40 results on '"Corella, J. P."'
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2. Characterising the heterogeneous nature of tufa mounds by integrating petrographic, petrophysical, acoustic and electromagnetic measurements.
- Author
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Schröder, S., Corella, J. P., Pellicer, X. M., Rook, P., Kara, A., and Comas, X.
- Subjects
ELECTROMAGNETIC measurements ,ACOUSTIC measurements ,GROUND penetrating radar ,TUFAS ,SPEED of sound ,LATERAL loads - Abstract
Determination of the physical properties of subsurface geological bodies is essential for georesource management and geotechnical applications. In the absence of direct measurements, this usually passes via geophysical methods such as seismic and ground‐penetrating radar. These require conversion to physical properties, and measurements at different scales to test for consistency. This approach is non‐trivial in geobodies with heterogeneous patterns of properties. Tufa mounds—in‐situ terrestrial carbonate buildups precipitating from geothermal waters—are characterised by high contrasts in facies and petrophysical properties from microscale to macroscale, and are therefore ideally suited to test the ability of non‐invasive geophysical methods to estimate such contrasts, and to develop petrophysical models based on geophysical properties. Here, a laboratory‐based study of a Pleistocene tufa mound in Spain is presented that combines (1) petrography, (2) digital 2D pore network analysis, (3) gas porosity and permeability measurements, (4) acoustic velocity measurements and (5) electromagnetic wave velocity and porosity determination from ground‐penetrating radar, to develop empirical petrophysical models. These results show the consistency of petrophysical properties determined with different methods across various observational scales. Electromagnetically derived porosity positively correlates with gas porosity. Petrophysical properties depend on measurable rock fabric parameters and the degree of cementation, which provide predictive tools for subsurface geobodies. Strongly cemented peloidal‐thrombolitic fabrics with intergranular and intercrystalline pores, and a dominance of small complex pores best transmit acoustic waves. Weak cementation and a significant fraction of large simple pores (framework, vegetation moulds) increase porosity and permeability of shrubby fabrics, while causing lower acoustic velocity. This study demonstrates that ground‐penetrating radar models can be used in combination with direct measurements of physical subsurface properties to capture highly contrasting physical properties associated with different sedimentary facies that would not be achievable with other methods, thus improving the understanding of formational processes. [ABSTRACT FROM AUTHOR]
- Published
- 2024
- Full Text
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3. Three millennia of heavy rainfalls in Western Mediterranean: frequency, seasonality and atmospheric drivers
- Author
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Corella, J. P., Valero-Garcés, B. L., Vicente- Serrano, S. M., Brauer, A., and Benito, G.
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- 2016
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4. Sediment dynamics in the subaquatic channel of the Rhone delta (Lake Geneva, France/Switzerland)
- Author
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Corella, J. P., Arantegui, A., Loizeau, J. L., DelSontro, T., le Dantec, N., Stark, N., Anselmetti, F. S., and Girardclos, S.
- Published
- 2014
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5. Spatial heterogeneity of benthic methane dynamics in the subaquatic canyons of the Rhone River Delta (Lake Geneva)
- Author
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Sollberger, S., Corella, J. P., Girardclos, S., Randlett, M.-E., Schubert, C. J., Senn, D. B., Wehrli, B., and DelSontro, T.
- Published
- 2014
- Full Text
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6. Métodos de datación en sedimentos cuaternarios con laminación anual: Ejemplos de la Península Ibérica.
- Author
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Corella, J. P. and Martín-Puertas, C.
- Subjects
HOLOCENE Epoch ,VARVES ,LAKE sediments ,PENINSULAS ,SEDIMENTS ,LAMINATED materials - Abstract
Copyright of Cuaternario y Geomorfología is the property of Cuaternario y Geomorfologia 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
- 2022
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7. Holocene atmospheric iodine evolution over the North Atlantic
- Author
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Corella, J. P., Maffezzoli, N., Cuevas, C. A., Vallelonga, P., Spolaor, A., Cozzi, G., Müller, J., Vinther, B., Barbante, C., Kjær, H. A., Edwards, R., Saiz-Lopez, A., Corella, J. P., Maffezzoli, N., Cuevas, C. A., Vallelonga, P., Spolaor, A., Cozzi, G., Müller, J., Vinther, B., Barbante, C., Kjær, H. A., Edwards, R., and Saiz-Lopez, A.
- Abstract
Atmospheric iodine chemistry has a large influence on the oxidizing capacity and associated radiative impacts in the troposphere. However, information on the evolution of past atmospheric iodine levels is restricted to the industrial period while its long-term natural variability remains unknown. The current levels of iodine in the atmosphere are controlled by anthropogenic ozone deposition to the ocean surface. Here, using high-resolution geochemical measurements from coastal eastern Greenland ReCAP (REnland ice CAP project) ice core, we report the first record of atmospheric iodine variability in the North Atlantic during the Holocene (i.e., the last 11 700 years). Surprisingly, our results reveal that the highest iodine concentrations in the record were found during the Holocene Thermal Maximum (HTM; ∼ 11 500–5500 years before-present). These high iodine levels could be driven by marine primary productivity resulting in an Early Holocene “biological iodine explosion”. The high and stable iodine levels during this past warm period are a useful observational constraint on projections of future changes in Arctic atmospheric composition and climate resulting from global warming.
