K., Birke M., Baritz R., Haslinger E., Albanese S., Andersson M., Batista M. J., Bel lan A., Cicchella D., Demetriades A., De Vivo B., De Vos W., Duriš M., Dusza Dobek A., Eggen O. A., Eklund M., Ernstsen V., Filzmoser P., Flight D. M. A., Forrester S., Fuchs M., Fügedi U., Gilucis A., Gosar M., Gregorauskiene V., De Groot W., Gulan A., Halamić J., Hayoz P., Hoffmann R., Hoogewerff J., Hrvatovic H., Husnjak S., Janik L., Jordan G., Kaminari M., Kirby J., Kivisilla J., Klos V., Krone F., Kwećko P., Kuti L., Ladenberger A., Lima A., Locutura J., Lucivjansky D. P., Mann A., Mackovych D., McLaughlin M., Malyuk B. I., Maquil R., Meuli R. G., Mol G., Negrel P., O'Connor P., Oorts R. K., Ottesen R. T., Pasieczna A., Petersel, W., Pfleiderer S., Poňavič M., Pramuka S., Prazeres C., Rauch U., Radusinović S., Salpeteur I., Scanlon R., Schedl A., Scheib A. J., Schoeters I., Šefčik P., Sellersjö E., Skopljak F., Slaninka I., Šorša A., Srvkota R., Stafilov T., Tarvainen T., Trendavilov V., Valera P., Verougstraete V., Vidojević D., Zissimos A., Zomeni Z., DINELLI, ENRICO, Fabian C., Reimann C., Fabian K., Birke M., Baritz R., Haslinger E., Albanese S., Andersson M., Batista M.J., Bel-lan A., Cicchella D., Demetriades A., De Vivo B., De Vos W., Dinelli E., Duriš M., Dusza-Dobek A., Eggen O.A., Eklund M., Ernstsen V., Filzmoser P., Flight D.M.A., Forrester S., Fuchs M., Fügedi U., Gilucis A., Gosar M., Gregorauskiene V., De Groot W., Gulan A., Halamić J., Hayoz P., Hoffmann R., Hoogewerff J., Hrvatovic H., Husnjak S., Janik L., Jordan G., Kaminari M., Kirby J., Kivisilla J., Klos V., Krone F., Kwećko P., Kuti L., Ladenberger A., Lima A., Locutura J., Lucivjansky D.P., Mann A., Mackovych D., McLaughlin M., Malyuk B.I., Maquil R., Meuli R.G., Mol G., Negrel P., O'Connor P., Oorts R.K., Ottesen R.T., Pasieczna A., Petersel, W., Pfleiderer S., Poňavič M., Pramuka S., Prazeres C., Rauch U., Radusinović S., Salpeteur I., Scanlon R., Schedl A., Scheib A.J., Schoeters I., Šefčik P., Sellersjö E., Skopljak F., Slaninka I., Šorša A., Srvkota R., Stafilov T., Tarvainen T., Trendavilov V., Valera P., Verougstraete V., Vidojević D., Zissimos A., Zomeni Z., Fabian, C., Reimann, C., Fabian, K., Birke, M., Baritz, R., Haslinger, E., Albanese, Stefano, Andersson, M., Batista, M. J., BEL LAN, A., Cicchella, D., Demetriades, D., DE VIVO, Benedetto, DE VOS, W., Dinelli, E., Duriš, M., DUSZA DOBEK, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fugedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., DE GROOT, W., Gulan, A., Halamic, J., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Ladenberger, A., Lima, Annamaria, Locutura, J., Lucivjansky, D. P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., Negrel, P., O’Connor, P., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Ponavic, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., Šefcik, P., Sellersjo, E., Skopljak, F., Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zissimos, A., and Zomeni, Z.
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Hydrology ,Soil test ,Spatial distribution ,Pollution ,Agricultural soil ,Grazing soil ,GEMAS ,chemistry.chemical_compound ,soil pH ,GEochemical Mapping ,chemistry ,Geochemistry and Petrology ,Soil pH ,Soil water ,Grazing ,Environmental Chemistry ,Carbonate ,Environmental science ,Precipitation ,Glacial period ,grazing land soil ,pH value ,Grazing land soil ,geochemistry - Abstract
During 2008 the GEochemical Mapping of Agricultural Soils (GEMAS) project collected 2108 agricultural (ploughed soil, Ap horizon, 0–20 cm) and 2023 grazing land soil samples (Gr, 0–10 cm) evenly spread over 33 European countries and covering an area of 5.6 million km2. The pH of all samples was determined by one single laboratory applying a 0.01 M CaCl2 extraction, and following a strict quality-control procedure. The resulting pH-value distributions for European Ap and Gr soil are both bimodal. Broad acidic modes, with pH between 4 and 6, and sharp alkaline modes, with pH between 7 and 8 due to the Ca2+ buffer system, are clearly separated. The European median pH is 5.8 for the GEMAS Ap soil samples and 5.5 for the GEMAS Gr soil samples. According to the pH distribution maps, Europe is separated into two main zones: northern Europe with generally lower pH values (Ap: 5.2, Gr: 4.8), dominated by acidic soils occurring in Fennoscandia, and southern Europe with higher pH values (Ap: 6.3, Gr: 5.9), dominated by carbonate rich soils. The separation line coincides with the southern border of the sediments of the last glaciation. The dominant factors controlling pH at the European scale are thus geology (crystalline bedrock) in combination with climate (temperature and precipitation). The GEMAS pH maps mainly reflect the natural site conditions on the European scale, whilst anthropogenic impact is hardly detectable. The GEMAS results provide a unique set of homogenous and spatially representative soil pH data for the continent. The data set defines a dependable continental-scale background, and offers the possibility to calibrate studies on more detailed scales.
