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Resumen
Soil structural degradation and water erosion processes were observed even in no-tillage schemes in the Pampas region. Within these conservation systems, agrochemical application per hectare is one of the highest globally. Thus, this entails a serious risk of water contamination. The objectives of this study were to (1) test the hypothesis that the hydrological dynamics and sediment concentration related to surface runoff were conditioned by soil [ver mas...]
dc.contributor.authorSainz, Daiana Soledad
dc.contributor.authorBehrends Kraemer, Filipe
dc.contributor.authorCarfagno, Patricia
dc.contributor.authorEiza, Maximiliano Joaquin
dc.contributor.authorChagas, Celio Ignacio
dc.date.accessioned2024-08-02T10:53:36Z
dc.date.available2024-08-02T10:53:36Z
dc.date.issued2024-07-09
dc.identifier.issn1537-2537
dc.identifier.issn0047-2425
dc.identifier.otherhttps://doi.org/10.1002/jeq2.20596
dc.identifier.urihttp://hdl.handle.net/20.500.12123/18759
dc.identifier.urihttps://acsess.onlinelibrary.wiley.com/doi/10.1002/jeq2.20596
dc.description.abstractSoil structural degradation and water erosion processes were observed even in no-tillage schemes in the Pampas region. Within these conservation systems, agrochemical application per hectare is one of the highest globally. Thus, this entails a serious risk of water contamination. The objectives of this study were to (1) test the hypothesis that the hydrological dynamics and sediment concentration related to surface runoff were conditioned by soil structure regardless of the presence of maize (Zea mays L.) crop residue and (2) assess the incidence of maize crop residue on glyphosate and aminomethylphosphonic acid (AMPA) concentration in runoff. The soil under study corresponded to Arroyo Dulce Series (Typic Argiudoll silty loam soil). Rain simulations were performed in the laboratory on undisturbed soil samples. Total runoff and infiltration rate were similar between treatments with C(+) and without C(−) maize crop residues (C(+) 1381.40 mL and 14.27 mm h−1, C(−): 1529.70 mL and 21.67 mm h−1). The C(−) treatments showed a higher sediment concentration than C(+) (1.58 and 0.42 g 100 mL−1, respectively). Glyphosate and AMPA average values in runoff were 15.9 and 33.9 μg L−1. High variability of the hydro-physical properties and occurrence of soil structure, particularly platy ones, were detected. The hydrological variables were conditioned mainly by the occurrence of platy structures regardless of crop residue presence. Glyphosate concentration was increased in the first runoff event by the presence of corn residues, while AMPA concentrations were higher in the second runoff event in both residue treatments. In this study, maize residue on the soil surface protected the soil from sediment detachment but did not change runoff or infiltration. Thus, the implementation of agricultural management practices that promote vegetative residue cover has shown positive results to erosion.eng
dc.formatapplication/pdfes_AR
dc.language.isoenges_AR
dc.publisherWileyes_AR
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_AR
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/es_AR
dc.sourceJournal of Environmental Quality 53 (4) : 1-14. (July-August 2024)es_AR
dc.subjectSoil Propertieseng
dc.subjectPropiedades del Sueloes_AR
dc.subjectEscorrentia
dc.subjectRunoffeng
dc.subjectResiduo de Cosechas
dc.subjectCrop Residueseng
dc.subjectPérdida de Suelo
dc.subjectSoil Losseng
dc.subjectGlifosato
dc.subjectGlyphosateeng
dc.subject.otherPlaty Structureeng
dc.subject.otherEstructura Laminares_AR
dc.subject.otherSoil Covereng
dc.subject.otherCobertura del Sueloes_AR
dc.titleSoil hydro-physical variables and crop residues determinate runoff soil loss, and glyphosate and AMPA concentration in the aqueous phase under simulated rainfall eventses_AR
dc.typeinfo:ar-repo/semantics/artículoes_AR
dc.typeinfo:eu-repo/semantics/articlees_AR
dc.typeinfo:eu-repo/semantics/publishedVersiones_AR
dc.rights.licenseCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)es_AR
dc.description.origenInstituto de Suelos
dc.description.filFil: Sainz, Daiana Soledad. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentina. Universidad de Buenos Aires. Facultad de Agronomía. Cátedra de Conservación y Manejo de Suelos; Argentinaes_AR
dc.description.filFil: Behrends Kraemer, Filipe. Universidad de Buenos Aires. Facultad de Agronomía. Cátedra de Conservación y Manejo de Suelos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentinaes_AR
dc.description.filFil: Carfagno, Patricia. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentinaes_AR
dc.description.filFil: Eiza, Maximiliano Joaquín. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Balcarce; Argentinaes_AR
dc.description.filFil: Chagas, Celio. Universidad de Buenos Aires. Facultad de Agronomía. Cátedra de Conservación y Manejo de Suelos; Argentinaes_AR
dc.subtypecientifico


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