22 results on '"Cardelli V."'
Search Results
2. Soil affects throughfall and stemflow under Turkey oak (Quercus cerris L.)
- Author
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Corti, G., Agnelli, A., Cocco, S., Cardelli, V., Masse, J., and Courchesne, F.
- Published
- 2019
- Full Text
- View/download PDF
3. Soil bacterial communities under slash and burn in Mozambique as revealed by a metataxonomic approach
- Author
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Serrani, D., Ferrocino, I., Garofalo, C., Osimani, A., Corvaglia, M.R., Milanovic', V., Aquilanti, L., Cocco, S., Cardelli, V., Rafael, R.B.A., Franciosi, E., Tuohy, K., Clementi, F., and Corti, G.
- Subjects
Settore AGR/16 - MICROBIOLOGIA AGRARIA ,Land-use change ,Soil Science ,Agroforestry ,Soil microbiota ,16S rRNA gene sequencing ,Soil physicochemical properties - Published
- 2023
- Full Text
- View/download PDF
4. Altitude affects the quality of the water-extractable organic matter (WEOM) from rhizosphere and bulk soil in European beech forests
- Author
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De Feudis, M., Cardelli, V., Massaccesi, L., Hofmann, D., Berns, A.E., Bol, R., Cocco, S., Corti, G., and Agnelli, A.
- Published
- 2017
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- View/download PDF
5. Effect of beech (Fagus sylvatica L.) rhizosphere on phosphorous availability in soils at different altitudes (Central Italy)
- Author
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De Feudis, M., Cardelli, V., Massaccesi, L., Bol, R., Willbold, S., Cocco, S., Corti, G., and Agnelli, A.
- Published
- 2016
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- View/download PDF
6. Influence of forest management on nutrient stock (C and Pav) and earthworm fauna in chestnut woods in central Italy
- Author
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Camponi, L., Gavinelli, F., Cardelli, V., Serrani, D., Salvucci, A., Concheri, G., Nardi, S., Cocco, S., and Corti, G.
- Published
- 2022
7. Assessing geomorphological and pedological processes in the genesis of pre-desert soils from southern Tunisia
- Author
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Corti, G., primary, Cocco, S., additional, Hannachi, N., additional, Cardelli, V., additional, Weindorf, D.C., additional, Marcellini, Mirco, additional, and Agnelli, A., additional
- Published
- 2020
- Full Text
- View/download PDF
8. Small altitudinal change and rhizosphere affect the SOM light fractions but not the heavy fraction in European beech forest soil
- Author
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De Feudis, M., primary, Cardelli, V., additional, Massaccesi, L., additional, Trumbore, S.E., additional, Vittori Antisari, L., additional, Cocco, S., additional, Corti, G., additional, and Agnelli, A., additional
- Published
- 2019
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- View/download PDF
9. Data on soil physicochemical properties and chemical composition of rainfall and of throughfall and stemflow generated by Turkey oak trees (Quercus cerris L.) in acid and sub-alkaline soils
- Author
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Corti, G., primary, Agnelli, A., additional, Cocco, S., additional, Cardelli, V., additional, Masse, J., additional, and Courchesne, F., additional
- Published
- 2018
- Full Text
- View/download PDF
10. TORRE DEL CERRANO E NATURA 2000
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Vallarola, F., Cargini, D., De Ascentiis, A., Di Giandomenico, M., Zollo, A., Aretusi, G., Crocetti, C., Casareale, C., D'Andrea, R., Lombardi, A., Di Meo, C., Iachini, A., Tiscar, Pietro Giorgio, Pedicini, Silvia, Ferrara, Ermete, Gadaleta, F., DI FRANCESCO, Cristina Esmeralda, Mosca, Francesco, Mercurio, M., Cardone, F., Corriero, G., Piccirilli, R., DI GUARDO, Giovanni, Profeta, Francesca, Chiodo, E., De Nicola, M., Dimplflmeier, F., Cocco, E., Sabatino, P., Cerrano, C., Di Camillo, C. G., Pica, D., Torsani, F., Bastari, A., Corti, G., Cocco, S., Cardelli, V., Borguete Alves, R. R., Agnelli, A., and Fornasier, F.
