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1. Water pressure head and temperature impact on isoxaflutole degradation in crop residues and loamy surface soil under conventional and conservation tillage management.

Author

Alletto L, Coquet Y, Bergheaud V, and Benoit P

Subjects
Isoxazoles chemistry, Kinetics, Minerals metabolism, Pesticide Residues chemistry, Pesticide Residues metabolism, Conservation of Natural Resources methods, Crops, Agricultural metabolism, Isoxazoles metabolism, Pressure, Soil chemistry, Temperature, Water
Abstract

Laboratory incubations were performed in order to evaluate the dissipation of the proherbicide isoxaflutole in seedbed layer soil samples from conventional and conservation tillage systems and in maize and oat residues left at the soil surface under conservation tillage. The effects of temperature and water pressure head on radiolabelled isoxaflutole degradation were studied for each sample for 21d. Mineralisation of isoxaflutole was low for all samples and ranged from 0.0% to 0.9% of applied (14)C in soil samples and from 0.0% to 2.4% of applied (14)C in residue samples. In soil samples, degradation half-life of isoxaflutole ranged from 9 to 26h, with significantly higher values under conservation tillage. In residue samples, degradation half-life ranged from 3 to 31h, with significantly higher values in maize residues, despite a higher mineralisation and bound residue formation than in oat residues. Whatever the sample, most of the applied (14)C remained extractable during the experiment and, after 21d, less than 15% of applied (14)C were unextractable. This extractable fraction was composed of diketonitrile, benzoic acid derivative and several unidentified metabolites, with one of them accounting for more than 17% of applied (14)C. This study showed that tillage system design, including crop residues management, could help reducing the environmental impacts of isoxaflutole., (Copyright © 2012 Elsevier Ltd. All rights reserved.)

Published
2012
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2. Variability of retention process of isoxaflutole and its diketonitrile metabolite in soil under conventional and conservation tillage.

Author

Alletto L, Benoit P, Bergheaud V, and Coquet Y

Subjects
Adsorption, Avena chemistry, Avena growth & development, Avena metabolism, Biodegradation, Environmental, Herbicides metabolism, Isoxazoles metabolism, Nitriles metabolism, Sulfones metabolism, Zea mays chemistry, Zea mays growth & development, Zea mays metabolism, Agriculture methods, Herbicides chemistry, Isoxazoles chemistry, Nitriles chemistry, Soil chemistry, Sulfones chemistry
Abstract

Background: Sorption largely controls pesticide fate in soils because it influences its availability for biodegradation or transport in the soil water. In this study, variability of sorption and desorption of isoxaflutole (IFT) and its active metabolite diketonitrile (DKN) was investigated under conventional and conservation tillage., Results: According to soil samples, IFT K(D) values ranged from 1.4 to 3.2 L kg(-1) and DKN K(D) values ranged from 0.02 to 0.17 L kg(-1) . Positive correlations were found between organic carbon content and IFT and DKN sorption. IFT and DKN sorption was higher under conservation than under conventional tillage owing to higher organic carbon content. Under conservation tillage, measurements on maize and oat residues collected from the soil surface showed a greater sorption of IFT on plant residues than on soil samples, with the highest sorbed quantities measured on maize residues (K(D) ≈ 45 L kg(-1) ). Desorption of IFT was hysteretic, and, after five consecutive desorptions, between 72 and 89% of the sorbed IFT was desorbed from soil samples. For maize residues, desorption was weak (<50% of the sorbed IFT), but, after two complementary desorptions allowing for IFT hydrolysis, DKN was released from maize residues., Conclusion: Owing to an increase in organic carbon in topsoil layers, sorption of IFT and DKN was enhanced under conservation tillage. Greater sorption capacities under conservation tillage could help in decreasing DKN leaching to groundwater., (Copyright © 2012 Society of Chemical Industry.)

Published
2012
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3. Pedotransfer functions for isoproturon sorption on soils and vadose zone materials.

Author

Moeys J, Bergheaud V, and Coquet Y

Subjects
Absorption, Models, Statistical, Herbicides chemistry, Models, Chemical, Phenylurea Compounds chemistry, Soil chemistry, Soil Pollutants chemistry
Abstract

Background: Sorption coefficients (the linear K(D) or the non-linear K(F) and N(F)) are critical parameters in models of pesticide transport to groundwater or surface water. In this work, a dataset of isoproturon sorption coefficients and corresponding soil properties (264 K(D) and 55 K(F)) was compiled, and pedotransfer functions were built for predicting isoproturon sorption in soils and vadose zone materials. These were benchmarked against various other prediction methods., Results: The results show that the organic carbon content (OC) and pH are the two main soil properties influencing isoproturon K(D) . The pedotransfer function is K(D) = 1.7822 + 0.0162 OC(1.5) - 0.1958 pH (K(D) in L kg(-1) and OC in g kg(-1)). For low-OC soils (OC < 6.15 g kg(-1)), clay and pH are most influential. The pedotransfer function is then K(D) = 0.9980 + 0.0002 clay - 0.0990 pH (clay in g kg(-1)). Benchmarking K(D) estimations showed that functions calibrated on more specific subsets of the data perform better on these subsets than functions calibrated on larger subsets., Conclusion: Predicting isoproturon sorption in soils in unsampled locations should rely, whenever possible, and by order of preference, on (a) site- or soil-specific pedotransfer functions, (b) pedotransfer functions calibrated on a large dataset, (c) K(OC) values calculated on a large dataset or (d) K(OC) values taken from existing pesticide properties databases., (Copyright © 2011 Society of Chemical Industry.)

Published
2011
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4. Effect of urban waste compost application on soil near-saturated hydraulic conductivity.