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- 2014
28. Geochemical fingerprinting and source discrimination of agricultural soils at continental scale
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Négrel, P., Sadeghi, M., Ladenberger, A., Reimann, C., Birke, M., Albanese, S., Andersson, M., Baritz, R., Batista, M. J., Bel lan, A., Cicchella, D., Demetriades, A., De Vivo, B., De Vos, W., Duriš, M., Dusza Dobek, A., Eggen, O. A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D. M. A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Lima, A., Locutura, J., Lucivjansky, D. P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B. I., Maquil, R., Meuli, R. G., Mol, G., O'Connor, P., Oorts, R. K., Ottesen, R. T., Pasieczna, A., Petersell, W., Pfleiderer, S., Ponavic, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A. J., Schoeters, I., Šefcik, P., Sellersjö, E., Skopljak, F., Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zissimos, A., Z. , Zomeni, DINELLI, ENRICO, Négrel, P., Sadeghi, M., Ladenberger, A., Reimann, C., Birke, M., Albanese, S., Andersson, M., Baritz, R., Batista, M.J., Bel-lan, A., Cicchella, D., Demetriades, A., De Vivo, B., De Vos, W., Dinelli, E., Duriš, M., Dusza-Dobek, A., Eggen, O.A., Eklund, M., Ernstsen, V., Filzmoser, P., Flight, D.M.A., Forrester, S., Fuchs, M., Fügedi, U., Gilucis, A., Gosar, M., Gregorauskiene, V., De Groot, W., Gulan, A., Halamic, J., Haslinger, E., Hayoz, P., Hoffmann, R., Hoogewerff, J., Hrvatovic, H., Husnjak, S., Janik, L., Jordan, G., Kaminari, M., Kirby, J., Kivisilla, J., Klos, V., Krone, F., Kwecko, P., Kuti, L., Lima, A., Locutura, J., Lucivjansky, D.P., Mann, A., Mackovych, D., Mclaughlin, M., Malyuk, B.I., Maquil, R., Meuli, R.G., Mol, G., O'Connor, P., Oorts, R.K., Ottesen, R.T., Pasieczna, A., Petersell, W., Pfleiderer, S., Ponavic, M., Pramuka, S., Prazeres, C., Rauch, U., Radusinovic, S., Salpeteur, I., Scanlon, R., Schedl, A., Scheib, A.J., Schoeters, I., Šefcik, P., Sellersjö, E., Skopljak, F., Slaninka, I., Šorša, A., Srvkota, R., Stafilov, T., Tarvainen, T., Trendavilov, V., Valera, P., Verougstraete, V., Vidojevic, D., Zissimos, A., Z., Zomeni., Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Geological Survey of Sweden, sgu, Geological Survey of Norway (NGU), Geological Survey of Norway, and Federal Institute for Geosciences and Natural Resources (BGR)
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Soil map ,genetic structures ,Soil test ,Weathering ,Parent material ,Mineralogy ,Sediment ,Geology ,15. Life on land ,Soil type ,Agricultural soil ,Upper continental crust UCC ,Geochemistry ,Geochemistry and Petrology ,[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry ,Soil water ,Chemical composition - Abstract
International audience; 2108 agricultural soil samples (Ap-horizon, 0–20 cm) were collected in Europe (33 countries, area 5.6 million km2) as part of the recently completed GEMAS (GEochemical Mapping of Agricultural and grazing land Soil) soil mapping project. GEMAS soil data have been used to provide a general view of element origin and mobility with a main focus on source parent material (and source rocks) at the continental scale, either by reference to average crustal abundances or to normalized patterns of element mobility during weathering processes. The survey area covers a large territory with diverse types of soil parent materials, with distinct geological history and a wide range of climate zones, and landscapes.To normalize the chemical composition of European agricultural soil, mean values and standard deviation of the selected elements have been compared to model compositions of the upper continental crust (UCC) and mean European river suspended sediment. Some elements are enriched relative to the UCC (Al, P, Pb, Zr,) whereas others, such as Mg, Na and Sr are depleted. The concept of the UCC extended normalization pattern has been applied to selected elements. The mean values of Rb, K, Y, Ti, Al, Si, Zr, Ce and Fe are very similar to the values from the UCC model, even when standard deviations indicate slight enrichment or depletion. Zirconium has the best fit to the UCC model using both mean value and standard deviation. Lead and Cr are enriched in European soil when compared to the UCC model, but their standard deviation values span a large, particularly towards very low values, which can be interpreted as a lithological effect.GEMAS soil data have been normalized to Al and Na, taking into account the main lithologies of the UCC, in order to discriminate provenance sources. Additionally, sodium normalization highlights variations related to the soluble and insoluble behavior of some elements (e.g., K, Rb versus Ti, Al, Si, V, Y, Zr, Ba, and La, respectively), their reactivity (e.g, Fe, Mn, Zn) and association with carbonates (e.g., Ca and Sr). Maps of Europe showing the spatial distribution of normalized compositions and element ratios reveal difficulties with the use of classical element ratios because of the large lithological differences in compositions of soil parent material. The ratio maps and color composite images extracted from the GEMAS data can help to discriminate the main lithologies in Europe at the regional scale but need to be used with caution due to the complexity of superimposed processes responsible for the soil chemical composition.