- Published
- 2019
8. Spatial heterogeneity of benthic methane dynamics in the subaquatic canyons of the Rhone River Delta (Lake Geneva)
- Author
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Sollberger, S., primary, Corella, J. P., additional, Girardclos, S., additional, Randlett, M.-E., additional, Schubert, C. J., additional, Senn, D. B., additional, Wehrli, B., additional, and DelSontro, T., additional
- Published
- 2013
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9. Sediment dynamics in the subaquatic channel of the Rhone delta (Lake Geneva, France/Switzerland)
- Author
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Corella, J. P., primary, Arantegui, A., additional, Loizeau, J. L., additional, DelSontro, T., additional, le Dantec, N., additional, Stark, N., additional, Anselmetti, F. S., additional, and Girardclos, S., additional
- Published
- 2013
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10. A multi-proxy perspective on millennium-long climate variability in the Southern Pyrenees
- Author
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Morellón, M., primary, Pérez-Sanz, A., additional, Corella, J. P., additional, Büntgen, U., additional, Catalán, J., additional, González-Sampériz, P., additional, González-Trueba, J. J., additional, López-Sáez, J. A., additional, Moreno, A., additional, Pla-Rabes, S., additional, Saz-Sánchez, M. Á., additional, Scussolini, P., additional, Serrano, E., additional, Steinhilber, F., additional, Stefanova, V., additional, Vegas-Vilarrúbia, T., additional, and Valero-Garcés, B., additional
- Published
- 2012
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11. A multi-proxy perspective on millennium-long climate variability in the Southern Pyrenees
- Author
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Morellón, M., primary, Pérez-Sanz, A., additional, Corella, J. P., additional, Büntgen, U., additional, Catalán, J., additional, González-Sampériz, P., additional, González-Trueba, J. J., additional, López-Sáez, J. A., additional, Moreno, A., additional, Pla, S., additional, Saz-Sánchez, M. Á., additional, Scussolini, P., additional, Serrano, E., additional, Steinhilber, F., additional, Stefanova, V., additional, Vegas-Vilarrúbia, T., additional, and Valero-Garcés, B., additional
- Published
- 2011
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12. A multi-proxy perspective on millennium-long climate variability in the Southern Pyrenees.
- Author
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Morellón, M., Pérez-Sanz, A., Corella, J. P., Büntgen, U., Catalán, J., González-Sampériz, P., González-Trueba, J. J., López-Sáez, J. A., Moreno, A., Pla, S., Saz-Sánchez, M. Á., Scussolini, P., Serrano, E., Steinhilber, F., Stefanova, V., Vegas-Vilarrúbia, T., and Valero-Garcés, B.
- Abstract
A review of selected, well-dated, multiproxy paleoclimatic records (lacustrine, dendrochronological, geomorphological) characterizes the main environmental changes occurred in the Southern Pyrenees during the last millennium. Warmer and relatively arid conditions prevailed during the Medieval Climate Anomaly (MCA, < 1300 AD), with a significant development of xerophytes and Mediterranean vegetation and limited deciduous tree formations (mesophytes). The Little Ice Age (LIA, 1300-1800 AD) was generally colder and moister, with an expansion of deciduous taxa and cold-adapted mountainous conifers. Two major phases occurred within this period: (i) a transition MCA-LIA, characterized by fluctuating, moist conditions and relatively cold temperatures (ca. 1300 and 1600 AD); - (ii) a second period, characterized by coldest conditions and higher humidity, coinciding with maximum (recent) glacier advances (ca. 1600-1850 AD). After the LIA a warming and more arid phase started coinciding with glacier retreat, and interrupted by a short-living cooling episode during the late 19th to early 20th centuries. Some records suggest a response to solar activity with colder and slightly moister conditions during solar minima. Centennial-scale hydrological fluctuations are in phase with reconstructions of NAO variability, which appears to be the main forcing for humidity in the region during the last millennium. [ABSTRACT FROM AUTHOR]
- Published
- 2011
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13. Catalytic Hot Gas Cleaning with Monoliths in Biomass Gasification in Fluidized Beds. 3. Their Effectiveness for Ammonia Elimination
- Author
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Corella, J., Toledo, J. M., and Padilla, R.
- Abstract
Biomasses with relatively high N contents generate a gasification gas with a NH
3 content between 500 and 6000 ppm, with 2000 ppm of NH3 as the value that can be selected as a reference. This NH3 would generate NOx contents above the legally accepted limits; this is the reason why very often NH 3 has to be removed from a gasification gas that also contains tar and particulates. The present paper only focuses on the performance of Ni-based monoliths for NH3 elimination from a realistic gasification gas coming from a bubbling-fluidized-bed biomass gasifier, at small pilot-plant scale. Besides using NH3 conversions, analysis of the results was also made using effective kinetic constants (keff ) not only for NH3 but also for the simultaneous and competitive tar removal reaction. Correlations were found between the keff,NH 3 and keff,tar values, included in effective Sherwood numbers, and the Reynolds and Schmidt numbers, the pitch of the channels of the monolith, and the temperature. The effect of the temperature is of the potential type, not Arrhenius, with an exponent of 2.75 ± 1.75, because of the control by the external mass transfer. keff,NH 3 is also somewhat smaller (0.8 ± 0.3) than the equivalent one for tar elimination (keff,tar ). Data on the deactivation of the monoliths, their causes, and their possible solutions are also provided. A final discussion on the poor performance of these monoliths in biomass gasification in a fluidized bed is also included in this paper.- Published
- 2005
14. Catalytic Hot Gas Cleaning with Monoliths in Biomass Gasification in Fluidized Beds. 2. Modeling of the Monolithic Reactor
- Author
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Corella, J., Toledo, J. M., and Padilla, R.
- Abstract
Nickel-containing monoliths can be used to eliminate tar and ammonia in a real biomass gasification gas. They can work with a fuel gas containing important amounts of particulates, as in the case of the fuel gas produced in fluidized-bed gasifiers. The use of monoliths is a very recent and promising technology that has not yet reached a commercial level and requires experimental studies at pilot scale. Those studies indicate that tar and ammonia conversions (eliminations) with these monoliths depend on so many experimental variables that a model is needed to understand and correlate the results obtained with these monolithic reactors. A model is developed in this paper for the monolithic reactor that has two very different zones: the gas reheating zone and the monolith itself. The model is developed according to the basic rules of chemical reaction engineering, and it includes two microkinetic models for the tar and NH
3 elimination reactions, mass balances for tar and NH3 , and a heat balance in the monolith. Several important facts appear and are confirmed in this study, such as the control of the external mass transfer in the channels of the monolith, which generates a dependence of the overall kinetic constants on the temperature of potential, not Arrhenius, type. The ΔT across the monolith is also analyzed in detail. The equations developed for the model are easy to handle, allow a correct analysis of experimental data, and may be used to design new monolithic reactors for this application.- Published
- 2004
15. On the Modeling of the Kinetics of the Selective Deactivation of Catalysts. Application to the Fluidized Catalytic Cracking Process
- Author
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Corella, J.