Author

Schneider S, Coquet Y, Vachier P, Labat C, Roger-Estrade J, Benoit P, Pot V, and Houot S

Subjects
Carbon analysis, Nitrogen analysis, Organic Chemicals analysis, Porosity, Seeds, Sewage chemistry, Soil analysis, Water analysis
Abstract

Compost application tends to increase soil fertility and is likely to modify soil hydrodynamic properties by acting on soil structural porosity. Two composts, a municipal solid waste compost (MSW) and a co-compost of green wastes and sewage sludge (SGW), have been applied every other year for 6 yr to cultivated plots located on a silt loam soil in the Parisian Basin, France. Four soil zones were defined in the topsoil after plowing: the plowpan located at the base of the plowed layer, compacted (Delta) or noncompacted (Gamma) zones located within the plowed layer, and interfurrows created by plowing and containing a large quantity of crop residues together with the recently-applied compost. To assess the effect of compost application on the near-saturated soil hydraulic conductivity, infiltration rates were measured using a tension disc infiltrometer at three water pressure potentials -0.6, -0.2, and -0.05 kPa in the various zones of the soil profile. Compost addition decreased K((sat)) in the interfurrows after plowing by almost one order of magnitude with average values of 5.6 x 10(-5) m.s(-1) in the MSW plot and 4.1 x 10(-5) m.s(-1) in the SGW plot, against 2.2 x 10(-4) m.s(-1) in the control plot. This effect had disappeared 6 mo after plowing when the average K((sat)) in the control plot had decreased to 1.9 x 10(-5) m.s(-1) while that in the compost-amended plots remained stable.

Published
2009
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5. Temperature and water pressure head effects on the degradation of the diketonitrile metabolite of isoxaflutole in a loamy soil under two tillage systems.

Author

Alletto L, Benoit P, Bergheaud V, and Coquet Y

Subjects
Adsorption, Biodegradation, Environmental, Ecology methods, Humic Substances, Hydrostatic Pressure, Isoxazoles analysis, Poaceae metabolism, Temperature, Agriculture, Herbicides analysis, Nitriles analysis, Soil analysis, Soil Pollutants analysis, Sulfones analysis
Abstract

Laboratory studies were conducted to evaluate the effects of temperature and water pressure head on the degradation of the diketonitrile metabolite (DKN) of isoxaflutole during 84d in samples collected in a loamy soil under conventional (CT) and conservation (MT) tillage systems. Soil temperature was the major factor controlling DKN degradation in the two tillage systems. The shortest half-lives (T(1/2)) were measured in the seedbed samples under MT at 25 degrees C and -33cm water pressure head. We found that mouldboard ploughing under CT was responsible for the spatial variability of herbicide degradation properties, whereas under MT herbicide degradation was associated to the vertical distribution of organic matter.

Published
2008
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6. Impact of rainfall intensity on the transport of two herbicides in undisturbed grassed filter strip soil cores.

Author

Pot V, Simůnek J, Benoit P, Coquet Y, Yra A, and Martínez-Cordón MJ

Subjects
Diffusion, Poaceae, Porosity, Herbicides analysis, Models, Chemical, Phenylurea Compounds analysis, Rain, Soil analysis, Triazines analysis
Abstract

Two series of displacement experiments with isoproturon and metribuzin herbicides were performed on two undisturbed grassed filter strip soil cores, under unsaturated steady-state flow conditions. Several rainfall intensities (0.070, 0.147, 0.161, 0.308 and 0.326 cm h(-1)) were used. A water tracer (bromide) was simultaneously injected in each displacement experiment. A descriptive analysis of experimental breakthrough curves of bromide and herbicides combined with a modeling analysis showed an impact of rainfall intensity on the solute transport. Two contrasting physical non-equilibrium transport processes occurred. Multiple (three) porosity domains contributed to flow at the highest rainfall intensities, including preferential flow through macropore pathways. Macropores were not active any longer at intermediate and lowest velocities, and the observed preferential transport was described using dual-porosity-type models with a zero or low flow in the matrix domain. Chemical non-equilibrium transport of herbicides was found at all rainfall intensities. Significantly higher estimated values of degradation rate parameters as compared to batch data were correlated with the degree of non-equilibrium sorption. Experimental breakthrough curves were analyzed using different physical and chemical equilibrium and non-equilibrium transport models: convective-dispersive model (CDE), dual-porosity model (MIM), dual-permeability model (DP), triple-porosity, dual permeability model (DP-MIM); each combined with both chemical instantaneous and kinetic sorption.

Published
2005
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7. Spatial variability in 14C-herbicide degradation in surface and subsurface soils.

Author

Charnay MP, Tuis S, Coquet Y, and Barriuso E

Subjects
Biodegradation, Environmental, Carbon Radioisotopes, Half-Life, Pesticide Residues, Soil Microbiology, Time Factors, Atrazine chemistry, Herbicides chemistry, Phenylurea Compounds chemistry, Soil analysis, Triazines chemistry
Abstract