- Published
- 2015
11. Heavy metal load and effects on biochemical properties in urban soils of a medium-sized city, Ancona, Italy
- Author
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Franco Ajmone-Marsan, Valeria Cardelli, Stefania Cocco, Dominique Serrani, Paola Adamo, Giuseppe Corti, Serrani, D., Ajmone-Marsan, F., Corti, G., Cocco, S., Cardelli, V., and Adamo, P.
- Subjects
Chromium ,China ,Environmental Engineering ,chemistry.chemical_element ,Biomass ,Zinc ,Risk Assessment ,Metal ,Soil ,Nickel ,Geochemistry and Petrology ,Soil functions ,Metals, Heavy ,Soil Pollutants ,Environmental Chemistry ,Cities ,General Environmental Science ,Water Science and Technology ,Cobalt ,Mercury ,General Medicine ,Mercury (element) ,Lead ,chemistry ,Environmental chemistry ,visual_art ,Soil water ,visual_art.visual_art_medium ,Clay ,Environmental science ,Spatial variability ,Copper ,Environmental Monitoring - Abstract
Urban soils are often mixed with extraneous materials and show a high spatial variability that determine great differences from their agricultural or natural counterparts. The soils of 18 localities of a medium-sized city (Ancona, Italy) were analysed for their main physicochemical and biological properties, and for chromium (Cr), copper (Cu), cobalt (Co), lead (Pb), nickel (Ni), zinc (Zn), and mercury (Hg) total content, distribution among particle-size fractions, and extractability. Because of the absence of thresholds defining a hot spot for heavy metal pollution in urban soils, we defined a “threshold of attention” (ToA) for each heavy metal aiming to bring out hot spot soils where it is more impellent to intervene to mitigate or avoid potential environmental concerns. In several city locations, the soil displayed sub-alkaline pH, large contents of clay-size particles, and higher TOC, total N, and available P with respect to the surrounding rural areas, joined with high contents of total heavy metals, but low availability. The C biomass, basal respiration, qCO2, and enzyme activities were compared to that detected in the near rural soils, and results suggested that heavy metals content has not substantially compromised the soil ecological services. We conclude that ToA can be considered as a valuable tool to highlight soil hot spots especially for cities with a long material history and, for a proper risk assessment in urban soils, we suggest considering the content of available heavy metals (rather than the total content) and soil functions.
- Published
- 2021
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12. Mineral weathering and lessivage affect microbial community and enzyme activity in mountain soils
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Alberto Agnelli, Giuseppe Corti, Sara Marinari, L. Vittori Antisari, Gilmo Vianello, Valeria Cardelli, Luisa Massaccesi, Gloria Falsone, Rosita Marabottini, Stefania Cocco, Dominique Serrani, Marinari S., Marabottini R., Falsone G., Vianello G., Vittori Antisari L., Agnelli A., Massaccesi L., Cocco S., Cardelli V., Serrani D., and Corti G.