- Abstract
The deactivation of a solid catalyst may affect in different ways each reaction taking place in a complex network. This creates a variation with time on stream of the product distribution at the reactor exit. To handle data from this common situation, a selective deactivation kinetic model fits the data much better than a nonselective one. Selective deactivation kinetic models are scarcely used because they are often complex and difficult to handle. They also introduce more deactivation kinetic parameters than the nonselective models. Nevertheless, selective deactivation kinetic models are a refinement and are a step forward in the modeling of deactivation kinetics. They might also improve the existing macrokinetic models for commercial reactors. In this paper, several new concepts and ideas are given relating to selective deactivation kinetic models. These concepts are applied to the kinetics of the deactivation of commercial fluidized catalytic cracking catalysts with commercial feedstocks. It is also proven how the kinetics of cracking of the feedstock (heavy oils) is much more affected by the catalyst deactivation than the cracking of the gasoline. A discussion of the results is included.
- Published
- 2004
16. Catalytic Hot Gas Cleaning with Monoliths in Biomass Gasification in Fluidized Beds. 1. Their Effectiveness for Tar Elimination
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Corella, J., Toledo, J. M., and Padilla, R.
- Abstract
Full-size 15 × 15 × 30 cm nickel-based monoliths are tested for tar elimination in fuel gas produced by biomass gasification in a fluidized bed at a small pilot-plant scale. The feedstocks used were mixtures of pine wood chips and orujillo, the residue from olive oil production. Temperatures at the front or face of the monolith ranged from 820 to 956 °C, gas hourly space velocities in the monolith ranged from 1280 to 4550 h-1 (normal conditions, nc), area velocities ranged from 2.7 to 7.1 m/h, and superficial or face gas velocities at the inlet of the monolith ranged from 0.34 to 1.3 m/s. Samples of gas and tar were taken before and after the monolith reactor, and variations in gas composition and tar content were determined. Using a macrokinetic model presented elsewhere, some key kinetic constants for the tar-removal reaction are calculated for the monolith and used as indexes of its activity. The effects of some important operating conditions on the activity and sometimes on the deactivation of the monolith are presented here. The intrinsic activity of the monolith for tar abatement is finally compared with those of other competing catalysts such as dolomites and commercial steam-reforming catalysts. It is concluded that these monoliths are not very high in activity, but they can operate with a fuel gas containing particulates, thereby avoiding the use of hot filters, which are problematic when used in biomass gasification.
- Published
- 2004
17. Two Advanced Models for the Kinetics of the Variation of the Tar Composition in Its Catalytic Elimination in Biomass Gasification
- Author
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Corella, J., Caballero, M. A., Aznar, M.-P., and Brage, C.
- Abstract
Biomass gasification in fluidized beds generates tar that can be effectively eliminated with catalysts located downstream from the biomass gasifier. Some previously obtained results from such catalytic tar elimination were hard to be understood because the tar was considered as only one or two lumps. For this reason, in this work, tar is considered in two ways: (i) as being composed of six different lumps and (ii) as a continuous mixture. For these studies, tar was sampled before and after two catalytic beds located in a slip-flow downstream from a fluidized-bed gasifier (pilot scale). Such tar samples were then completely characterized, and the tar composition was thus determined before and after the catalytic bed. The conversion of each of the species present in tar, and thus of the lumps, was calculated at different temperatures and space-times in the catalytic reactor. The two most advanced reaction networks and their corresponding kinetic models are presented here. The first one provides the evolution with gas residence time of the mean molecular weight of the tar and of the variance of the tar molecular weight distribution. The second kinetic model is based on a set of six kinetic equations and eleven kinetic constants, which are calculated here. This second model allows the species present in tar to be ranked according to their reactivity or resistance to being destroyed. Predictions from these models are consistent with all existing data on this matter.
- Published
- 2003
18. Improving the Modeling of the Kinetics of the Catalytic Tar Elimination in Biomass Gasification
- Author
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Corella, J., Toledo, J. M., and Aznar, M.-P.
- Abstract
A single one-lump first-order reaction for the catalytic elimination of tar present in the flue gas from biomass-fluidized bed gasifiers is not good enough for some applications. A new and more advanced reacting network and microkinetic model has been generated and is here presented. It is based on two lumps, the more and the less reactive tar species, and has four kinetic constants. Each lump reacts (disappears) by both catalytic and thermal reactions. The microkinetic model is applied to results obtained at around 840 °C and at small pilot plant level with two very different solids: silica sand and a commercial (ICI 46-1) nickel-based steam-reforming catalyst. The values found for the four kinetic constants are self-consistent, fit well the results, and mean a clear step forward in the modeling of the catalytic tar abatement.
- Published
- 2002
19. Testing Total Oxidation Catalysts for Gas Cleanup in Waste Incineration at Pilot Scale
- Author
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Corella, J. and Toledo, J. M.
- Abstract
Seven different total oxidation catalysts (PRO*CLEAN*500; EF 258 H/D; Siemens A; ZERONOX; and Ru, Pd, and V
2 O5 on a TiO2 support) have been tested for abatement of principal organic hazardous compounds (POHCs) in the flue gas from a waste incinerator of the fluidized-bed type. These catalysts were placed in a slip flow downstream from the waste incinerator. The catalytic reactors used were both metallic and glass, made for monoliths and for particulates. The temperatures used in the catalytic reactors ranged from 240 to 510 °C, and the volumetric gas hourly space velocities (GHSVs) ranged from 1200 to 5700 [(mgas,normal conditions 3/h)/mcatalyst 3]. The catalysts operated under a realistic flue gas, which was sampled before and after the catalytic reactor at different times on stream. Condensates after the catalytic reactor were also analyzed for organics and for compounds sometimes lost from the catalyst. Gas sampling and analysis were carried out using standarized methods. Conversions (destructions) of most of the POHCs were 99.99%, but small GHSV values were required. Experimental conditions for an even more refined catalyst comparison are also provided.- Published
- 2002
20. Biomass Gasification with Air in Fluidized Bed. Hot Gas Cleanup with Selected Commercial and Full-Size Nickel-Based Catalysts
- Author
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Caballero, M. A., Corella, J., Aznar, M.-P., and Gil, J.