The spatial variability in mineralization of atrazine, isoproturon and metamitron in soil and subsoil samples taken from a 135-ha catchment in north France was studied. Fifty-one samples from the top layer were taken to represent exhaustively the 31 agricultural fields and 21 soil types of the catchment. Sixteen additional samples were collected between depths of 0.7 and 10 m to represent the major geological materials encountered in the vadose zone of the catchment. All these samples were incubated with 14C-labelled atrazine under laboratory conditions at 28 degrees C. Fourteen selected surface samples which exhibited distinctly different behaviour for atrazine dissipation (including sorption and mineralization) were incubated with 14C-isoproturon and 14C-metamitron. Overall soil microbial activity and specific herbicide degradation activities were monitored during the incubations through measurements of total carbon dioxide and 14C-carbon dioxide respectively. At the end of the incubations, extractable and non-extractable (bound) residues remaining in soils were measured. Variability of herbicide dissipation half-life in soil surface samples was lower for atrazine and metamitron (CV < 12%) than for isoproturon (CV = 46%). The main contributor to the isoproturon dissipation variability was the variability of the extractable residues. For the other herbicides, spatial variability was mainly related to the variability of their mineralization. In all cases, herbicide mineralization half-lives showed higher variability than those of dissipation. Sorption or physicochemical soil properties could not explain atrazine and isoproturon degradation, whose main factors were probably directly related to the dynamics of the specific microbial degradation activity. In contrast, variability of metamitron degradation was significantly correlated to sorption coefficient (K(d)) through correlation with the sorptive soil components, organic matter and clay. Herbicide degradation decreased with depth as did the overall microbial activity. Atrazine mineralization activity was found down to a depth of 2.5 m; beyond that, it was negligible., (Copyright 2005 Society of Chemical Industry)

Published
2005
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8. Pesticide adsorption in the vadose zone: a case study on Eocene and Quaternary materials in Northern France.

Author

Coquet Y, Ribière C, and Vachier P

Subjects
Adsorption, Agriculture, Aluminum Silicates, Atrazine analysis, Atrazine chemistry, Clay, France, Fresh Water chemistry, Herbicides chemistry, Phenylurea Compounds analysis, Phenylurea Compounds chemistry, Soil Pollutants metabolism, Solubility, Triazines analysis, Triazines chemistry, Herbicides analysis, Soil analysis, Soil Pollutants analysis
Abstract

We present a set of adsorption coefficients measured on various Eocene and Quaternary materials sampled from the vadose zone of a catchment in Northern France for three herbicides, atrazine, isoproturon and metamitron. Some vadose zone materials were found to have higher adsorption coefficients than the topsoil. The adsorption coefficients were strongly dependent on the clay content of the material. From 83% to 97% of the variability in the adsorption coefficients could be explained by a linear relationship to the clay content. Adsorption coefficients normalized for clay content, Kclay, ranged between 1.6 and 17.6 litre kg(-1) for atrazine. Neglecting the adsorption properties of the vadose zone and relying exclusively on Koc values to predict mobility may bias regional or local risk assessment of groundwater contamination by pesticides. More information on the adsorption properties of geological materials should be collected to improve our ability to predict pesticide concentrations in groundwaters.

Published
2004
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9. Variation of pesticide sorption isotherm in soil at the catchment scale.

Author

Coquet Y

Subjects
Agriculture, Atrazine analysis, Atrazine chemistry, Carbon analysis, France, Herbicides chemistry, Methylurea Compounds analysis, Methylurea Compounds chemistry, Molecular Structure, Triazines analysis, Triazines chemistry, Herbicides analysis, Phenylurea Compounds, Soil analysis, Soil Pollutants analysis
Abstract

The variation of the sorption isotherm of pesticides has seldom been explored at the catchment scale. Such a study was conducted at the scale of a 187-ha agricultural catchment for three herbicides: atrazine, isoproturon and metamitron. Partition coefficient (Kd) values were measured in batch experiments on 51 topsoil samples, and showed moderate variability at the catchment scale (coefficient of variation CV approximately 30%). Values of Kd ranged from 0.47 to 1.70 litre kg(-1) for atrazine, 0.47 to 1.81 for isoproturon, and 0.55 to 2.21 for metamitron. A clustering method was used to reduce the number of samples on which to measure sorption isotherms to 14. Sorption isotherms agreed with the Freundlich rather than the linear model. Kf parameters had CV values similar to those for Kd, with values ranging from 0.78 to 2.13 mg(1 - Nf) litre(Nf) kg(-1) for atrazine, 0.61 to 1.82 for isoproturon, and 0.69 and 2.58 for metamitron. Nf exponents showed little variation (CV < 5%). Nf values were between 0.86 and 0.98 for atrazine, 0.85 and 0.90 for isoproturon, and 0.82 and 0.87 for metamitron. More than 97% of the Kf catchment-scale variations could be explained by the variations of the soil organic carbon content.

Published
2003
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10. Development and analysis of the Soil Water Infiltration Global database