- Subjects
0106 biological sciences ,Microbial bioma ,Population ,Microbial biomass ,Soil Science ,Weathering ,Pedogenic processes ,01 natural sciences ,Organic matter ,education ,Soil horizons ,chemistry.chemical_classification ,Topsoil ,education.field_of_study ,Ecology ,Illuviation ,Lessivage ,04 agricultural and veterinary sciences ,Organo-mineral interactions ,Agricultural and Biological Sciences (miscellaneous) ,Pedogenesis ,chemistry ,Environmental chemistry ,Soil water ,040103 agronomy & agriculture ,0401 agriculture, forestry, and fisheries ,Pedogenic processe ,Organo-mineral interaction ,Clay minerals ,010606 plant biology & botany - Abstract
The aim of the study was to assess if pedogenic processes such as mineral weathering and lessivage, other than organic matter accumulation, can affect soil microbial population and enzyme activities. This study examines six soil profiles located in a karst region of the North-Eastern Italian Alps and characterized by a vertical textural differentiation due to lessivage. For each soil, four pedological layers were recognized according to the dominant soil forming process: i) the top soil (Tp layer), formed by A and AB horizons, characterized by organic matter accumulation; ii) the subsurface eluviated layer (Elu layer), comprising AE and EB horizons; iii) the layer dominated by the in-situ mineral weathering (Wh layer), made by Bw horizons; iv) the deepest layer (Ls), subjected to clay illuviation and comprised by Bt horizons. In the upper layers (Tp and Elu), because of the low pH, weathering also occurred, as indicated by the presence of disordered smectite and by the high values of pedogenic Fe oxi-hydroxides to pseudo-total Fe ratio. The microbial biomass content and structure, and the enzyme activities significantly differed in the four pedological layers. The amount of microbial biomass was, as expected, most abundant in the Tp layer, where bacteria and actinomycetes abounded. Conversely, in Elu and Wh we observed a fungal-to-bacterial biomass ratio significantly higher than in Tp and Ls; in Elu, also the gram (+)/gram (−) ratio was the highest. In the upper layer, the interaction between enzymes and minerals like disordered smectite and pedogenic Fe-oxides appeared as responsible for the inhibition of the total enzyme activity per unit of organic C, and of the lipase activity. In Ls layer, where clay illuviation and high organo-minerals interaction occurred, the potential hydrolysis of organic matter was low, as revealed by the SEI/TOC ratio, the reduced lipase activity, and the inhibited activity of α-fucosidase and α-mannosidase. Even if the activity of most enzymes depends on the substrate availability, which decreases with soil depth, those involved in lipid degradation displayed the maximum activities in Elu and Wh layers, where a relative increase of the fungal population was observed. In conclusion, our findings showed that the soil functionality, expressed by the microbial community structure and enzymes activity, can vary according to organic matter–mineral interaction following the weathering and lessivage gradients along the soil profiles.
- Published
- 2021
13. Role of land set-up systems on soil (physicochemical) conditions
- Author
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Stefania Cocco, Valeria Cardelli, Giuseppe Corti, Giuseppe Lo Papa, Rogério Borguete Alves Rafael, Carmelo Dazzi, Dominique Serrani, Cocco S., Cardelli V., Corti G., Serrani D., Rafael R.B.A., Dazzi C., and Lo Papa G.
- Subjects
soil fertility ,lcsh:S ,Land reclamation ,Agricultural engineering ,soil erosion ,lcsh:Plant culture ,Land reclamation, soil erosion, soil fertility, soilscape, time of concentration ,soilscape ,Set (abstract data type) ,lcsh:Agriculture ,Settore AGR/14 - Pedologia ,Environmental science ,time of concentration ,lcsh:SB1-1110 ,Agronomy and Crop Science - Abstract
Land reclamation and drainage networks represent one of the most ancient human modifications of the Italian soilscape, where tailored land set-up systems were developed in agro- and forestecosystems in three millennia of man’s activity. Most of once manually maintained land settings are currently scarcely working or even disappeared because of the cost needed for their maintenance and the advent of mechanization that have simplified the field organization. The scarce attention to the soil experienced in the last decades, has accelerated soil erosion and flooding events, which entailed high costs in terms of money and human lives, but also caused reduction of soil thickness, water holding capacity, and fertility. In view of a sustainable agriculture, it is mandatory to assess the role of land set-up systems, which for centuries have been key in protecting soil from erosion, but also in increasing soil fertility. Such an effort cannot be made without considering the different pedo-climatic conditions and land uses of the Italian territory, which is different with respect to the past because of the multiple transformations made to favour the mechanization of agriculture. In this review we discuss the main effect of Italian land settings on the soilscape and on soil physicochemical conditions. Since land settings were developed centuries ago, detailed information about their effect on specific soil parameters is scarce in the scientific literature; thus, in some case, we provide information gathered in places where land set-up systems are still present. Highlights - Land set-up systems increase soil fertility. - Land set-up systems reduce incidence and seriousness of flooding events. - Land set-up systems need improvement for forest ecosystems. - Each soilscape needs its own land set-up system.