- Abstract
Three selected commercial, full-size steam-reforming catalysts for naphthas, BASF G1-50, ICI 46-1, and Topsøe R-67, are tested at pilot-scale level for hot gas cleanup in biomass gasification in a fluidized bed. Gas composition and tar content in the flue gas are measured before and after the catalytic bed. Variations of the catalytic bed in H
2 , CO, CO2 , CH4 , and H2 O contents are reported for different operating conditions. Tar conversions and an apparent first-order kinetics constant for the overall tar removal reaction are calculated. Tar contents at the exit of the catalytic reactor as low as 10 mg/mn 3 are obtained in a test of 50 h-on-stream without noticeable catalyst deactivation. Important variations in tar conversion with space time in the catalytic bed, with H2 O/C* in the flue gas, and with the equivalence ratio in the upstream gasifier are observed. These results obtained at the pilot-scale level and with the use of full-sized commercial catalysts are an important forward step in demonstrating the technical feasibility of the overall biomass gasification process.- Published
- 2000
21. Biomass Gasification with Air in Fluidized Bed: Reforming of the Gas Composition with Commercial Steam Reforming Catalysts
- Author
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Corella, J., Orio, A., and Aznar, P.
- Abstract
Four commercial catalysts for steam reforming of higher hydrocarbons (naphthas) and three for steam reforming of light hydrocarbons are tested for hot gas clean up and upgrading in biomass gasification with air in fluidized bed. The catalysts used originate from four manufacturers: BASF AG, ICI-Katalco, Haldor Topsoe a/s, and United Catalysts Inc. The work is performed in a small pilot plant (1−2 kg of biomass fed/h) with three reactors in series: gasifier, guard bed of dolomite, and full flow catalytic bed. Samples of gas are taken before and after the catalytic bed at different times-on-stream. It is shown how the H
2 , CO, CO2 , CH4 and steam contents in the flue gas change because of the catalytic bed approaching contents near to the ones corresponding to the equilibrium state. Variations in the heating value of the gas and gas yield as a result of the catalytic bed are also reported.- Published
- 1998
22. Biomass Gasification with Air in a Fluidized Bed: Effect of the In-Bed Use of Dolomite under Different Operation Conditions
- Author
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Gil, J., Caballero, M. A., Martin, J. A., Aznar, M.-P., and Corella, J.
- Abstract
The performance of a biomass gasifier, fluidized-bed type, is improved by in-bed use of calcined dolomite. Tar contents in the raw flue gas below 1 g/m
n 3 are obtained by using a bed with a percentage between 15 and 30 wt % of dolomite (the rest being silica sand). The work is carried out at small pilot-plant scale (10 kg of biomass/h) with equivalence ratios (ER) between 0.20 and 0.35 and temperatures of 800−840 °C in the gasifier bed. To replace the eroded and elutriated dolomite (from the gasifier bed), an amount of dolomite (0.40−0.63 mm) is continuously fed, mixed with the biomass at 3 wt %. When the results obtained with in-bed dolomite are compared to the ones gained in a gasifier bed without dolomite, change of the following variables is reported: gas composition and its corresponding heating value, gas and char yields, apparent thermal efficiency, and tar contents. Once the usefulness of the in-bed use of dolomite is established, three main operation variables (ER and temperatures of the gasifier bed and freeboard) are studied in the improved gasifier. Carryover of solids from the gasifier also increases when calcined dolomite is used because of its softness. Elutriation rate constants are calculated for several operational parameters. - Published
- 1999
23. Fresh Tar (from a Biomass Gasifier) Elimination over a Commercial Steam-Reforming Catalyst. Kinetics and Effect of Different Variables of Operation
- Author
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Narvaez, I., Corella, J., and Orio, A.
- Abstract
The upgrading of the raw gas from a biomass gasifier is studied with the commercial steam-reforming BASF G1-25 S nickel-based catalyst. It is located downstream of the gasifier, a bubbling fluidized bed type in which air is used as gasifying agent. To increase the catalyst lifetime, a guard bed of a calcined dolomite at 800−850 °C is used. It decreases the throughput of tar entering the catalytic bed to amounts below 2 g tar/m3(NC). This work is focused only on the catalytic bed which easily decreases the tar content in the gas to only 1−2 mg/m3(NC). Variables studied include the particle diameter of the catalyst, time-on-stream, temperature of the catalytic bed, and gas and tar compositions. Both tar and gas compositions in the catalytic (Ni) reactor depend on the equivalence and H/C ratios existing in the gasifier and on the operating conditions of the guard bed of dolomite. A simple kinetic model is used to describe the overall tar elimination network. Its overall kinetic constant is used as index of the catalyst activity for tar elimination. Values of this overall kinetic constant are given for very different operating conditions.
- Published
- 1997
24. Calcined Dolomite, Magnesite, and Calcite for Cleaning Hot Gas from a Fluidized Bed Biomass Gasifier with Steam: Life and Usefulness
- Author
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Delgado, J., Aznar, M. P., and Corella, J.
- Abstract
Calcined dolomites, limestones, and magnesites are active and inexpensive solids for cleaning raw hot gas from biomass gasifiers with steam. The variations of their activities with time-on-stream are studied here. Simultaneous coke formation and coke elimination by steam gasification increases the life of these naturally occurring catalysts under some circumstances. The lives of these solids are studied at different temperatures (800−880 °C), space times (0.08−0.32 kg of dolomite·h/nm3), particle diameters (1−4 mm), and types of solid. Not much deactivation was observed for tar concentration in the raw gas below 48 g/nm3, particle diameters of less than 1.9 mm, temperatures above 800 °C, and space times above 0.13 kg·h/nm3. The effectiveness of these calcined minerals is compared with that of an inert material (silica sand) and with a commercial steam reforming catalyst (R-67 from Haldor Topsøe).
- Published
- 1996
25. Biomass Gasification with Air in an Atmospheric Bubbling Fluidized Bed. Effect of Six Operational Variables on the Quality of the Produced Raw Gas
- Author
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Narvaez, I., Orio, A., Aznar, M. P., and Corella, J.
- Abstract
Biomass gasification with air in a bubbling fluidized bed is studied in a small pilot plant. Variables analyzed are equivalence ratio (from 0.20 to 0.45), temperatures of the gasifier bed (750−850 °C) and of its freeboard (500−600 °C), H/C ratio in the feed, use of secondary air (10% of the overall) in the freeboard, and addition (2−5 wt %) of a calcined dolomite mixed with the biomass used as the feedstock. Using advanced tar and gas sampling and analysis methods, the gas composition and tar content in the gas are determined and their variation with the operation parameters is given. A statistical analysis of the effects of the gasification variables is also here presented.
- Published
- 1996
26. Commercial Steam Reforming Catalysts To Improve Biomass Gasification with Steam−Oxygen Mixtures. 2. Catalytic Tar Removal
- Author
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Aznar, M. P., Caballero, M. A., Gil, J., Martin, J. A., and Corella, J.