Author

M. Rahmati, L. Weihermüller, J. Vanderborght, Y. A. Pachepsky, L. Mao, S. H. Sadeghi, N. Moosavi, H. Kheirfam, C. Montzka, K. Van Looy, B. Toth, Z. Hazbavi, W. Al Yamani, A. A. Albalasmeh, M. Z. Alghzawi, R. Angulo-Jaramillo, A. C. D. Antonino, G. Arampatzis, R. A. Armindo, H. Asadi, Y. Bamutaze, J. Batlle-Aguilar, B. Béchet, F. Becker, G. Blöschl, K. Bohne, I. Braud, C. Castellano, A. Cerdà, M. Chalhoub, R. Cichota, M. Císlerová, B. Clothier, Y. Coquet, W. Cornelis, C. Corradini, A. P. Coutinho, M. B. de Oliveira, J. R. de Macedo, M. F. Durães, H. Emami, I. Eskandari, A. Farajnia, A. Flammini, N. Fodor, M. Gharaibeh, M. H. Ghavimipanah, T. A. Ghezzehei, S. Giertz, E. G. Hatzigiannakis, R. Horn, J. J. Jiménez, D. Jacques, S. D. Keesstra, H. Kelishadi, M. Kiani-Harchegani, M. Kouselou, M. Kumar Jha, L. Lassabatere, X. Li, M. A. Liebig, L. Lichner, M. V. López, D. Machiwal, D. Mallants, M. S. Mallmann, J. D. de Oliveira Marques, M. R. Marshall, J. Mertens, F. Meunier, M. H. Mohammadi, B. P. Mohanty, M. Pulido-Moncada, S. Montenegro, R. Morbidelli, D. Moret-Fernández, A. A. Moosavi, M. R. Mosaddeghi, S. B. Mousavi, H. Mozaffari, K. Nabiollahi, M. R. Neyshabouri, M. V. Ottoni, T. B. Ottoni Filho, M. R. Pahlavan-Rad, A. Panagopoulos, S. Peth, P.-E. Peyneau, T. Picciafuoco, J. Poesen, M. Pulido, D. J. Reinert, S. Reinsch, M. Rezaei, F. P. Roberts, D. Robinson, J. Rodrigo-Comino, O. C. Rotunno Filho, T. Saito, H. Suganuma, C. Saltalippi, R. Sándor, B. Schütt, M. Seeger, N. Sepehrnia, E. Sharifi Moghaddam, M. Shukla, S. Shutaro, R. Sorando, A. A. Stanley, P. Strauss, Z. Su, R. Taghizadeh-Mehrjardi, E. Taguas, W. G. Teixeira, A. R. Vaezi, M. Vafakhah, T. Vogel, I. Vogeler, J. Votrubova, S. Werner, T. Winarski, D. Yilmaz, M. H. Young, S. Zacharias, Y. Zeng, Y. Zhao, H. Zhao, H. Vereecken, Institute of Bio- and Geosciences [Jülich] (IBG), Forschungszentrum Jülich GmbH, Department of Soil Science and Engineering, Faculty of Agriculture, University of Maragheh, ISMC International Soil Modeling Consortium, Institute of Bio and Geosciences Forschungszentrum Jülich, USDA-ARS : Agricultural Research Service, Chinese Academy of Agricultural Sciences (CAAS), Tarbiat Modares University [Tehran], Urmia University, Hungarian Academy of Sciences (MTA), University of Pannonia, UAE University, Jordan University of Science and Technology [Irbid, Jordan], Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés (LEHNA), Institut National de la Recherche Agronomique (INRA)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École Nationale des Travaux Publics de l'État (ENTPE)-Centre National de la Recherche Scientifique (CNRS), Centro Acadêmico do Agreste (CAA), Universidade Federal de Pernambuco [Recife] (UFPE), Hellenic Agricultural Organization, Soil and Water Resources Institute, Department of Physics (DFI), Federal University of Lavras (UFLA), University of Tehran, Makerere University (MAK), Ecologie fonctionnelle et écotoxicologie des agroécosystèmes (ECOSYS), Institut National de la Recherche Agronomique (INRA)-AgroParisTech, Innovative Groundwater Solutions, Interactions et dynamique des environnements de surface (IDES), Université Paris-Sud - Paris 11 (UP11)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Université Paris-Saclay, Eau et Environnement (IFSTTAR/GERS/EE), Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-PRES Université Nantes Angers Le Mans (UNAM), Department of Earth Sciences, Institute of Geographical Sciences, Freie Universität Berlin, Centre for Water Resource Systems, Institute of Hydraulic Engineering and Water Resources Management, University of Technology, University of Rostock [Germany], Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA), Pyrenean Institute of Ecology (CSIC), Universitat de València (UV), Mount Albert Research Station, New Zealand Institute for Plant and Food Research Limited, Czech Technical University in Prague (CTU), The New Zealand Institute for Plant & Food Research (NEW ZEALAND), Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO), Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Biogéosystèmes Continentaux - UMR7327, PSL Research University (PSL)-PSL Research University (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Ghent University [Belgium] (UGENT), Department of Civil and Environmental Engineering of the University of Perugia, Italy, Università degli Studi di Perugia (UNIPG), UniRedentor University Center, Embrapa Solos, Ministério da Agricultura, Department of Soil Science, Faculty of Agriculture, Ferdowsi University of Mashhad, Agricultural Research, Education and Extension Organization Maragheh, Dryland Agricultural Research Institute, East Azerbaijan Agricultural and Natural Resources Research and Education center, Scientific Member of Soil and Water Research Department, Department of Civil and Environmental Engineering, Virginia Polytechnic Institute and State University, Centre for Agricultural Research [Budapest] (ATK), Department of Natural Resources and Environment, Faculty of Agriculture, Jordan University of Science and Technology, Department of Watershed Management Engineering, Faculty of Natural Resources, Life and Environmental Sciences, University of California, Geographisches Institut, Rheinische Friedrich-Wilhelms-Universität Bonn, Institute of Plant Nutrition and Soil Science, Christian-Albrechts-Universität zu Kiel (CAU), ARAID Researcher, Spanish National Research Council (IPE-CSIC), Instituto Pirenaico de Ecología-CSIC (IPE-CSIC), Enginereed and Geosystems Analysis Unit, Belgian Nuclear Research Centre, Soil, Water and Land Use Team, Wageningen Environmental Researc, Civil, Surveying and Environmental Engineering, University of Newcastle [Australia] (UoN), Department of Soil Science, College of Agriculture, Isfahan University of Technology, Agricultural and Food Engineering Department, Indian Institute of Technology Kharagpur (IIT Kharagpur), State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Research Soil Scientist, United States Department of Agriculture - Agricultural Research Service, Slovak Academy of Sciences, Slovak Academy of Science [Bratislava] (SAS), Departamento de Suelo y Agua, Consejo Superior de Investigaciones Científicas (CSIC), Pomology Department, Estación Experimental de Aula Dei, Regional Research Station, ICAR-Central Arid Zone Research Institute, CSIRO Land and Water, Commonwealth Scientific and Industrial Research Organisation [Canberra] (CSIRO), Soil Science Graduate Program (ufsm.br/ppgcs), Federal University of Santa Maria, Science and Technology of the Amazonas – IFAM, Federal Institute of Education, Environment Centre Wales, Bangor University, ENGIE, Earth and Life Institute - Environmental Sciences (ELIE), Université Catholique de Louvain (UCL), Department of Environmental Sciences, Urmia Lake Research Institute, Department of Biological and Agricultural Engineering, 2117 TAMU, College Station, Texas A&M University System, Department of Agroecology, Research Centre Foulum, Aarhus University, Shiraz University (Shiraz University ), University of Kurdistan, University of Tabriz, Department of Hydrology, Geological Survey of Brazil (CPRM), Department of Water Resources and Environment, Soil and Water Research Department, Agricultural Research, Education and Extension Organization (AREEO), Sistan Agricultural and Natural Resources Research and Education Center, Department of Soil Science, University of Saskatchewan, Department of Earth and Environmental Sciences [Leuven-Heverlee], Catholic University of