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- 2015
- Full Text
- View/download PDF
29. Geochemistry of European Bottled Waters
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REIMANN C., BIRKE M., KOLLER F., ONUZI K., HOBIGER G., SCHEDL A., HASLINGER E., FILZMOSER P., GREGORAUSKIENE V., DE VOS W., SCHOETERS I., HRVATOVIC H., MIOSIC N., SKOPLJAK F., SAMARDZIC N., TRENDAVILOV V., HALAMIĆ J., ŠORŠA A., DURIS M., OTTESEN R. T., KIVISILLA J., PETERSELL V., BITYUKOVA L., TARVAINEN T., JARVA J., SALPETEUR I., INNOCENT C., STAFILOV T., DEMETRIADES A., STEFOULI M., GLATTE W., HARAZIM B., FLOHR F., DEGTJAREV A., JAEHNE F., RAUSCH J., RAUCH U., KASTE L., LORENZ H., JORDAN G., WIGUM B. J., FLYNN R., CICCHELLA D., DINELLI E., VALERA P., GILUCIS A., MAQUIL R., TITOVET M., DEVIC N., EGGEN O., FRENGSTAD B., SMIETANSKI L., LOURENÇO C., BATISTA M. J., ION A., IONESCO C., PHILLIPOV N., KARNACHUK O., SALMINEN R., ZLOKOLICA MANDIC M., PETROVIC T., GULAN A., VELJKOVIC N., MALIK P., GOSAR M., LOCUTURA J., BEL LAN A., CORRAL M., LAX K., ANDERSSON M., HAYOZ P., FLIGHT D., REEDER S., SMEDLEY P., BANKS D., MALYUK B. I., KLOS V., VLADYMYROVA M., DE VIVO, BENEDETTO, LIMA, ANNAMARIA, ALBANESE, STEFANO, Reimann, C., Birke, M., Koller, F., Onuzi, K., Hobiger, G., Schedl, A., Haslinger, E., Filzmoser, P., Gregorauskiene, V., DE VOS, W., Schoeters, I., Hrvatovic, H., Miosic, N., Skopljak, F., Samardzic, N., Trendavilov, V., Halamić, J., Šorša, A., Duris, M., Ottesen, R. T., Kivisilla, J., Petersell, V., Bityukova, L., Tarvainen, T., Jarva, J., Salpeteur, I., Innocent, C., Stafilov, T., Demetriades, A., Stefouli, M., Glatte, W., Harazim, B., Flohr, F., Degtjarev, A., Jaehne, F., Rausch, J., Rauch, U., Kaste, L., Lorenz, H., Jordan, G., Wigum, B. J., Flynn, R., DE VIVO, Benedetto, Lima, Annamaria, Albanese, Stefano, Cicchella, D., Dinelli, E., Valera, P., Gilucis, A., Maquil, R., Titovet, M., Devic, N., Eggen, O., Frengstad, B., Smietanski, L., Lourenço, C., Batista, M. J., Ion, A., Ionesco, C., Phillipov, N., Karnachuk, O., Salminen, R., ZLOKOLICA MANDIC, M., Petrovic, T., Gulan, A., Veljkovic, N., Malik, P., Gosar, M., Locutura, J., BEL LAN, A., Corral, M., Lax, K., Andersson, M., Hayoz, P., Flight, D., Reeder, S., Smedley, P., Banks, D., Malyuk, B. I., Klos, V., and Vladymyrova, M.
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Europe ,Geochemistry ,Underground water - Abstract
Vengono riportate le concentrazioni di elementi in traccia delle acque minerali dell'Europa acquistate nei punti di vendita
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- 2010
30. The EuroGeoSurveys geochemical mapping of agricultural and grazing land soils project (GEMAS) - Evaluation of quality control results of aqua regia extraction analysis
- Author
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REIMANN C., DEMETRIADES A., EGGEN O. A., FILMOZER P., THE EUROGEOSURVEYS GEOCHEMISTRY EXPERT GROUP, ALBANESE S., BATISTA M. J., BEL LAN A., BIRKE M., CICCHELLA D., DE VIVO B., DE VOS W., DURIS M., DUSZA DOBEK A., ERNSTSEN V., FLIGHT D., GILUCIS A., GOSAR M., GREGORAUSKIENE V., GULAN A., HAYOZ P., HALAMIC J., HASLINGER E., HRATOVIC H., ION A., IVANOVNA Y., JOHNSON C., JORDAN G., KISIVILLA J., KLEIN P., KWECKO P., LAX K., LIMA A., LOCUTURA J., MALYUK B. I., MAQUIL R., MARKU S., MARTINS L., MAZREKU A., MESSINA A., O’CONNOR P. J., OTTESEN R. T., PASIECZNA A., PETERSELL W., REEDER S., SALPETEUR I., SCHEDL A., SEFCIK P., SLANINKA I., SORSA A., SELINUS O., STAFILOV T., TARVAINEN T., TRENDAVILOV V., UTERMANN J., VALERA P., VIDOJEVIC D., VOLDEN T., DINELLI, ENRICO, REIMANN C., DEMETRIADES A., EGGEN O.A., FILMOZER P., THE EUROGEOSURVEYS GEOCHEMISTRY EXPERT GROUP, ALBANESE S., BATISTA M. J., BEL-LAN A., BIRKE M., CICCHELLA D., DE VIVO B., DE VOS W., DINELLI E., DURIS M., DUSZA-DOBEK A., ERNSTSEN V., FLIGHT D., GILUCIS A., GOSAR M., GREGORAUSKIENE V., GULAN A., HAYOZ P., HALAMIC J., HASLINGER E., HRATOVIC H., ION A., IVANOVNA Y., JOHNSON C., JORDAN G., KISIVILLA J., KLEIN P., KWECKO P., LAX K., LIMA A., LOCUTURA J., MALYUK B. I., MAQUIL R., MARKU S., MARTINS L., MAZREKU A., MESSINA A., O’CONNOR P. J., OTTESEN R. T., PASIECZNA A., PETERSELL W., REEDER S., SALPETEUR I., SCHEDL A., SEFCIK P., SLANINKA I., SORSA A., SELINUS O., STAFILOV T., TARVAINEN T., TRENDAVILOV V., UTERMANN J., VALERA P., VIDOJEVIC D., and VOLDEN T.