- Abstract
Eight different commercial catalysts, nickel based, for steam reforming of naphthas and of natural gas are tested in biomass gasification for hot gas cleanup and conditioning. They were manufactured by BASF AG, ICI−Katalco, UCI, and Haldor Topsøe a/s. The catalysts were tested in a slip flow after a biomass gasifier of fluidized bed type at small pilot-plant scale (10−20 kg of biomass/h). The gasifying agent used is steam-oxygen mixtures. A guard bed containing a calcined dolomite is used to decrease the tar content in the gas at the inlet of the catalytic bed. Main variables studied are catalyst type, bed temperature, H
2 O + O2 to biomass feed ratio, and time-on-stream. All catalysts for reforming of naphthas show to be very active and useful for tar removal and gas conditioning (in biomass gasification). 98% tar removal is easily obtained with space velocities of 14 000 h-1 (n.c.). No catalysts deactivation is found in 48 h-on-stream tests when the catalyst temperature is relatively high (780−830 °C). Using a simple first-order kinetic model for the overall tar removal reaction, apparent energies of activation (of around 58 kJ/mol) and preexponential factors are obtained for the most active catalysts.- Published
- 1998
27. Commercial Steam Reforming Catalysts To Improve Biomass Gasification with Steam−Oxygen Mixtures. 1. Hot Gas Upgrading by the Catalytic Reactor
- Author
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Caballero, M. A., Aznar, M. P., Gil, J., Martin, J. A., Frances, E., and Corella, J.
- Abstract
Commercial steam reforming (nickel-based) catalysts are used for hot gas cleaning and upgrading in biomass gasification with steam−oxygen mixtures. The gasifier used was an atmospheric and bubbling fluidized bed with an internal diameter of 15 cm and a total height of 3.2 m and was continuously fed with 5−20 kg of biomass/h. Eight different catalysts from four different manufacturers (BASF AG, TOPSOE A/S, ICI, and UCI) have been tested. They were located in a downflow fixed-bed reactor of 4 cm i.d. placed in a slip flow after the gasifier. A guard bed with a calcined dolomite was also used before the catalytic bed to decrease the tar content in the raw gas below the limit of 2 g of tar/m3
n , thus avoiding the catalyst deactivation by coke formation. The main variables studied were the temperature of the catalytic bed and the gas composition in the bed. Effects concerning tar elimination will be reported in part 2 of this work. This paper is mainly devoted to characterization of catalysts and to upgrading of the flue gas. H2 and CO contents increased by 4−14 and 1−8 vol %, dry basis, respectively. CO2 , CH4 , and steam contents decreased by 0−14, 87−99, and 2−6 vol %, dry basis, respectively. Other parameters varied in the following ways: the lower heating value decreased by 0.3−1.7 MJ/m3n , gas yield increased by 0.1−0.4 m3n /kg of biomass daf, and apparent thermal efficiency increased by 1−20%. The results presented allow screening of the best catalysts to get an upgraded and useful gas in biomass gasification with steam−oxygen mixtures.- Published
- 1997
28. Biomass Gasification: Produced Gas Upgrading by In-Bed Use of Dolomite
- Author
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Olivares, A., Aznar, M. P., Caballero, M. A., Gil, J., Frances, E., and Corella, J.
- Abstract
When some calcined dolomite (OCa·OMg) is used in the bed of a biomass gasifier of fluidized bed type the raw gas produced is cleaner than when only silica sand is used in it as fluidizing medium. In-bed dolomite changes the product distribution at the gasifier exit because of in-situ catalytic reactions promoted by the calcined dolomite. Gasifying with steam−O
2 mixtures causes the tar content in the exit gas to decrease from 12 to 2−3 g tar/m3n , the H2 content to increase from 25−28 to 43 vol %, and the CO content to decrease from 45 to 27 vol % when the gas and char yields, heating value of the gas, and other main variables also undergo important changes because of the in-bed dolomite. The experimental work here reported is carried out at small pilot plant scale in a 15 cm i.d. atmospheric and bubbling fluidized bed gasifier fed by 10 kg biomass/h. Dolomite is continuously fed to the gasifier, mixed with the biomass in percentages of 2−3 wt % of the total mass flow fed. A 10 wt % of calcined dolomite in the gasifier bed is enough to significantly improve the product distribution and gas quality.- Published
- 1997
29. Performance of Different Dolomites on Hot Raw Gas Cleaning from Biomass Gasification with Air
- Author
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Orio, A., Corella, J., and Narvaez, I.
- Abstract
Calcined dolomites (CaO−MgO) from four different quarries have been tested for the upgrading of the hot raw gas from a fluidized bed gasifier of biomass with air. These calcined dolomites have big macropores (900−4000 Å) and low (3.8−12 m2/g) BET surface areas. They have been tested in a fixed bed of 6 cm i.d. downstream from the air-blown biomass gasifier. The change in gas composition (contents in H
2 , CO, CO2 , CH4 , ...), tar content, gas heating value, etc., has been studied at different temperatures (780−920 °C) as well as space-times for the gas in the bed (0.03−0.10 kg·h/m3) and the type of dolomite. Increasing the equivalence ratio used in the gasifier and decreasing the H/C ratio of the gas increases the refractoriness of the tars to be eliminated by the calcined dolomite. Activation energies (100 ± 20 kJ/mol) and preexponential factors for the overall tar elimination reaction have been calculated for the different dolomites under realistic conditions. The activity of the dolomite for tar elimination can increase by 20% on increasing its pore diameter or its Fe2 O3 content. Comparison of results with similar ones obtained in biomass gasification with steam is also presented.- Published
- 1997
30. Biomass Gasification with Steam in Fluidized Bed: Effectiveness of CaO, MgO, and CaO−MgO for Hot Raw Gas Cleaning
- Author
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Delgado, J., Aznar, M. P., and Corella, J.