Leuven - Katholieke Universiteit Leuven (KU Leuven), GeoEnvironmental Research Group, Faculty of Philosophy and Letters, University of Extremadura, Soil Science Department, University of Panonia, Department of Soil Management, UNESCO Chair on Eremology, Ghent University, Agricultural Research, Education and Extension Organization (AREEO), Karaj, Iran, Soil and Water Research Institute, Instituto de Geomorfología y Suelos, Department of Geography, Universidad de Málaga [Málaga], Department of Physical Geography, Trier University, Civil Engineering Program, Alberto Luiz Coimbra Institute for Postgraduate Studies and Research in Engineering (COPPE), Federal University of Rio de Janeiro, Faculty of Agriculture, United Graduate School of Agricultural Science, Department of Materials and Life Science, Seikei University, Plant and Environmental Sciences, University of Gothenburg (GU), Rural Development Division, Japan International Research Center for Agricultural Sciences (JIRCAS), RiverLy (UR Riverly), Department of Agricultural and Bio-Resources Engineering, Faculty of Engineering, Ahmadu Bello University Zaria, Federal Agency for Water Management, Institute for land and water management research, Department of Water Resources, ITC Faculty of Geo-Information Science and Earth Observation, Twente University, Faculty of Agriculture and Natural Resources, Ardakan University, Department of Rural Engineering, University of Córdoba, Soil Physics, Embrapa Soils, Department of Soil Science, Agriculture Faculty, University of Zanja, Faculty of Civil Engineering, Department of Geography, Escuela Militar de Ingeniería (EMI), Engineering Faculty, Civil Engineering Department, Munzur University, Bureau of Economic Geology, John A. and Katherine G. Jackson School of Geosciences, University Station, University of Texas at Austin [Austin], Monitoring and Exploration Technologies, Helmholtz Centre for Environmental Research (UFZ), College of Resources and Environmental Engineering, Ludong University, ANR-11-BS56-0027,FLOODSCALE,Observation et modélisation multi-échelles pour la compréhension et la simulation des crues éclair(2011), ANR-07-VULN-0001,AVUPUR,Assessing the Vulnerability of Peri-Urban-Rivers.(2007), MEHDI RAHMATI, University of Maragheh, Maragheh, Iran/Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany, LUTZ WEIHERMÜLLER, Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany, SEYED HAMIDREZA SADEGHI, Tarbiat Modares University, Iran, LILI MAO, Chinese Academy of Agricultural Sciences, Beijing, YAKOV A. PACHEPSKY, USDA-ARS Environmental Microbial and Food Safety Laboratory, Beltsville, MD, JAN VANDERBORGHT, Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany, NILOOFAR MOOSAVI, Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany, HOSSEIN KHEIRFAM, Urmia University, Urmia, Iran, CARSTEN MONTZKA, Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany, KRIS VAN LOOY, Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany, ZEINAB HAZBAVI, Tarbiat Modares University, Iran, BRIGITTA TOTH, Hungarian Academy of Sciences, Budapest, Hungary/University of Pannonia, Keszthely, Hungary, WAFA AL YAMANI, Environment Agency, Abu Dhabi, UAE, AMMAR A. ALBALASMEH, Jordan University of Science and Technology, RAFAEL ANGULO-JARAMILLO, Univ Lyon, Université Claude Bernard Lyon, ANTÔNIO CELSO DANTAS ANTONINO, UFPE, GEORGE ARAMPATZIS, Hellenic Agricultural Organization, Soil and Water Resources Institute, Greece, ROBSON ANDRÉ ARMINDO, UFLA, HOSSEIN ASADI, University of Tehran, Karaj, Iran, YAZIDHI BAMUTAZE, Makerere University, Kampala, Uganda, JORDI BATLLE-AGUILAR, INRA, AgroParisTech Thiverval-Grignon, France/IDES CNRS/Université Paris-Sud, Orsay CEDEX/Innovative Groundwater Solutions (IGS), South Australia, Australia, BÉATRICE BÉCHET, IFSTTAR, GERS, France, MA'IN Z. ALGHZAWI, Jordan University of Science and Technology, FABIAN BECKER, Freie Universität Berlin, BRENT CLOTHIER, Plant and Food Research, Palmerston North, New Zealand, WIM CORNELIS, Ghent University, Ghent, Belgium, CORRADO CORRADINI, University of Perugia, Perugia, Italy, ARTUR PAIVA COUTINHO, UFPE, MURIEL BASTISTA DE OLIVEIRA, UniRedentor, Itaperuna, JOSE RONALDO DE MACEDO, CNPS, MATHEUS FONSECA DURÃES, UFLA, NÁNDOR FODOR, Agricultural Institute, Centre for Agricultural Research, Hungarian Academy of Sciences, GÜNTER BLÖSCHL, Centre for Water Resource Systems, TU Wien, Karlsplatz/Institute of Hydraulic Engineering and Water Resources Management, ALESSIA FLAMMINI, Ghent University, Ghent, Belgium, ASGHAR FARAJNIA, East Azerbaijan Agricultural and Natural Resources Research and Education Center, Iran, IRAJ ESKANDARI, Dryland Agricultural Research Institute, Agricultural Research, Education and Extension Organization Maragheh, East Azerbaijan, Iran, HOJAT EMAMI, Ferdowsi University of Mashhad, Mashhad, Iran, KLAUS BOHNE, University of Rostock, Germany, ISABELLE BRAUD, Irstea, UE RiverLy, Lyon-Villeurbanne Center, France, CLARA CASTELLANO, Pyrenean Institute of Ecology-CSIC, ARTEMI CERDÀ, University of Valencia, Spain, MAHA CHALHOUB, INRA AgroParisTech Functional Ecology and Ecotoxicology of Agroecosystems, ROGERIO CICHOTA, Plant and Food Research, Mount Albert Research Station, Auckland, New Zealand, MILENA CÍSLEROVÁ, Czech Technical University in Prague, Faculty of Civil Engineering, YVES COQUET, INRA AgroParisTech Functional Ecology and Ecotoxicology of Agroecosystems/Université d'Orléans, CNRS, Orléans, France, HAMID KELISHADI, Isfahan University of Technology, Iran, RAINER HORN, Christian-Albrechts-Universität zu Kiel, Germany, EVANGELOS G. HATZIGIANNAKIS, Hellenic Agricultural Organization, Soil and Water Resources Institute, Greece, SIMONE GIERTZ, Universität Bonn, Bonn, Germany, TEAMRAT A. GHEZZEHEI, University of California, Merced, USA, MOHAMAD HOSSEIN GHAVIMIPANAH, Tarbiat Modares University, Iran, MAMOUN GHARAIBEH, Jordan University of Science and Technology, JUAN JOSÉ JIMÉNEZ, ARAID Researcher, Instituto Pirenaico de Ecología, Spanish National Research Council, SASKIA DEBORAH KEESSTRA, Soil, Water and Land Use Team, Wageningen Environmental Research/the University of Newcastle, Australia, DIEDERIK JACQUES, Enginereed and Geosystems Analysis Unit, Belgian Nuclear Research Centre, Mol, Belgium, MAHBOOBEH KIANI-HARCHEGANI, Faculty of Natural Resources, Tarbiat Modares University, Iran, MEHDI KOUSELOU, Faculty of Agriculture, University of Maragheh, Maragheh, Iran, MADAN KUMAR JHA, Indian Institute of Technology Kharagpur, India, LAURENT LASSABATERE, Univ Lyon, Université Claude Bernard Lyon 1, CNRS, ENTPE, Vaulx-en-Velin, France, XIAOYAN LI, Beijing Normal University, Beijing, China, MARK A. LIEBIG, USDA Agricultural Research Service, Mandan, ND, USA, DENIZ YILMAZ, Munzur University, Tunceli, Turkey, MICHAEL H. YOUNG, University of Texas at Austin, University Station, USA, HONG ZHAO, University of Twente, Enschede, the Netherlands, HARRY VEREECKEN, Forschungszentrum Jülich GmbH, Institute of Bio- and Geosciences: Agrosphere (IBG-3), Jülich, Germany/ISMC International Soil Modeling Consortium, Institute of Bio and Geosciences Forschungszentrum, Germany., MARÍA VICTORIA LÓPEZ, Departamento de Suelo y Agua, Estación Experimental de Aula Dei (EEAD), Consejo Superior de Investigaciones Científicas, Spain, DEEPESH MACHIWAL, ICAR-Central Arid Zone Research Institute, Regional Research Station, Gujarat, India, DIRK MALLANTS, CSIRO Land and Water, Glen Osmond, South Australia, Australia, MICAEL STOLBEN MALLMANN, UFSM, JEAN DALMO DE OLIVEIRA MARQUES, IFAM, MILES R. MARSHALL, Centre