- Abstract
Rigorous quality control (QC) is one of the keystones to the success of any regional geochemical mapping programme. For the EuroGeoSurveys (EGS) GEMAS (Geochemical mapping of agricultural and grazing land soils) project 2211 samples (including field duplicates) of agricultural soil (Ap, Ap-horizon, 0-20 cm) and 2118 samples (including field duplicates) from land under permanent grass cover ("grazing land" - Gr, topsoil 0-10 cm) were collected from a large part of Europe, centrally prepared (air dried, sieved to
- Published
- 2009
31. EuroGeoSurveys geochemical mapping of agricultural and grazing land soil of Europe (GEMAS). Field manual
- Author
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REIMANN C., ALBANESE S., BATISTA M. J., BEL LAN A., BIRKE M., CICCHELLA D., DEMETRIADES A., DE VIVO B., DE VOS W., DURIS M., DUSZA DOBEK A., ERNSTSEN V., FLIGHT D., GILUCIS A., GOSAR M., GREGORAUSKIENE V., GULAN A., HAYOZ P., HALAMIC J., HASLINGER E., HRATOVIC H., ION A., IVANOVNA Y., JOHNSON C., JORDAN G., KISIVILLA J., KLEIN P., KWECKO P., LAX K., LIMA A., LOCUTURA J., MALYUK B. I., MAQUIL R., MARKU S., MARTINS L., MAZREKU A., MESSINA A., O’CONNOR P. J., OTTESEN R. T., PASIECZNA A., PETERSELL W., REEDER S., SALPETEUR I., SCHEDL A. | SEFCIK P., SLANINKA I., SORSA A., SELINUS O., STAFILOV T., TARVAINEN T., TRENDAVILOV V., UTERMANN J., VALERA P., VIDOJEVIC D., VOLDEN T., DINELLI, ENRICO, REIMANN C., ALBANESE S., BATISTA M. J., BEL-LAN A., BIRKE M., CICCHELLA D., DEMETRIADES A., DE VIVO B., DE VOS W., DINELLI E., DURIS M., DUSZA-DOBEK A., ERNSTSEN V., FLIGHT D., GILUCIS A., GOSAR M., GREGORAUSKIENE V., GULAN A., HAYOZ P., HALAMIC J., HASLINGER E., HRATOVIC H., ION A., IVANOVNA Y., JOHNSON C., JORDAN G., KISIVILLA J., KLEIN P., KWECKO P., LAX K., LIMA A., LOCUTURA J., MALYUK B. I., MAQUIL R., MARKU S., MARTINS L., MAZREKU A., MESSINA A., O’CONNOR P. J., OTTESEN R. T., PASIECZNA A., PETERSELL W., REEDER S., SALPETEUR I., SCHEDL A.| SEFCIK P., SLANINKA I., SORSA A., SELINUS O., STAFILOV T., TARVAINEN T., TRENDAVILOV V., UTERMANN J., VALERA P., VIDOJEVIC D., and VOLDEN T.
- Abstract
REACH (Registration, Evaluation and Authorisation of Chemicals), the new European Chemicals Regulation was adopted in December 2006. It came into force on the 1st June 2007. REACH, as well as the pending EU Soil Protection Directive, require additional knowledge about "soil quality" at the European scale. The GEMAS (geochemical mapping of agricultural soils and grazing land of Europe) project aims at providing harmonized geochemical data of arable land and land under permanent grass cover at the continental, European scale. Geological Surveys in 34 European countries, covering an area of 5.6 million km2, have agreed to sample their territory at a sample density of 1 site each, arable land (0-20 cm) and land under permanent grass cover (0-10 cm), per 2500 km2. Sampling will take place during 2008, following a jointly agreed field protocol which is presented in this report. All samples will be prepared in just one laboratory, a strict quality control procedure has been established and all samples will always be jointly analyzed in just one laboratory for any one chemical element/parameter.
- Published
- 2008
32. Distribution of elements in stream sediments
- Author
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DE VOS W., BATISTA M. J., PIRC S., ALTRI, DE VIVO, BENEDETTO, LIMA, ANNAMARIA, DE VOS W., TARVAINEN T., ALTRI, DE VOS, W., Batista, M. J., Pirc, S., DE VIVO, Benedetto, Lima, Annamaria, and Altri
- Published
- 2006
33. Geochemical atlas of Europe. FOREGS geochemical baseline mapping. The Portuguese experience
- Author
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BATISTA M. J., MARTINS L., SALMINEN R., BIDOVEC M., PIRC S., DEMETRIADES A., ALTRI, DE VIVO, BENEDETTO, LIMA, ANNAMARIA, Batista, M. J., Martins, L., Salminen, R., Bidovec, M., Pirc, S., Demetriades, A., DE VIVO, Benedetto, Lima, Annamaria, and Altri
- Published
- 2005
34. Iberian Pyrite Belt Exploration Preface.
- Author
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Matos, J. X., de Oliveira, D. P. S., Batista, M. J., Pereira, Z., Albardeiro, L., Morais, I., Mendes, M., Marques, F., Solá, R., Salgueiro, R., Carvalho, J., Gonçalves, P., and Oliveira, J. T.