- Published
- 2020
14. Altitude affects the quality of the water-extractable organic matter (WEOM) from rhizosphere and bulk soil in European beech forests
- Author
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Diana Hofmann, Stefania Cocco, Anne E. Berns, Giuseppe Corti, Valeria Cardelli, Roland Bol, Alberto Agnelli, M. De Feudis, Luisa Massaccesi, DE FEUDIS, MAURO, Cardelli, V., MASSACCESI, LUISA, Hofmann, D., Berns, A. E., Bol, R., Cocco, S., Corti, G., and AGNELLI, Alberto
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010504 meteorology & atmospheric sciences ,Mountain soils ,Bulk soil ,Soil Science ,01 natural sciences ,Fagus sylvatica ,Climate change ,Organic matter ,Mountain soil ,Beech ,0105 earth and related environmental sciences ,chemistry.chemical_classification ,Rhizosphere ,biology ,Chemistry ,Soil organic matter ,04 agricultural and veterinary sciences ,biology.organism_classification ,Humus ,Polyphenolic compound ,Agronomy ,Labile soil C pool ,Soil water ,040103 agronomy & agriculture ,0401 agriculture, forestry, and fisheries ,ESI FT-ICR MS ,Labile soil C pool, Mountain soils, Polyphenolic compounds, ESI FT-ICR MS, Climate change ,Polyphenolic compounds - Abstract
Water-extractable organic matter (WEOM) is the most dynamic and bioavailable fraction of the soil organic matter pool. Although the litter floor is considered the main source of WEOM, roots also release a great amount of labile organic compounds through rhizodeposition processes. This makes the rhizosphere, the small soil volume in proximity to the roots, a soil compartment relatively enriched in WEOM. Since both the rhizosphere and the labile organic C pool are highly sensitive to the environmental conditions we evaluated the characteristics of WEOM from rhizosphere and bulk soil collected from the A horizons of European beech (Fagus sylvatica L.) forest soils of Apennines mountains (central Italy) at two altitudes (800 and 1000 m), using elevation as a proxy for temperature change. Specifically, we tested if i) the rhizosphere contains higher amounts of WEOM with a greater diversity of compounds with respect to the bulk soil, and ii) this effect is more pronounced at higher altitude. At both 800 m and 1000 m above sea level, the main distinction between WEOM from rhizosphere and bulk soil was the larger amounts of sugars in the soil close to the roots. Further, our results indicated an influence of altitude on rhizospheric processes as suggested by the larger concentrations of organic C and soluble phenols, and richness of tannins in the rhizosphere WEOM than in the bulk soil at 1000 m. We attributed this influence to environmental constraints which enhanced the release of labile organics and secondary metabolites by rhizodeposition and humification processes in the rhizosphere. As a whole, our data draw a picture where the roots are able to affect the characteristics of WEOM and environmental constraints enhance the differentiation between rhizosphere and bulk soil. This view confirms the influence of the rhizosphere on the soil C cycle, and the importance of the rhizospheric processes when environmental conditions become harsher.
- Published
- 2017
15. Effect of beech (Fagus sylvatica L.) rhizosphere on phosphorous availability in soils at different altitudes (central Italy)
- Author
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Luisa Massaccesi, Stefania Cocco, Roland Bol, Sabine Willbold, Valeria Cardelli, Alberto Agnelli, Giuseppe Corti, M. De Feudis, DE FEUDIS, MAURO, Cardelli, V., MASSACCESI, LUISA, Bol, R., Willbold, S., Cocco, S., Corti, G., and AGNELLI, Alberto
- Subjects
0106 biological sciences ,Mountain soils ,Bulk soil ,Soil Science ,01 natural sciences ,Water extractable organic matter ,Nutrient ,Altitude ,Fagus sylvatica ,Botany ,Climate change ,Organic matter ,Available P ,Mountain soil ,Beech ,Mountain soils, Rhizosphere effect, Available P, Soil phosphatase activities, Water extractable organic matter, Climate change ,chemistry.chemical_classification ,Rhizosphere ,biology ,Soil phosphatase activities ,04 agricultural and veterinary sciences ,biology.organism_classification ,Soil phosphatase activitie ,Agronomy ,chemistry ,Soil water ,040103 agronomy & agriculture ,0401 agriculture, forestry, and fisheries ,Environmental science ,Rhizosphere effect ,010606 plant biology & botany - Abstract