for Ecology & Hydrology, Environment Centre Wales, Deiniol Road, Bangor, UK, JAN MERTENS, ENGIE Research and Technologies, Brussels, Belgium, FÉLICIEN MEUNIER, Université catholique de Louvain, Earth and Life Institute-Environmental Sciences, Louvain-la Neuve, Belgium, MOHAMMAD HOSSEIN MOHAMMADI, University of Tehran, Karaj, Iran, BINAYAK P. MOHANTY, Department of Biological and Agricultural Engineering, Texas A&M Univ., College Station, USA, MANSONIA PULIDO-MONCADA, Aarhus University, Department of Agroecology, Research Centre Foulum, Tjele, Denmark, SUZANA MONTENEGRO, UFPE, RENATO MORBIDELLI, University of Perugia, Perugia, Italy, DAVID MORET-FERNÁNDEZ, Departamento de Suelo y Agua, Estación Experimental de Aula Dei (EEAD), Consejo Superior de Investigaciones Científicas (CSIC), Spain, ALI AKBAR MOOSAVI, Department of Soil Science, College of Agriculture, Shiraz University, Shiraz, Iran, MOHAMMAD REZA MOSADDEGHI, Department of Soil Science, College of Agriculture, Isfahan University of Technology, Iran, SEYED BAHMAN MOUSAVI, Department of Soil Science and Engineering, Faculty of Agriculture, University of Maragheh, Maragheh, Iran, HASAN MOZAFFARI, Department of Soil Science, College of Agriculture, Shiraz University, Shiraz, Iran, KAMAL NABIOLLAHI, Department of Soil Science and Engineering, Faculty of Agriculture, University of Kurdistan, Iran, MOHAMMAD REZA NEYSHABOURI, Department of Soil Science, Faculty of Agriculture, University of Tabriz, Tabriz, Iran, MARTA VASCONCELOS OTTONI, CPRM, THEOPHILO BENEDICTO OTTONI FILHO, UFRJ, MOHAMMAD REZA PAHLAVAN-RAD, Soil and Water Research Department, Sistan Agricultural and Natural Resources Research and Education Center, Agricultural Research, Education and Extension Organization (AREEO), Zabol, Iran, ANDREAS PANAGOPOULOS, Hellenic Agricultural Organization, Soil and Water Resources Institute, Greece, STEPHAN PETH, Department of Soil Science, University of Kassel, Germany, PIERRE-EMMANUEL PEYNEAU, IFSTTAR, Bouguenais, France, TOMMASO PICCIAFUOCO, Centre for Water Resource Systems, Vienna, Austria/University of Perugia, Perugia, Italy, JEAN POESEN, Catholic University of Leuven, Geo-Institute, Belgium, MANUEL PULIDO, GeoEnvironmental Research Group, University of Extremadura, Cáceres, Spain, DALVAN JOSÉ REINERT, UFSM, SABINE REINSCH, Centre for Ecology & Hydrology, Environment Centre Wales, UK, MEISAM REZAEI, Department of Soil Management, UNESCO Chair on Eremology, Ghent University, Ghent, Belgium/Soil and Water Research Institute, Agricultural Research, Education and Extension Organization (AREEO), Karaj, Iran, FRANCIS PARRY ROBERTS, Centre for Ecology & Hydrology, Environment Centre Wales, UK, DAVID ROBINSON, Centre for Ecology & Hydrology, Environment Centre Wales, Deiniol Road, UK, JESÚS RODRIGO-COMINO, University of Málaga, Spain/Trier University, Trier, Germany, OTTO CORRÊA ROTUNNO FILHO, UFRJ, TADAOMI SAITO, Faculty of Agriculture, Tottori University, Japan, HIDEKI SUGANUMA, Seikei University, Tokyo, Japan, CARLA SALTALIPPI, Department of Civil and Environmental Engineering, University of Perugia, Perugia, Italy, RENÁTA SÁNDOR, Agricultural Institute, Centre for Agricultural Research, Hungarian Academy of Sciences, Hungary, BRIGITTA SCHÜTT, Freie Universität Berlin, Department of Earth Sciences, Institute of Geographical Sciences, Berlin, Germany, MANUEL SEEGER, Department of Physical Geography, Trier University, Germany, NASROLLAH SEPEHRNIA, Department of Soil Science, College of Agriculture, Isfahan University of Technology, Isfahan, Iran, EHSAN SHARIFI MOGHADDAM, Department of Watershed Management Engineering, Faculty of Natural Resources, Tarbiat Modares University, Iran, MANOJ SHUKLA, Plant and Environmental Sciences, New Mexico State University, Las Cruces, New Mexico, USA, SHIRAKI SHUTARO, Japan International Research Center for Agricultural Science, Rural Development Division, Tsukuba, Japan, RICARDO SORANDO, Irstea, UE RiverLy, Lyon-Villeurbanne Center, France, AJAYI ASISHANA STANLEY, Ahmadu Bello University Zaria, Nigeria, PETER STRAUSS, Institute for Land and Water Management Research, Federal Agency for Water Management, Austria, ZHONGBO SU, University of Twente, Enschede, the Netherlands, RUHOLLAH TAGHIZADEH-MEHRJARDI, Ardakan University, Ardakan, Yazd Province, Iran, ENCARNACIÓN TAGUAS, University of Córdoba, Spain, WENCESLAU GERALDES TEIXEIRA, CNPS, ALI REZA VAEZI, University of Zanjan, Zanjan, Iran, MEHDI VAFAKHAH, Tarbiat Modares University, Iran, YING ZHAO, Ludong University, China, YIJIAN ZENG, University of Twente, Enschede, the Netherlands, STEFFEN ZACHARIAS, UFZ Helmholtz Centre for Environment Research, Monitoring and Exploration Technologies, Leipzig, Germany, LUBOMÍR LICHNER, Institute of Hydrology, Slovak Academy of Sciences, Bratislava, Slovakia, TOMAS VOGEL, Czech Technical University in Prague, Faculty of Civil Engineering, Czech Republic, IRIS VOGELER, Plant and Food Research, Mount Albert Research Station, Auckland, New Zealand, JANA VOTRUBOVA, Czech Technical University in Prague, Faculty of Civil Engineering, Czech Republic, STEFFEN WERNER, Department of Geography, Ruhr University Bochum, Germany, THIERRY WINARSKI, Univ Lyon, Université Claude Bernard Lyon 1, CNRS, ENTPE, Vaulx-en-Velin, France, Jülich Research Centre, European Commission, Ministerio de Economía y Competitividad (España), Czech Science Foundation, Slovak Research and Development Agency, Rahmati, Mehdi, López Sánchez, María Victoria, Moret-Fernández, David, Centre National de la Recherche Scientifique (CNRS)-Institut National de la Recherche Agronomique (INRA)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École Nationale des Travaux Publics de l'État (ENTPE), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, PSL Research University (PSL)-PSL Research University (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), PSL Research University (PSL)-PSL Research University (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Rahmati, Mehdi [0000-0001-5547-6442], López Sánchez, María Victoria [0000-0003-4113-0381], Moret-Fernández, David [0000-0002-6674-0453], Forschungszentrum Jülich GmbH | Centre de recherche de Juliers, Helmholtz-Gemeinschaft = Helmholtz Association-Helmholtz-Gemeinschaft = Helmholtz Association, Université Claude Bernard Lyon 1 (UCBL), Hellenic Agricultural Organization Demeter (HAO Demeter), Makerere University [Kampala, Ouganda] (MAK), University of Rostock, Plant & Food Research, Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)-Centre National de la Recherche Scientifique (CNRS)-Université d'Orléans (UO)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers en région Centre (OSUC), Universiteit Gent = Ghent University [Belgium] (UGENT), Virginia Polytechnic Institute and State University [Blacksburg], Beijing Normal University (BNU), Slovak Academy of Sciences (SAS), Université Catholique de Louvain = Catholic University of Louvain (UCL), Aarhus University [Aarhus], Universidad de Málaga [Málaga] = University of Málaga [Málaga], Programa de Engenharia Civil (COC/COPPE-UFRJ), Instituto Alberto Luiz Coimbra de Pós-Graduação e Pesquisa de Engenharia (COPPE-UFRJ), Universidade Federal do Rio de Janeiro (UFRJ)-Universidade Federal do Rio de Janeiro (UFRJ), Ahmadu Bello University, Helmholtz Zentrum für Umweltforschung = Helmholtz Centre for Environmental Research (UFZ), College of Resources and Environmental Engineering [Yantai], Department of Water Resources, UT-I-ITC-WCC, and Faculty of Geo-Information Science and Earth Observation