- Subjects
MINES & mineral resources - Published
- 2020
35. FOREGS geochemical baseline mapping programme - A new European wide database and geochemical atlas
- Author
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SALMINEN R., BATISTA M. J., BIDOVEC M., DEMETRIADES A., DE VOS W., DURIS M., GILUCIS A., GREGORAUSKIENE V., HALAMIC J., HETZNANN P., JORDAN G., KLAVER G., KLEIN P., LIS J., LOCUTURA J., MARSINA K., MAZREKU A., O'CONNOR P. J., OLSSON S. A., OTTESEN R. T., PETERSELL V., PLANT J. A., REEDER S., SALPATEUR I., SANDSTROM H., SIEWERS U., STEENFELT A., TARVAINEN T., DE VIVO, BENEDETTO, Juvonen, R., Farmer, John, Salminen, R., Batista, M. J., Bidovec, M., Demetriades, A., DE VIVO, Benedetto, DE VOS, W., Duris, M., Gilucis, A., Gregorauskiene, V., Halamic, J., Hetznann, P., Jordan, G., Klaver, G., Klein, P., Lis, J., Locutura, J., Marsina, K., Mazreku, A., O'Connor, P. J., Olsson, S. A., Ottesen, R. T., Petersell, V., Plant, J. A., Reeder, S., Salpateur, I., Sandstrom, H., Siewers, U., Steenfelt, A., and Tarvainen, T.
- Subjects
Geochemical mapping ,Elements ,Heavy metals ,Baseline ,Europe - Abstract
The IUGS/IAGC Global Geochemical Baselines Programme has a goal of establishing a land-surface global geochemical reference network, prowiding multi-media, multi-element baseline data for a wide range of environmental and resource applications. As a European contribution to the global programme, 26 countries established a project under the auspices of the Forum of European Geological Surveys (FOREGS) to provide high quality environmental geochemical baseline data. The main aims of the project are: - to establish uniform methods for sampling, analysis and the data managemnt ; - the collection and analysis of geochemical materials throughout Europe ; - the preparation of a standardised reference dataset of geochemical baseline data. According to the recomendation of IGCP 259 (International Geochemical Mapping) Europe was divided into 160 by 160 km grid cells. Stream water, minerogenic stream sediment, minerogenic topsoil and sub soil and the soil organic layer samples were collected from five randomly selected 100 km2 catchment areas in each grid cell. Respectively minerogenic floodplain sediment (the uppermost 25 cm) was sampled from five 1000 km2 catchemnt areas (icluding the 100 km2 catchment area). Field work was carried out according to the commonly accepted published Field amnual. Samples were analysed for more than 50 elements and other parameters (such as pH and grain size). Both total and aqua regia extractable concentrations were detrmined from
- Published
- 2003
36. FOREGS geochemical baseline mapping: a new European wide database and geochemical atlas
- Author
-
SALMINEN R., BATISTA M. J., BIDOVEC M., DEMETRIADES A., DE VOS W., DURIS M., GILUCIS A., GREGORAUSKIENE V., HALAMIC J., HEITZMANN P., JORDAN G., KIVISILLA J., KLAVER G., KLEIN P., LIS J., LOCUTURA J., MARSINA K., O'CONNOR P. J., OLSSON S., OTTESEN R. T., PLANT J. A., REEDER S., SALPATEUR I., SIEWERS U., STEENFELT A., DE VIVO, BENEDETTO, Salminen, R., Batista, M. J., Bidovec, M., Demetriades, A., DE VIVO, Benedetto, DE VOS, W., Duris, M., Gilucis, A., Gregorauskiene, V., Halamic, J., Heitzmann, P., Jordan, G., Kivisilla, J., Klaver, G., Klein, P., Lis, J., Locutura, J., Marsina, K., O'Connor, P. J., Olsson, S., Ottesen, R. T., Plant, J. A., Reeder, S., Salpateur, I., Siewers, U., and Steenfelt, A.