Phosphorus (P) is an important nutrient for plant growth but its availability in soil is limited. Although plants are able to respond to the P shortage, climatic factors might modify the soil-plant-microorganisms system and reduce P availability. In this study we evaluated the rhizosphere effect of beech (Fagus sylvatica L.) in forest soils of Apennines mountains (central Italy) at two altitudes (800 and 1000 m) and along 1° of latitudinal gradient, using latitude and altitude as proxies for temperature change. Specifically, we tested if 1) soil organic C, total N, and organic and available P decrease with increasing latitude and altitude, and 2) the rhizosphere effect on P availability becomes more pronounced when potential nutrient limitations are more severe, as it happens with increasing latitude and altitude. The results showed that the small latitudinal gradient has no effect on soil properties. Conversely, significant changes occurred between 800 and 1000 m above sea level, as the soils at higher altitude showed greater total organic C (TOC) content, organic and available P contents, and alkaline mono-phosphatases activity than the soils at lower altitude. Further, at the higher altitude, a marked rhizosphere effect was detected, as indicated by greater concentration of TOC, water extractable organic C, and available P, and its fulfillment was mainly attributed to the release of labile organics through rhizodeposition. The availability of easy degradable compounds in the rhizosphere should foster the mineralization of the organic matter with a consequent increase of available P. Hence, we speculate that at high altitude the energy supplied by the plants through rhizodeposition to the rhizosphere heterotrophic microbial community is key for fuelling the rhizospheric processes and, in particular, P cycling.
- Published
- 2016
16. Producing agri-food derived composts from coffee husk as primary feedstock at different temperature conditions.
- Author
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Hoseini M, Cocco S, Casucci C, Cardelli V, Ruello ML, Serrani D, and Corti G
- Subjects
- Agriculture, Manure, Italy, Soil chemistry, Fertilizers analysis, Hydrogen-Ion Concentration, Animals, Coffee, Temperature, Composting methods
- Abstract
There is a great global concern about agricultural wastes from food and feed crop processing that have significant environmental impacts. Composting is the most environmentally friendly, cost-effective, and efficient processes that can solve the problems of accumulation and toxicity of agricultural waste. The aim of this study is the detoxification of coffee husk by composting at two temperature conditions ("warm" and "cold"). In the greenhouse, the ambient temperature was changed day by day to mimic the situation of a spring to summer "warm" period (≈16-34 °C) and a spring "cold" period (≈7-20 °C) typical of central Italy. The coffee industry should accept the responsibility for the large amount of organic waste production, which presents toxicity and mass accumulation problems. Coffee husk as the main raw material is not used directly as bio-fertilizer in agriculture sector due to the leaching of phenolic compounds and high pH value. The brewing industry is famous for its mass production, and the brewer residues as a by-product have an extremely acidic pH that makes them an unsuitable material for direct composting, but the mixture of these materials can optimize pH. The addition of cow manure accelerates microbial activity and is a strategy to improve composting rate and maturity. The following mixtures were tested: coffee husk and brewer spent grains in a proportion of 2:1 (Compost 1), coffee husk and cow manure in a proportion of 4:1 (Compost 2), and coffee husk, brewer spent grain, and cow manure in a proportion of 5:3:2 (Compost 3). Quality and maturity of the final composts appeared to be affected by the ambient temperature conditions, which remarkably affected pH, C/N ratio, nutrient and trace elements availability, germination index, microbial biomass carbon, and FDA hydrolysis. Results showed that both sets of temperatures produced composts to be considered standard compost, but "warm" conditions compost showed greater maturity, while the composts produced under "cold" conditions were able to increase seed gemination., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2024 Elsevier Ltd. All rights reserved.)
- Published
- 2025
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17. Short term effects of digestate and composted digestate on soil health and crop yield: Implications for sustainable biowaste management in the bioenergy sector.