Subjects
Condutividade Hidráulica, [SDV]Life Sciences [q-bio], 0208 environmental biotechnology, 02 engineering and technology, Silt, computer.software_genre, Soil, RING INFILTROMETERS, 900 Geschichte und Geografie::910 Geografie, Reisen::910 Geografie, Reisen, Hydraulic conductivity, ELECTRICAL-CONDUCTIVITY, Agricultural land, ddc:550, Meteorology & Atmospheric Sciences, SATURATED HYDRAULIC CONDUCTIVITY, Geosciences, Multidisciplinary, database, lcsh:Environmental sciences, 2. Zero hunger, lcsh:GE1-350, Database, IN-SITU, lcsh:QE1-996.5, Geology, 04 agricultural and veterinary sciences, PE&RC, Pedo-transfer functions, 6. Clean water, Infiltration (hydrology), HYDROPHYSICAL PARAMETERS, [SDE]Environmental Sciences, Physical Sciences, INFILTRATION GLOBAL DATABASE, Hidrologia, PHYSICAL-PROPERTIES, SANDY SOIL, TENSION INFILTROMETER, Ecology and Environment, Pedotransfer function, PEDOTRANSFER FUNCTIONS, Life Science, SOIL INFILTRATION MEASUREMENTS, Land surface models, Soil Water Infiltration Global database, ANALYSIS OF THE SOIL WATER, Science & Technology, Land use, Infiltration, 15. Life on land, 020801 environmental engineering, Infiltração, lcsh:Geology, Solo, Infiltration, Land surface models, Land use, Pedo-transfer functions, SWIG, Agriculture and Soil Science, Data quality, ITC-ISI-JOURNAL-ARTICLE, Earth and Environmental Sciences, INFILTROMETER MEASUREMENTS, Soil water, 040103 agronomy & agriculture, 0401 agriculture, forestry, and fisheries, General Earth and Planetary Sciences, Environmental science, Hydrology, ITC-GOLD, computer
Abstract