- Abstract
Geological Survey of Finland and the International Association of Geoanalysis, Books of Abstracts
- Published
- 2003
37. The concept of compositional data analysis in practice--total major element concentrations in agricultural and grazing land soils of Europe
- Author
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Reimann C., Filzmoser P., Fabian K., Hron K., Birke M., Demetriades A., Ladenberger A., Albanese S., Andersson M., Arnoldussen A., Baritz R., Batista M. J., Bel lan A., Cicchella D., De Vivo B., De Vos W., Duris M., Dusza Dobek A., Eggen O. A., Eklund M., Ernstsen V., Finne T. E., Flight D., Forrester S., Fuchs M., Fugedi U., Gilucis A., Gosar M., Gregorauskiene V., Gulan A., Halamic J., Haslinger E., Hayoz P., Hobiger G., Hoffmann R., Hoogewerff J., Hrvatovic H., Husnjak S., Janik L., Johnson C. C., Jordan G., Kirby J., Kivisilla J., Klos V., Krone F., Kwecko P., Kuti L., Lima A., Locutura J., Lucivjansky P., Mackovych D., Malyuk B. I., Maquil R., McLaughlin M. J., Meuli R. G., Miosic N., Mol G., Négrel P., O'Connor P., Oorts K., Ottesen R. T, Pasieczna A., Petersell V., Pfleiderer S., Ponavic M., Prazeres C., Rauch U., Salpeteur I., Schedl A., Scheib A., Schoeters I., Sefcik P., Sellersjö E., Skopljak F., Slaninka I., Šorša A., Srvkota R., Stafilov T., Tarvainen T., Trendavilov V., Valera P., Verougstraete V., Vidojevic D., Zissimos A. M., Zomeni Z., DINELLI, ENRICO, Reimann, C., Filzmoser, P., Fabian, K., Hron, K., Birke, M., Demetriades, A., Dinelli, E., Ledenberger, A., GEMAS Project, Team, Albanese, Stefano, Cicchella, D., DE VIVO, Benedetto, Lima, Annamaria, Valera, P., Reimann C., Filzmoser P., Fabian K., Hron K., Birke M., Demetriades A., Dinelli E., Ladenberger A., Albanese S., Andersson M., Arnoldussen A., Baritz R., Batista M.J., Bel-lan A., Cicchella D., De Vivo B., De Vos W., Duris M., Dusza-Dobek A., Eggen O.A., Eklund M., Ernstsen V., Finne T.E., Flight D., Forrester S., Fuchs M., Fugedi U., Gilucis A., Gosar M., Gregorauskiene V., Gulan A., Halamic J., Haslinger E., Hayoz P., Hobiger G., Hoffmann R., Hoogewerff J., Hrvatovic H., Husnjak S., Janik L., Johnson C.C., Jordan G., Kirby J., Kivisilla J., Klos V., Krone F., Kwecko P., Kuti L., Lima A., Locutura J., Lucivjansky P., Mackovych D., Malyuk B.I., Maquil R., McLaughlin M.J., Meuli R.G., Miosic N., Mol G., Négrel P., O'Connor P., Oorts K., Ottesen R.T, Pasieczna A., Petersell V., Pfleiderer S., Ponavic M., Prazeres C., Rauch U., Salpeteur I., Schedl A., Scheib A., Schoeters I., Sefcik P., Sellersjö E., Skopljak F., Slaninka I., Šorša A., Srvkota R., Stafilov T., Tarvainen T., Trendavilov V., Valera P., Verougstraete V., Vidojevic D., Zissimos A.M., and Zomeni Z.
- Subjects
Environmental Engineering ,Multivariate analysis ,XRF ,Agricultural soil ,Major elements ,Europe ,Geochemistry ,Compositional data ,Scandinavian and Nordic Countries ,Stability (probability) ,Data type ,Major element ,Soil ,Statistics ,Environmental Chemistry ,Soil Pollutants ,Waste Management and Disposal ,Mathematics ,geochemistry ,Measure (data warehouse) ,Compositional data, Agricultural Soils, Grazing soils ,agricultural soil ,major elements ,Agriculture ,Pollution ,compositional data ,Trace Elements ,Euclidean distance ,Variable (computer science) ,Exploratory data analysis ,Multivariate Analysis ,Europa ,Environmental Monitoring - Abstract
Applied geochemistry and environmental sciences invariably deal with compositional data. Classically, the original or log-transformed absolute element concentrations are studied. However, compositional data do not vary independently, and a concentration based approach to data analysis can lead to faulty conclusions. For this reason a better statistical approach was introduced in the 1980s, exclusively based on relative information. Because the difference between the two methods should be most pronounced in large-scale, and therefore highly variable, datasets, here a new dataset of agricultural soils, covering all of Europe (5.6 million km2) at an average sampling density of 1 site/2500 km2, is used to demonstrate and compare both approaches. Absolute element concentrations are certainly of interest in a variety of applications and can be provided in tabulations or concentration maps. Maps for the opened data (ratios to other elements) provide more specific additional information. For compositional data XY plots for raw or log-transformed data should only be used with care in an exploratory data analysis (EDA) sense, to detect unusual data behaviour, candidate subgroups of samples, or to compare pre-defined groups of samples. Correlation analysis and the Euclidean distance are not mathematically meaningful concepts for this data type. Element relationships have to be investigated via a stability measure of the (log-)ratios of elements. Logratios are also the key ingredient for an appropriate multivariate analysis of compositional data, Geological Survey of Norway, Noruega, Institute for Statistics and Probability Theory, Vienna University of Technology, Austria, Department of Mathematical Analysis and Applications of Mathematics, Palacký University, República Checa, Federal Institute for Geosciences and Natural Resources, Alemania, Institute of Geology and Mineral Exploration, Grecia, Dipartimento di Scienze della Terra, Università di Bologna, Italia, Geological Survey of Sweden, Suecia
- Published
- 2011
38. Ceria promotion of acetaldehyde photo-oxidation in a TiO2-based catalyst: a spectroscopic and kinetic study
- Author
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Muñoz-Batista, M. J., primary, Ballari, M. M., additional, Cassano, A. E., additional, Alfano, O. M., additional, Kubacka, A., additional, and Fernández-García, M., additional
- Published
- 2015
- Full Text
- View/download PDF
39. Tin distribution in soils and plants, Cistus ladanifer L., in Neves Corvo mining area
- Author
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Batista, M. J., Abreu, M. M., and Pinto, M. Serrano
- Subjects
Portugal ,estanho ,tin ,cistus ladanifer ,mining area ,soil - Abstract