- Author
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Gurmessa B, Cocco S, Ashworth AJ, Udawatta RP, Cardelli V, Ilari A, Serrani D, Fornasier F, Del Gatto A, Pedretti EF, and Corti G
- Subjects
- Carbon, Fertilizers analysis, Nitrogen analysis, Soil, Composting
- Abstract
Composting mitigates environmental risks associated with using solid digestate as fertilizer. However, evidence is lacking on benefits of using composted digestate as fertilizer in enhancing soil health and increasing agronomic yield compared to non-composted digestate (hereafter, digestate). A field study was conducted consisting of digestate, composted digestate, co-composted digestate with biogas feedstocks (corn [Zea mays L.] silage, poultry litter, corn silage + poultry litter or food processing by-product), inorganic nitrogen fertilizer, and control (no treatment applied) on soil microbial biomass, enzyme activities (EA), soil organic carbon (SOC), bioavailable P (P), total nitrogen (TN), soil health index (SHI), and sunflower (Helianthus annuus L.) yield. The Partial Least Square Path Model (PLS-PM) was used to predict: 1) nutrient cycling in response to changes in microbial growth and EA and 2) agronomic yield in response to SHI and soil nutrients dynamics. Composted digestate had equivalent soil health benefits with most of co-composted materials and digestate, albeit agronomic yield was greatest with composted digestate, which was 40 % and 100 % greater than with inorganic nitrogen fertilizer and digestate, respectively, indicating composted digestate's potential to replace the synthetic N fertilizer. Moreover, composts from a sole digestate, rather than the ones from co-composted with fresh feedsstocks, can be promising organic amendments and fertilizers for growing sunflower. The PLS-PM model identified that triggered microbial biomass growth and EA, following digestate and composted digestate applications, catalyzed organic matter decomposition, resulting in enhanced nutrients contents and soil health. However, the model revealed that improved SHI did not predict agronomic yield, as opposed to P and TN, suggesting agronomic performance may have been more sensitive to changes in specific soil nutrients status than the overall soil health condition. We conclude that the benefits of composted digestate as fertilizer hint the significance of digestate valorization via post-digestate composting and compost utilization for sustainability of the bioenergy sector., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2023 Elsevier B.V. All rights reserved.)
- Published
- 2024
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18. Holm oak (Quercus ilex L.) cover: A key soil-forming force in controlling C and nutrient stocks in long-time coppice-managed forests.
- Author
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Camponi L, Cardelli V, Cocco S, Serrani D, Salvucci A, Cutini A, Agnelli A, Fabbio G, Bertini G, Roggero PP, Weindorf DC, and Corti G
- Subjects
- Ecosystem, Forests, Minerals, Trees, Soil chemistry, Quercus
- Abstract
In forest ecosystems, soil-plant interactions drive the physical, chemical, and biological soil properties and, through soil organic matter cycling, control the dynamics of nutrient cycles. Parent material also plays a fundamental role in determining soil's chemical properties and nutrient availability. In this study, eight long-time coppice-managed Holm oak forests under conversion to high forest, located under similar climatic conditions in Tuscany and Sardinia Regions (Italy), and grown on soils developed from three different lithologies (limestone, biotite granite, and granite with quartz veins) were evaluated. The research aimed to a) estimate the amount of C and nutrients (total N and potentially available P, Ca, Mg, and K) stored both in the organic, organo-mineral, and mineral horizons and at fixed depth intervals (0-0.3 and 0.3-0.5 m), and b) assess the dominant pedological variables driving elemental accumulation. The soils were described and sampled by genetic horizons and each sample was analyzed for its C and nutrient concentration in both the fine earth and skeleton fractions. Despite the different parent materials from which the soils had evolved, the physicochemical properties and the C and nutrient stocks for the 0-0.3 and 0.3-0.5 m layers did not show substantial differences among the eight soils. Conversely, some differences were observed in the stocks of potentially available P and Ca per 0.01 m of mineral horizons. The findings show that over time, plant-induced pedogenic processes (acidification, mineral weathering, organic matter addition, and nutrient cycling) almost obliterated the influence of parent materials on soil properties. This resulted in the upper soil horizons that showed similar characteristics, even though derived from different lithologies. However, among the study sites, some differences occurred due to lithology, as in the case of the soils derived from calcareous parent materials that had high concentrations of exchangeable Ca in the mineral horizons and, likely, to environmental variables (e.g., exposure), which possibly influenced litter degradation and the release of nutrients such as N and available P., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2023 Elsevier Ltd. All rights reserved.)
