Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina

The objective of the present study was to describe the relationships between soil physical properties and to identify variables that determine the pore system and hydrological functions which are specifically important in drought prone semiarid marginal croplands. We compared Mollisols under natural vegetation (NV) with their agriculture (AG) pairs in the central Argentinean Dry Pampas to obtain the range of values for variables that characterize the soil pore system. These were total carbon (OC), bulk density (BD), structural instability index (SII), volumetric weight of aggregates (VAW), total porosity (TP), macropores (Ma), saturated hydraulic conductivity (K), infiltration rate (IR), Dexter's S index (S), and least limiting water range (LLWR). To a depth of more than 23 cm, TP and Ma were considerably lower (~ 35% and 50% less, respectively) in AG versus NV. The changes in porosity and pore size resulted in 74% smaller IR and 65% lower K. The S index had mean values of 0.16 and 0.14 for the upper and middle layer respectively in NV; while for AG, these values were significantly lower (0.09 and 0.10, respectively). The LLWR was also lower in AG (21 and 59% less in the upper and middle layer, respectively), due to high soil resistance even at non-limiting BDs (1.17 and 1.32 g cm−3 for AG2 and AG1, respectively). Soil OC was positively correlated with TP, Ma, and S, and negatively correlated with BD and SII. Multiple regression models for S included SII, TP, and clay contents, while for LLWR the variables were OC, TP, and clay plus silt. Thus, these complex soil quality indices can be predicted by using simpler physical parameters, but texture and organic matter also have a strong effect on them. Moreover, our results contribute to a better understanding of the role of texture and organic matter in controlling soil physical quality and for maintaining soil-based ecosystem services.

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Main Authors: Fernandez, Romina, Belmonte, Valeria, Quiroga, Alberto Raul, Lobartini, Carlos, Noellemeyer, Elke
Format: info:ar-repo/semantics/artículo biblioteca
Language:eng
Published: Elsevier 2021-06-01
Subjects:Suelo, Fisica del Suelo, Utilización de la Tierra, Molisoles, Porosidad del Suelo, Infiltración, Conductividad Hidráulica, Soil, Soil Physics, Land Use, Mollisols, Soil Porosity, Infiltration, Hydraulic Conductivity,
Online Access:http://hdl.handle.net/20.500.12123/9261
https://www.sciencedirect.com/science/article/abs/pii/S2352009421000390
https://doi.org/10.1016/j.geodrs.2021.e00394
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spelling oai:localhost:20.500.12123-92612021-05-04T15:50:44Z Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina Fernandez, Romina Belmonte, Valeria Quiroga, Alberto Raul Lobartini, Carlos Noellemeyer, Elke Suelo Fisica del Suelo Utilización de la Tierra Molisoles Porosidad del Suelo Infiltración Conductividad Hidráulica Soil Soil Physics Land Use Mollisols Soil Porosity Infiltration Hydraulic Conductivity The objective of the present study was to describe the relationships between soil physical properties and to identify variables that determine the pore system and hydrological functions which are specifically important in drought prone semiarid marginal croplands. We compared Mollisols under natural vegetation (NV) with their agriculture (AG) pairs in the central Argentinean Dry Pampas to obtain the range of values for variables that characterize the soil pore system. These were total carbon (OC), bulk density (BD), structural instability index (SII), volumetric weight of aggregates (VAW), total porosity (TP), macropores (Ma), saturated hydraulic conductivity (K), infiltration rate (IR), Dexter's S index (S), and least limiting water range (LLWR). To a depth of more than 23 cm, TP and Ma were considerably lower (~ 35% and 50% less, respectively) in AG versus NV. The changes in porosity and pore size resulted in 74% smaller IR and 65% lower K. The S index had mean values of 0.16 and 0.14 for the upper and middle layer respectively in NV; while for AG, these values were significantly lower (0.09 and 0.10, respectively). The LLWR was also lower in AG (21 and 59% less in the upper and middle layer, respectively), due to high soil resistance even at non-limiting BDs (1.17 and 1.32 g cm−3 for AG2 and AG1, respectively). Soil OC was positively correlated with TP, Ma, and S, and negatively correlated with BD and SII. Multiple regression models for S included SII, TP, and clay contents, while for LLWR the variables were OC, TP, and clay plus silt. Thus, these complex soil quality indices can be predicted by using simpler physical parameters, but texture and organic matter also have a strong effect on them. Moreover, our results contribute to a better understanding of the role of texture and organic matter in controlling soil physical quality and for maintaining soil-based ecosystem services. EEA Anguil Fil: Fernández, Romina. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Anguil; Argentina Fil: Belmonte, Valeria. Universidad Nacional de La Pampa. Facultad de Agronomía; Argentina Fil: Quiroga, Alberto. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Anguil; Argentina Fil: Lobartini, Carlos. Universidad Nacional del Sur. Departamento de Agronomía; Argentina Fil: Noellemeyer, Elke. Universidad Nacional de La Pampa. Facultad de Agronomía; Argentina 2021-05-04T14:44:44Z 2021-05-04T14:44:44Z 2021-06-01 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/9261 https://www.sciencedirect.com/science/article/abs/pii/S2352009421000390 2352-0094 https://doi.org/10.1016/j.geodrs.2021.e00394 eng info:eu-repograntAgreement/INTA/2019-PE-E2-I042-001/2019-PE-E2-I042-001/AR./Uso y gestión eficiente del Agua en Sistemas de Secano info:eu-repo/semantics/restrictedAccess application/pdf Elsevier Geoderma Regional 25 : e00394 (junio de 2021)