The Neves Corvo mining area includes the Mina de Neves Corvo (MNC) that started exploitation in 1988 for Cu and Sn and six abandoned Mn and Cu mines. The Volcano Sedimentary Complex (VSC) which hosts the massive sulphide deposits and the Flysch formations of schist and greywacke dominates the regional geology. The aim of this study was to evaluate tin distribution in soils as well as the capacity to absorb and translocate this element for plants (Cistus ladaniferL.) growing in the MNC area. Samples were collected in two campaigns: the first, for soils, in 1971-72 before MNC existence; and the second campaign (1998), 10 years after mining exploitation began in MNC, for soils and plants in the same places sampled in the first campaign. Soil and plant samples were digested with four acids for total elements extraction and analysed by ICP-AES. The soils developed from Flysch formations have the same average Sn concentrations in both campaigns (2.9 mg kg-1). In contrast, the Sn concentration in soils developed on VSC in the second campaign were twice those (10.4 mg kg-1) from soils of the first campaign (4.5 mg kg-1), reflecting mining. However, tin content in soils developed on both lithologies was considered as a background concentration. Generally, plant roots have higher Sn concentrations than leaves.C. ladaniferplants presented highest Sn concentration than soils suggesting tin accumulation by these plants. The soil pH and solid phases where tin was present were determinant factors for tin uptake and translocation from roots to shoots inC. ladaniferplants., A área mineira de Neves Corvo inclui a Mina de Neves Corvo (MNC) cuja exploração teve início em 1988 para Cu e Sn e outras seis minas de Mn e Cu já abandonadas. Na região ocorrem formações geológicas do Complexo Vulcano-Sedimentar (CVS) hospedeiras dos sulfuretos maciços portadores das mineralizações e formações do grupo do Flysch compostas de xistos e grauvaques. Neste trabalho, estudou-se a distribuição do estanho nos solos e a sua capacidade de absorção e translocação pelas plantas (Cistus ladaniferL.) na área mineira de Neves Corvo. As amostras foram colhidas em duas campanhas, entre 1971-72, cerca de 27 anos antes da laboração na MNC, e numa 2ª campanha (1998), 10 anos após o inicio da laboração desta mina, onde nos mesmos locais foram colhidos solos e plantas. As amostras de solos (horizonte superficial), de ambas as campanhas, e de plantas da 2ª campanha foram sujeitas a digestão com quatro ácidos para análise total dos elementos por ICP-AES. Os solos das duas campanhas, desenvolvidos no Flysch, apresentam as mesmas concentrações médias de Sn (2,9 mg kg-1), contrariamente ao que acontece nos solos que cobrem as formações do CVS cujas concentrações na 2º campanha são cerca do dobro das da primeira (4,5 e 10,4 mg kg-1, respectivamente na 1ª e 2ª campanhas), notando-se assim a influência da actividade mineira nestas formações que são hospedeiras da mineralização de estanho. No entanto, em ambos os casos, os solos apresentam concentrações médias de Sn consideradas de fundo geoquímico. Em geral, as plantas apresentam concentrações de Sn mais elevadas nas raízes do que na parte aérea. Os solos apresentam teores de Sn inferiores aos das plantas indicando que estas têm capacidade para acumular aquele elemento. Este facto, pode estar relacionado com a presença de estanho nos solos quase neutros, sob a forma de estanite, também observada nas mineralizações. Nas plantas próximas da exploração da MNC, onde o pH do solo é mais ácido, os teores de Sn podem ser devidos à deposição de material particulado rico em Sn que será adsorvido via estomas. O pH e as fases sólidas nas quais o estanho se encontra nos solos são determinantes para a sua disponibilidade no solo e capacidade para ser absorvido e translocado pelas plantas.
- Published
- 2009
40. Effect of g-C3N4 loading on TiO2-based photocatalysts: UV and visible degradation of toluene
- Author
-
Muñoz-Batista, M. J., primary, Kubacka, A., additional, and Fernández-García, M., additional
- Published
- 2014
- Full Text
- View/download PDF
41. Evaluation of trace elements mobility from soils to sediments between the Iberian Pyrite Belt and the Atlantic Ocean
- Author
-
Batista, M. J., Abreu, M. M., Locutura Rupérez, Juan, Oliveira, D. de, Matos, J. X., Silva, C., Bel-Lan Ballester, Alejandro, Martins, Luciano R., Batista, M. J., Abreu, M. M., Locutura Rupérez, Juan, Oliveira, D. de, Matos, J. X., Silva, C., Bel-Lan Ballester, Alejandro, and Martins, Luciano R.
- Abstract
An environmental study was conducted in 193 stream sediments and 355 soil samples collected in the lower section of Guadiana River Basin to evaluate the trace elements transfer from one compartment into another. The objective was to evaluate the dispersion of Pb, Cu, Zn and other chemical elements resulting from upstream mines into the lower N-S sector of the Guadiana River Basin to the Atlantic Ocean. The area partly includes the Iberian Pyrite Belt, a known volcanogenic massive sulphide (VMS) province with important mining activity history. Median concentrations of the elements Cu, Pb, Zn, Al, As, Ba, Br, Ca, Mg, Mn and Na are generally higher in the studied sediments than in soils. Soils are normally acidic and mobility of elements is in these conditions higher. When the relations between upstream soils and downstream sediments were established, median values were higher in the upstream soils only for elements such as Co, Ni, K, Pb, Mn and Ti, probably the less mobile, and the Cu, Zn, Al, As, Ba, Br, Ca, Cr, Fe, Mg and Na have highest concentrations in the downstream sediments. Lead was considered the less mobile element and Zn the highly mobile of the base metals in the mining area of the lower Guadiana River. Dispersion of the metals, considering the studied soil and sediment samples is partially restricted to the mining areas or downstream sediments but close to the mine sources, where ore tailings and acid waters occur. Near the mouth, concentrations of As, Cu, Pb and Zn increase in relation with mining and other pollution sources. Interaction with salt water forces chemical elements precipitation from water and subsequent increase of their concentration in sediments. This may be the reason for the increase of those chemical elements concentrations in the sediments
- Published
- 2012
42. Curva de dissipação de imazapyr em água de drenos de irrigação, após a aplicação para controle da taboa
- Author
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PRATES, H. T., SILVA, J. B., FABRIS, J. D., FERREIRA, G. A. L., LEITE, C. E. P., BATISTA, M. J., HÉLIO T. PRATES, CNPMS, JOÃO B. SILVA, CNPMS, JOSÉ D. FABRIS, CNPMS, GERALDO A. L. FERREIRA, Consultor, CARLOS E. P. LEITE, CNPMS, and MANUEL J. BATISTA, CODEVASF.