- Published
- 2023
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19. Soil fertility in slash and burn agricultural systems in central Mozambique.
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Serrani D, Cocco S, Cardelli V, D'Ottavio P, Rafael RBA, Feniasse D, Vilanculos A, Fernández-Marcos ML, Giosué C, Tittarelli F, and Corti G
- Subjects
- Agriculture methods, Carbon, Charcoal, Chlorides, Fluorides, Humans, Middle Aged, Mozambique, Nitrates, Nitrogen, Phosphorus Compounds, Sand, Soil chemistry, Ammonium Compounds, Burns
- Abstract
Slash and burn is a land use practice widespread all over the world, and nowadays it is formally recognized as the principal livelihood system in rural areas of South America, Asia, and Africa. The practice consists of a land rotation where users cut native or secondary forest to establish a new crop field and, in some cases, build charcoal kilns with the cut wood to produce charcoal. Due to several socio-economic changes in developing countries, some scientists and international organizations have questioned the sustainability of slash and burn since in some cases, crop yield does not justify the soil degradation caused. To estimate the soil quality in agricultural and forest soils at different ages of the forest-fallow period (25, 35, and 50 years), this survey investigated rural areas in three locations in Manica province, central Mozambique: Vanduzi, Sussundenga, and Macate. Soil profiles were trenched and sampled with a pedological approach under crop fields and forest-fallow. The chronosequence was selected to test the hypothesis that the increase in forest-fallow age causes an improvement of soil fertility. Results highlighted discrete variations among locations in mineralogy, Al- and Fe-oxyhydroxides, sand, silt, pH, total organic carbon, humic carbon, total nitrogen, available phosphorous, chloride, nitrate, fluoride, and ammonium. Few differences in mineralogy, Fe-oxyhydroxides, available P, chloride, and nitrate were detected between crop fields and forest-fallow within the same location. Such differences were mostly ascribed to intrinsic fertility inherited from the parent material rather than a longer forest-fallow period. However, physicochemical soil property improvement did not occur under a forest age of 50 years (the longest forest-fallow considered), indicating that harmonization of intrinsic fertility and agronomic practices may increase soil organic matter and nutrient contents more than a long forest-fallow period., Competing Interests: Declaration of competing interest The authors declare no competing interests., (Copyright © 2022 Elsevier Ltd. All rights reserved.)
- Published
- 2022
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20. Effect of coppice conversion into high forest on soil organic C and nutrients stock in a Turkey oak (Quercus cerris L.) forest in Italy.
- Author
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Camponi L, Cardelli V, Cocco S, Serrani D, Salvucci A, Cutini A, Agnelli A, Fabbio G, Bertini G, Roggero PP, and Corti G
- Subjects
- Carbon analysis, Ecosystem, Forests, Italy, Minerals, Nutrients, Quercus, Soil
- Abstract
In forest ecosystems, a variety of abiotic and biotic soil forming factors drives soil organic matter (SOM) and nutrients cycling with a profitable outcome on climate change mitigation. As a consequence, type and intensity of forest management, through its impact on carbon (C) and nutrient soil stocks, can be considered as an additional soil forming force. In this study, we investigated the influence of the coppice conversion into high forest on pedogenesis and on soil C and nutrient (N, P, Ca, Mg, and K) stocks, fifty years later the beginning of the conversion-cycle. The trial was established in a Turkey oak forest historically managed under the coppice system in central Italy. Specifically, we considered tree population density (natural evolution - control, moderate thinning, heavy thinning) where soil samples were collected according to genetic horizon to estimate C, N, and P stocks both in the forest floor and at fixed depth intervals (0-30, 30-50 and 50-75 cm). Further, the stocks of exchangeable Ca, Mg, and K were also assessed for the mineral layers. The results showed that litter and the upper layer of mineral soil (0-30 cm) contained a similar quantity of C (about 74-83 Mg ha
-1 ), independently of the trials and no differences were observed also in the whole soil stocks (about 192-213 Mg ha-1 ). The comparison of the mean stocks calculated per 1-cm of thickness of organic (O), organo-mineral (OM), and mineral (M) layers, although it did not display any difference among trials (excepted for P and Mg), showed a similar capability of the organo-mineral horizons to store C and nutrients compared with the organic ones (e.g., about 6-12 Mg ha-1 , 0.3-0.5 Mg ha-1 and 0.5-1.5 kg ha-1 for C, N and P, respectively). Our findings showed that thinning operated on Turkey oak coppice did not affect soil capacity to store C and nutrients. These results suggested that the forest ecosystem itself is the main soil forming force and this is consistent with the target of adopting forest management able to control the global C cycle through the storage of SOM in the mineral soil rather than in forest floor, where SOM turnover is faster., (Copyright © 2022 Elsevier Ltd. All rights reserved.)- Published
- 2022
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21. Post-digestate composting benefits and the role of enzyme activity to predict trace element immobilization and compost maturity.