institution INTA AR
collection DSpace
country Argentina
countrycode AR
component Bibliográfico
access En linea
databasecode dig-inta-ar
tag biblioteca
region America del Sur
libraryname Biblioteca Central del INTA Argentina
language eng
topic Suelo
Fisica del Suelo
Utilización de la Tierra
Molisoles
Porosidad del Suelo
Infiltración
Conductividad Hidráulica
Soil
Soil Physics
Land Use
Mollisols
Soil Porosity
Infiltration
Hydraulic Conductivity
Suelo
Fisica del Suelo
Utilización de la Tierra
Molisoles
Porosidad del Suelo
Infiltración
Conductividad Hidráulica
Soil
Soil Physics
Land Use
Mollisols
Soil Porosity
Infiltration
Hydraulic Conductivity
spellingShingle Suelo
Fisica del Suelo
Utilización de la Tierra
Molisoles
Porosidad del Suelo
Infiltración
Conductividad Hidráulica
Soil
Soil Physics
Land Use
Mollisols
Soil Porosity
Infiltration
Hydraulic Conductivity
Suelo
Fisica del Suelo
Utilización de la Tierra
Molisoles
Porosidad del Suelo
Infiltración
Conductividad Hidráulica
Soil
Soil Physics
Land Use
Mollisols
Soil Porosity
Infiltration
Hydraulic Conductivity
Fernandez, Romina
Belmonte, Valeria
Quiroga, Alberto Raul
Lobartini, Carlos
Noellemeyer, Elke
Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina
description The objective of the present study was to describe the relationships between soil physical properties and to identify variables that determine the pore system and hydrological functions which are specifically important in drought prone semiarid marginal croplands. We compared Mollisols under natural vegetation (NV) with their agriculture (AG) pairs in the central Argentinean Dry Pampas to obtain the range of values for variables that characterize the soil pore system. These were total carbon (OC), bulk density (BD), structural instability index (SII), volumetric weight of aggregates (VAW), total porosity (TP), macropores (Ma), saturated hydraulic conductivity (K), infiltration rate (IR), Dexter's S index (S), and least limiting water range (LLWR). To a depth of more than 23 cm, TP and Ma were considerably lower (~ 35% and 50% less, respectively) in AG versus NV. The changes in porosity and pore size resulted in 74% smaller IR and 65% lower K. The S index had mean values of 0.16 and 0.14 for the upper and middle layer respectively in NV; while for AG, these values were significantly lower (0.09 and 0.10, respectively). The LLWR was also lower in AG (21 and 59% less in the upper and middle layer, respectively), due to high soil resistance even at non-limiting BDs (1.17 and 1.32 g cm−3 for AG2 and AG1, respectively). Soil OC was positively correlated with TP, Ma, and S, and negatively correlated with BD and SII. Multiple regression models for S included SII, TP, and clay contents, while for LLWR the variables were OC, TP, and clay plus silt. Thus, these complex soil quality indices can be predicted by using simpler physical parameters, but texture and organic matter also have a strong effect on them. Moreover, our results contribute to a better understanding of the role of texture and organic matter in controlling soil physical quality and for maintaining soil-based ecosystem services.
format info:ar-repo/semantics/artículo
topic_facet Suelo
Fisica del Suelo
Utilización de la Tierra
Molisoles
Porosidad del Suelo
Infiltración
Conductividad Hidráulica
Soil
Soil Physics
Land Use
Mollisols
Soil Porosity
Infiltration
Hydraulic Conductivity
author Fernandez, Romina
Belmonte, Valeria
Quiroga, Alberto Raul
Lobartini, Carlos
Noellemeyer, Elke
author_facet Fernandez, Romina
Belmonte, Valeria
Quiroga, Alberto Raul
Lobartini, Carlos
Noellemeyer, Elke
author_sort Fernandez, Romina
title Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina
title_short Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina
title_full Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina
title_fullStr Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina
title_full_unstemmed Land-use change affects soil hydro-physical properties in Mollisols of semiarid Central Argentina
title_sort land-use change affects soil hydro-physical properties in mollisols of semiarid central argentina
publisher Elsevier
publishDate 2021-06-01
url http://hdl.handle.net/20.500.12123/9261
https://www.sciencedirect.com/science/article/abs/pii/S2352009421000390
https://doi.org/10.1016/j.geodrs.2021.e00394
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AT lobartinicarlos landusechangeaffectssoilhydrophysicalpropertiesinmollisolsofsemiaridcentralargentina
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