- Abstract
The upgrading of the raw hot gas from a bubbling fluidized bed biomass gasifier is studied using cheap calcined minerals or rocks downstream from the gasifier. Biomass gasification is made with steam (not air) at 750−780 °C and about 0.5−1.0 kg of biomass/h. Calcined solids used are dolomite (MgO−CaO), pure calcite (CaO), and pure magnesite (MgO). Variables studied have been temperature of the secondary bed (780−910 °C), time of contact or space-time of the gas (0.08−0.32 kg·h/m3n), and particle diameter (1−4 mm) and type of mineral. Their effects on tar conversion, tar amount in the exit gas, product distribution, and gas composition are presented. Using a macrokinetic model for the tar disappearance network, the activities of the stones are expressed by their apparent kinetic constant. Apparent energies of activation for tar elimination (42−47 kJ/mol) and preexponential and effectiveness factors are given for all tested solids of which the most active is the calcined dolomite.
- Published
- 1997
31. Ultra-Fast Biomass Pyrolysis in a High-Temperature (2200° C), Fluid-Wall Reactor
- Author
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Corella, J., Monzon, A., Santamaria, J., and Gonza´lez-Can˜ibano, J.
- Abstract
The pyrolysis of pine sawdust has been carried out in a High-Temperature Fluid-Wall Reactor. This unit has been specially designed to withstand working temperatures of up to 2200° C. The biomass is fed to the top of the reactor after sieving to the appropriate size, at a rate of 1.0 to 1.8 kg/min. The feed falls and, at the same time is very quickly heated by radiation to the reaction temperature. The estimated heating rate is on the order of 106° C/s for reactant surfaces. The fluid-wall, produced by a nitrogen flow through the 30 cm diameter porous reactor core, prevents both reactants and products from reaching the reactor wall. The product distribution at the reactor exit has been determined for different operating conditions. The influence of reactor temperature, biomass feed rate, and biomass particle size on the product distribution and on the heating value of the exit gas has been investigated.
- Published
- 1988
- Full Text
- View/download PDF
32. Hot Gas Cleaning and Upgrading with a Calcined Dolomite Located Downstream a Biomass Fluidized Bed Gasifier Operating with Steam−Oxygen Mixtures.
- Author
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Pérez, P., Aznar, P. M., Caballero, M. A., Gil, J., Martín, J. A., and Corella, J.
- Published
- 1997
- Full Text
- View/download PDF
33. Sedimentological processes in the Rhone Delta subaquatic canyons (France-Switzerland)
- Author
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Arantegui, A., Corella, J. P., Loizeau, J. L., Anselmetti, F. S., Stark, N., del Sontro, T., Le Dantec, N., and Girardclos, S.
- Abstract
Deltas are very sensitive environments and highly vulnerable to variations in water discharge and the amount of suspended sediment load provided by the delta-forming currents. Human activities in the watershed, such as building of dams and irrigation ditches, or river bed deviations, may affect the discharge regime and sediment input, thus affecting delta growth. Underwater currents create deeply incised canyons cutting into the delta lobes. Understanding the sedimentary processes in these subaquatic canyons is crucial to reconstruct the fluvial evolution and human impact on deltaic environments, and to carry out a geological risk assessment related to mass movements, which may affect underwater structures and civil infractructure. Recently acquired high-resolution multibeam bathymetry on the Rhone Delta in Lake Geneva (Sastre et al. 2010) revealed the complexity of the underwater morphology formed by active and inactive canyons first described by Forel (1892). In order to unravel the sedimentary processes and sedimentary evolution in these canyons, 27 sediment cores were retrieved in the distal part of each canyon and in the canyon floor/levee complex of the active canyon. Geophysical, sedimentological, geochemical and radiometric dating techniques were applied to analyse these cores. Preliminary data show that only the canyon originating at the current river mouth is active nowadays, while the others remain inactive since engineering works in the watershed occurred. However, alternating hemipelagic and turbiditic deposits in the easternmost canyons, evidence underflow processes during the last decades. Two canyons, which are located close to the Rhone river mouth, correspond to particularly interesting deeply incised crevasse channels formed when the underwater current broke through the outer bend of a meander in the proximal northern levee. In these canyons, turbidites were observed in the sediment record indicating ongoing sediment dynamics during whether extreme flood events or mass-movements due to deltaic scarp failures. The active canyon shows a classic turbiditic system with frequent spillover processes in the canyon floor/levee complex. Geotechnical measurements, a decrease in the frequency of turbidites and a fining upward sequence along the levee suggest that erosion dominates sedimentation in the canyon floor, while sedimentation dominates in the rapid levee building-up process, with sedimentation rates that exceed 2.5 cm/yr in the proximal areas. Therefore, mechanisms controlling the sedimentary evolution on the active canyon represent a complex interplay between erosion and sedimentation.
34. Searching the Rhone delta channel in Lake Geneva since François Alphonse FOREL
- Author
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Girardclos, S., Hilbe, M., Corella, J. P., Loizeau, J. -L, Katrina Kremer, Delsontro, T., Arantegui, A., Moscariello, A., Arlaud, F., Akhtman, Y., Anselmetti, F. S., and Lemmin, U.
- Subjects
ddc:333.7-333.9 ,Submersible ,Underflow ,Rhone delta ,ddc:550 ,Canyon ,Lake Geneva ,Multibeam bathymetry ,Léman ,Channel - Abstract
In the late 19th century, F.A. FOREL led investigations of the Rhone River delta area of Lake Geneva that resulted in the discovery of a textbook example of a river-fed delta system containing impressive subaquatic channels. Well ahead of the marine counterparts, scientific observations and interpretations of water currents shaping the delta edifice for the first time documented how underflow currents carry cold, suspension-laden waters from the river mouth all the way to the deep basin. These early investigations of the Rhone delta laid the basis for follow-up studies in the 20th and 21th centuries. Sediment coring, water-column measurements, manned submersible diving, seismic reflection profiling and bathymetric surveying eventually provided a rich database to unravel the key erosional and depositional processes, further documenting the impact of human-induced changes in the catchment. With the merging of old and new scientific knowledge, today a comprehensive understanding prevails of how a delta changes through time, how its channels are formed, and what potential natural hazards may be related to its evolution. New and efficient bathymetric techniques, paired with novel coring operations, provided a time-series of morphologic evolution showing and quantifying the high dynamics of the delta/channel evolution in an unprecedented temporal and spatial resolution. Future investigations will continue to further quantify these dynamic processes and to link the evolution of the subaquatic domain with changes and processes in the catchment and with natural hazards. Its size, easy access, and large variety of states and processes will continue to make the Rhone delta area a perfect ‘laboratory' in which general processes can be studied that could be upscaled or downscaled to other marine and lacustrine deltas.