27 Pags.- 11 Tabls.- 8 Figs. © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License., In this paper, we present and analyze a novel global database of soil infiltration measurements, the Soil Water Infiltration Global (SWIG) database. In total, 5023 infiltration curves were collected across all continents in the SWIG database. These data were either provided and quality checked by the scientists who performed the experiments or they were digitized from published articles. Data from 54 different countries were included in the database with major contributions from Iran, China, and the USA. In addition to its extensive geographical coverage, the collected infiltration curves cover research from 1976 to late 2017. Basic information on measurement location and method, soil properties, and land use was gathered along with the infiltration data, making the database valuable for the development of pedotransfer functions (PTFs) for estimating soil hydraulic properties, for the evaluation of infiltration measurement methods, and for developing and validating infiltration models. Soil textural information (clay, silt, and sand content) is available for 3842 out of 5023 infiltration measurements ( ∼ 76%) covering nearly all soil USDA textural classes except for the sandy clay and silt classes. Information on land use is available for 76 % of the experimental sites with agricultural land use as the dominant type (∼ 40%). We are convinced that the SWIG database will allow for a better parameterization of the infiltration process in land surface models and for testing infiltration models. All collected data and related soil characteristics are provided online in *.xlsx and *.csv formats for reference, and we add a disclaimer that the database is for public domain use only and can be copied freely by referencing it. Supplementary data are available at https://doi.org/10.1594/PANGAEA.885492 (Rahmati et al., 2018). Data quality assessment is strongly advised prior to any use of this database. Finally, we would like to encourage scientists to extend and update the SWIG database by uploading new data to it., First author thanks the International and Scientific Cooperation Office of the University of Maragheh, Iran, as well as the research committee and board members of the university for their assistance in conducting the current work. The financial support received from the Forschungszentrum Jülich GmbH is gratefully acknowledged by the first author. Parts of the database were made available through research work carried out in the framework of LIFE+ projects funded by the EC. The support of the Spanish Ministry of Economy through project CGL2014-53017-C2-1-R is acknowledged. The support of the Czech Science Foundation through project no. 16-05665S is acknowledged. The support of the Slovak Research and Development Agency through project no. APVV-15-0160 is acknowledged.

Published
2018
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