- Subjects
Planta daninha ,Monitoramento ambiental ,Impacto Ambiental ,Herbicida ,Resíduo - Abstract
O herbicida sistémico imazapyr foi usado no controle da taboa (Typha subulata Crespo & Peres-Moreau f.) em drenos de irrigação, como alternativa ao controle mecânico. O resíduo do princípio ativo do herbicida na água foi analisado por cromatografia líquida de alta performance (HPLC). A curv a de di ss ip ação de imazapyr mostrou que o herbicida pode ser usado para o contro le de taboa em drenos de irr iga ção, sem causar danos a culturas vizinhas, desde que a água seja usada, no mínimo, depois de 1,6 a 3,7 dias da aplicação das doses de 500 a 1500 g ha-1, respectivamente. Made available in DSpace on 2011-06-06T17:39:15Z (GMT). No. of bitstreams: 1 Curvadissipacao.pdf: 314304 bytes, checksum: f9fbbe437cb3821fdf97bd1baa0a1da5 (MD5) Previous issue date: 2004-11-09
- Published
- 1996
43. Elemental characterization of edible plants and soils in an abandoned mining region: assessment of environmental risk
- Author
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Gonzalez-Fernandez, O., primary, Batista, M. J., additional, Abreu, M. M., additional, Queralt, I., additional, and Carvalho, M. L., additional
- Published
- 2011
- Full Text
- View/download PDF
44. Ceria promotion of acetaldehyde photo-oxidation in a TiO2-based catalyst: a spectroscopic and kinetic study.
- Author
-
Muñoz-Batista, M. J., Ballari, M. M., Cassano, A. E., Alfano, O. M., Kubacka, A., and Fernández-García, M.
- Published
- 2015
- Full Text
- View/download PDF
45. Distribution of naturally radioactive elements (U, Th and K) in grazing land soils of the Iberian Peninsula compared with total natural radiation.
- Author
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Prazeres, C., Mártin-Mendez, I., Batista, M. J., Locutura, J., and Bel-Lan, A.
- Subjects
RADIOACTIVE elements ,PASTURES ,BACKGROUND radiation ,RADIOISOTOPES - Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2015
46. Análisis factorial de datos geoquímicos de suelos de la Península Ibérica, derivados del Proyecto GEMAS (Eurogeosurveys).
- Author
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Martín-Méndez, I., Prazeres, C., Locutura, J., Batista, M. J., and Bel-lan, A.
- Abstract
Copyright of Comunicaçõe Geológicas is the property of Laboratorio Nacional de Energia e Geologia, I.P. and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
- Published
- 2015
47. Effect of g-C3N4 loading on TiO2-based photocatalysts: UV and visible degradation of toluene.
- Author
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Muñoz-Batista, M. J., Kubacka, A., and Fernández-García, M.
- Published
- 2014
- Full Text
- View/download PDF
48. Effect of g-C3N4loading on TiO2-based photocatalysts: UV and visible degradation of tolueneElectronic supplementary information (ESI) available: Details for ea,scalculation are included. See DOI: 10.1039/c4cy00226a
- Author
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Muñoz-Batista, M. J., Kubacka, A., and Fernández-García, M.
- Abstract
g-C3N4was introduced into a highly active anatase TiO2-based photocatalyst using a simple yet effective impregnation method. The corresponding composite materials were obtained with a carbon nitride weight content ranging from 0.25 to 4 wt.%, and their surface, morphological and structural properties were characterized using BET and porosity measurements, X-ray diffraction, infrared, UV-vis and photoluminescence spectroscopy, and transmission electron microscopy. They were subsequently tested for toluene photoelimination under UV and sunlight-type illumination conditions. The photocatalytic performance of the materials was analysed quantitatively through calculation of the quantum yield of the reaction under all illumination conditions essayed. We observed that the addition of carbon nitride enhances the photoactivity and selectivity to CO2of samples containing 0.5 to 1 wt.% g-C3N4. Physicochemical characterization presented evidence that the enhanced behaviour is related to the intimate contact between the two components of the photocatalyst system, which provides two new (i.e.not present in the parent system) charge carrier handling routes affecting photocatalytic properties upon UV and visible light illumination.
- Published
- 2014
- Full Text
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49. Rhenium occurrence in Portugal: An overview considering the valorisation of mineral resources
- Author
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Silva, T. P., Oliveira, D. P. S., Batista, M. J., João Pedro Veiga, Noronha, F., and Matos, J. X.
50. Rhenium occurrence in Portugal: An overview considering the valorisation of mineral resources
- Author
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Silva, T. P., Oliveira, D. P. S., Batista, M. J., Veiga, J. P., Fernando Noronha, and Matos, J. X.
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