35. Triggering mechanisms and geomorphological implications of debris flows in subaquatic canyons: The Rhone delta (Lake Geneva, Switzerland, France)
- Author
-
Corella, J. P., Loizeau, J. L., Hilbe, M., Le Dantec, N., Sastre, V., Anselmetti, F. S., Stark, N., del Sontro, T., and Girardclos, S.
- Abstract
Subaquatic canyons in deltas are major pathways for the transport of particles from rivers / the upper delta slops to the deep basins. They represent active environments with frequent deltaic failures and massmovements potentially bearing hazard-related (tsunami waves) and economic (infrastructure damages) implications. Understanding sedimentary processes and mass-movement triggering mechanisms is crucial to assess related consequences and to carry out geological risk assessments. The Rhone River delta in Lake Geneva (Switzerland, France) is a complex underwater structure with several active and inactive subaquatic canyons, similar to marine deltas but at a smaller scale. The difference between two bathymetric surveys in 1986 and 2002 revealed an inversion in the topography of the distal active canyon, as a former distal canyon was transformed into a mound-like structure. A 12 m-thick layer was deposited in the canyon and modified the sediment transfer conduit. Sediment cores from this deposit were retrieved in-situ in 2002 and 2011 via the “F.-A. Forel” and Russian MIR submersibles, respectively. These cores contained a homogeneous, sandy material. Its sediment texture, grain-size, high density and shear strength, and low water content suggests that it corresponds to a debris-flow deposit that possibly took place after the initiation of a mass movement due to a scarp failure in proximal areas of the canyon. In addition, in situ geotechnical tests on the modern canyon floor have shown a soft top layer above a stiffer substratum. This soft layer, which increases in thickness towards distal areas, may act as a basal surface for hydroplaning, and might have allowed the debrite to be transported 9 km away from the source of the scarp failure. Similarities in textures and grain-size of the debris flow and levee deposits hint at the proximal northern levee as the source of this material. Rapid sediment loading in this area, at the rate of >2.5cm/yr, steep slopes in the canyon walls and increased pore pressure due to high methane concentrations may have reduced the stability of the canyon wall in this area. Discrete sandy intervals show very high methane concentrations and thus could correspond to potentially weak layers prone to scarp failures. Nevertheless, the probable cause for the 2000 AD Rhone delta event was an exceptional flood in October 2000 which undercut the slope, and subsequently decreased the stability by increasing the shear stress and triggered the mass failure in the already unstable canyon walls. Besides economic and hazard-related implications, such mass failures represent significant and underestimated causes in morphological evolution of underwater canyons by damming the channel and, eventually, forming short-term meanders susceptible to further erosion, as seen in a recent multibeam bathymetric map obtained in 2012.
36. Sedimentary processes and triggering mechanisms of debris flows in subaquatic canyons in Rhone delta (Lake Geneva, Switzerland, France)
- Author
-
Corella, J. P., Loizeau, J. L., Le Dantec, N., Sastre, V., Anselmetti, F. S., Stark, N., del Sontro, T., and Girardclos, S.
- Abstract
Subaquatic canyons in deltas are major pathways for the transport of particles from land to the deep basins. They represent active environments with frequent deltaic failures and mass-movement deposits potentially leading to hazardous (tsunami waves) and economic (infrastructure damages) implications. Understanding sedimentary processes and mass-movement triggering mechanisms is crucial to assess related consequences and to carry out geological risk assessments. The Rhone River delta in Lake Geneva (Switzerland, France) is a complex underwater structure with several active and inactive subaquatic canyons, similar to marine deltas but at a smaller scale. The difference between two bathymetric surveys in 1986 and 2002 revealed an inversion in the topography of the distal active canyon, as a former distal canyon was transformed into a mound-like structure. A 12 m-thick layer was deposited in the canyon and modified the sediment transfer conduit. Sediment cores from this deposit were retrieved in-situ in 2002 and 2011 via the "F.-A. Forel" and Russian MIR submersibles, respectively. These cores contained a homogeneous, sandy material. Its sediment texture, grain-size, high density and shear strength, and low water content suggests that it corresponds to a debris-flow deposit that possibly took place after the initiation of a mass movement due to a scarp failure in proximal areas of the canyon. In addition, in-situ geotechnical tests on the modern canyon floor have shown a soft top layer above a stiffer substratum. This soft layer, which increases in thickness towards distal areas, may act as a basal surface for hydroplaning, and might have allowed the debrite to be transported ~9 km away from the source of the scarp failure. Similarities in textures and grain-size of the debris flow and levee deposits hints at proximal northern levee as the source of this material. Rapid sediment loading in this area, at the rate of >3cm/yr, steep slopes in the canyon walls and increased pore pressure due to high methane concentrations may have reduced the stability of the canyon wall in this area. Discrete sandy intervals show very high methane concentrations and thus could correspond to potentially weak layers prone to scarp failures. Nevertheless, the probable cause for the 2000 AD Rhone delta event was an exceptional flood in October 2000 which undercut the slope, and subsequently decreased the stability by increasing the shear stress and triggered the mass failure in the already unstable canyon walls. Besides economic and hazardous implications, such mass failures represent significant and underestimated causes in morphological evolution of underwater canyons by damming the channel and, eventually, forming short-term meanders susceptible to further erosion.
37. ChemInform Abstract: Metal‐Mediated Addition of Carbon Dioxide to the Activated Benzene in (Cr(η4‐C6H6)(CO)3)2‐.
- Author
-
CORELLA, J. A. II and COOPER, N. J.
- Abstract
The benzene ligand in the complex (I) can be activated toward electrophiles by potassium naphthalenide reduction to the dianionic η4‐benzene complex (II).
- Published
- 1990
- Full Text
- View/download PDF
38. Antarctic ozone hole modifies iodine geochemistry on the Antarctic Plateau
- Author
-
Jean-Francois Lamarque, Elena Barbaro, Carlos A. Cuevas, Douglas E. Kinnison, Clara Turetta, Kitae Kim, Fabrizio de Blasi, Paul Vallelonga, Francois Burgay, Alfonso Saiz-Lopez, Massimo Frezzotti, Rafael P. Fernandez, J.P. Corella, Andrea Spolaor, Carlo Barbante, European Commission, National Science Foundation (US), Consejo Nacional de Investigaciones Científicas y Técnicas (Argentina), Universidad Nacional de Cuyo, Agencia Nacional de Promoción Científica y Tecnológica (Argentina), Korea Polar Research Institute, Ministero dell'Istruzione, dell'Università e della Ricerca, Spolaor, A., Burgay, F., Fernandez, R. P., Turetta, C., Cuevas, C. A., Kim, K., Kinnison, D. E., Lamarque, J. -F., de Blasi, F., Barbaro, E., Corella, J. P., Vallelonga, P., Frezzotti, M., Barbante, C., and Saiz-Lopez, A.