- Author
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Gurmessa B, Cocco S, Ashworth AJ, Foppa Pedretti E, Ilari A, Cardelli V, Fornasier F, Ruello ML, and Corti G
- Subjects
- Fertilizers analysis, Silage, Soil, Composting, Trace Elements
- Abstract
The current study evaluated the quality of agricultural waste digestate by composting or co-composting with biogas feedstock (maize silage, food processing waste, or poultry litter). Temperature, phytotoxicity, C/N ratio, water extractable trace elements, and 14 enzyme activities were monitored. Temperature dropped earlier in digestate and maize silage co-composting pile, reducing time to maturity by 20 days. Composting and co-composting reduced phytotoxicity and C/N ratio, but increased immobilization of Al, Ba, Fe, Zn, and Mn at least by 40% in all piles. All the enzyme activities, except arylsulfatase and α-glucosidase, increased at the maturity phase and negatively correlated with organic matter content and most of trace elements. Post-digestate composting or co-composting with biogas feedstock is a promising strategy to improve digestate quality for fertilizer use, and selected enzyme activities can be indicators of compost maturity and immobilization of trace elements., (Copyright © 2021 Elsevier Ltd. All rights reserved.)
- Published
- 2021
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22. Manure anaerobic digestion effects and the role of pre- and post-treatments on veterinary antibiotics and antibiotic resistance genes removal efficiency.
- Author
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Gurmessa B, Pedretti EF, Cocco S, Cardelli V, and Corti G
- Subjects
- Anaerobiosis, Drug Resistance, Microbial drug effects, Genes, Bacterial drug effects, Anti-Bacterial Agents pharmacology, Manure
- Abstract
This review was aimed to summarize and critically evaluate studies on removal of veterinary antibiotics (VAs), antibiotic resistance genes (ARGs) and mobile genetic elements (MGEs) with anaerobic digestion (AD) of manure and demonstrate areas of focus for improved removal efficiency. The environmental risks associated to the release of the same were also critically evaluated. The potential of AD and advanced AD of manure on removal rate of VAs, ARGs and MGEs was thoroughly assessed. In addition, the role of post and pre-AD treatments and their potential to support VAs and ARGs removal efficiency were evaluated. The overall review results show disparity among the different groups of VAs in terms of removal rate with relatively higher efficiency for β-lactams and tetracyclines compared to the other groups. Some of sulfonamides, fluoroquinolones and macrolides were reported to be highly persistent with removal rates as low as zero. Within group differences were also reported in many literatures. Moreover, removal of ARGs and MGEs by AD was widely reported although complete removal was hardly possible. Even in rare scenarios, some AD conditions were reported to increase copies of specific groups of the genes. Temperature pretreatments and temperature phased advanced AD were also reported to improve removal efficiency of VAs while contributing to increased biogas production. Moreover, a few studies also showed the possibility of further removal by post-AD treatments such as liquid-solid separation, drying and composting. In conclusion, the various studies revealed that AD in its current technological level is not a guarantee for complete removal of VAs, ARGs and MGEs from manure. Consequently, their possible release to the soils with digestate could threaten the healthcare and disturb soil microbial ecology. Thus, intensive management strategies need to be designed to increase removal efficiency at the different manure management points along the anaerobic digestion process., (Copyright © 2020 Elsevier B.V. All rights reserved.)
- Published
- 2020
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