- Subjects
Cryospheric science ,Ozone ,Atmospheric chemistry ,010504 meteorology & atmospheric sciences ,Science ,General Physics and Astronomy ,010501 environmental sciences ,Atmospheric sciences ,01 natural sciences ,General Biochemistry, Genetics and Molecular Biology ,Geochemical cycle ,Article ,TROPOSPHERE ,Ozone hole ,chemistry.chemical_compound ,Ice core ,CHEMISTRY ,Element cycles ,Ozone layer ,Marine ecosystem ,14. Life underwater ,MOLECULAR-IODINE ,EMISSIONS ,0105 earth and related environmental sciences ,Multidisciplinary ,EAST ANTARCTICA ,iodine ,General Chemistry ,Snowpack ,Ozone depletion ,SNOW ACCUMULATION ,BROMINE ,VARIABILITY ,chemistry ,13. Climate action ,Antarctica ,Environmental science ,SEA-ICE ,DOME-C - Abstract
9 pags., 3 figs., Polar stratospheric ozone has decreased since the 1970s due to anthropogenic emissions of chlorofluorocarbons and halons, resulting in the formation of an ozone hole over Antarctica. The effects of the ozone hole and the associated increase in incoming UV radiation on terrestrial and marine ecosystems are well established; however, the impact on geochemical cycles of ice photoactive elements, such as iodine, remains mostly unexplored. Here, we present the first iodine record from the inner Antarctic Plateau (Dome C) that covers approximately the last 212 years (1800-2012 CE). Our results show that the iodine concentration in ice remained constant during the pre-ozone hole period (1800-1974 CE) but has declined twofold since the onset of the ozone hole era (~1975 CE), closely tracking the total ozone evolution over Antarctica. Based on ice core observations, laboratory measurements and chemistry-climate model simulations, we propose that the iodine decrease since ~1975 is caused by enhanced iodine re-emission from snowpack due to the ozone hole-driven increase in UV radiation reaching the Antarctic Plateau. These findings suggest the potential for ice core iodine records from the inner Antarctic Plateau to be as an archive for past stratospheric ozone trends., This project received funding from the European Union’s Horizon 2020 Research and Innovation program under grant agreement no. 689443 via project iCUPE (Integrative and Comprehensive Understanding on Polar Environments), part of the European Commission (ERA-PLANET) and by the “Programma Nazionale per la Ricerca in Antartide” (PNRA, project number PNRA16_00295). This study also received funding from the European Research Council Executive Agency under the European Union’s Horizon 2020 Research and Innovation programme (Project ‘ERC-2016-COG 726349 CLIMAHAL’). NCAR is sponsored by the National Science Foundation under Grant Number 1852977. R.P.F. would like to express thanks for the financial support from CONICET-UNCuyo (SIIP-06/M111) and ANPCyT (PICT 2015-0714). This research was also supported by the Korea Polar Research Institute (KOPRI) project (PE20030) and by the Grant to Department of Science, Roma Tre University (MIUR-Italy Dipartimenti di Eccellenza)
- Published
- 2022
39. Recent and historical pollution legacy in high altitude Lake Marboré (Central Pyrenees): A record of mining and smelting since pre-Roman times in the Iberian Peninsula.
- Author
-
Corella JP, Sierra MJ, Garralón A, Millán R, Rodríguez-Alonso J, Mata MP, de Vera AV, Moreno A, González-Sampériz P, Duval B, Amouroux D, Vivez P, Cuevas CA, Adame JA, Wilhelm B, Saiz-Lopez A, and Valero-Garcés BL
- Abstract
We have analyzed potential harmful trace elements (PHTE; Pb, Hg, Zn, As and Cu) on sediment cores retrieved from lake Marboré (LM) (2612 m a.s.l, 42°41'N; 0° 2'E). PHTE variability allowed us to reconstruct the timing and magnitude of trace metal pollutants fluxes over the last 3000 years in the Central Pyrenees. A statistical treatment of the dataset (PCA) enabled us to discern the depositional processes of PHTE, that reach the lake via direct atmospheric deposition. Indeed, the location of LM above the atmospheric boundary layer makes this lake an exceptional site to record the long-range transport of atmospheric pollutants in the free troposphere. Air masses back-trajectories analyses enabled us to understand the transport pathways of atmospheric pollutants while lead isotopic analyses contributed to evaluate the source areas of metal pollution in SW Europe during the Late Holocene. PHTE variability, shows a clear agreement with the main exploitation phases of metal resources in Southern Europe during the Pre-Industrial Period. We observed an abrupt lead enrichment from 20 to 375 yrs CE mostly associated to silver and lead mining and smelting practices in Southern Iberia during the Roman Empire. This geochemical data suggests that regional atmospheric metal pollution during the Roman times rivalled the Industrial Period. PHTE also increased during the High and Late Middle Ages (10-15
th centuries) associated to a reactivation of mining and metallurgy activities in high altitude Pyrenean mining sites during climate amelioration phases. Atmospheric mercury deposition in the Lake Marboré record mostly reflects global emissions, particularly from Almadén mines (central Spain) and slightly fluctuates during the last three millennia with a significant increase during the last five centuries. Our findings reveal a strong mining-related pollution legacy in alpine lakes and watersheds that needs to be considered in management plans for mountain ecosystems as global warming and human pressure effects may contribute to their future degradation., 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 © 2020 Elsevier B.V. All rights reserved.)- Published
- 2021
- Full Text
- View/download PDF
40. Trace metal enrichment during the Industrial Period recorded across an altitudinal transect in the Southern Central Pyrenees.
- Author
-
Corella JP, Saiz-Lopez A, Sierra MJ, Mata MP, Millán R, Morellón M, Cuevas CA, Moreno A, and Valero-Garcés BL
- Published
- 2018
- Full Text
- View/download PDF
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