Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device

Soil hydraulic conductivity is a property that describes how easily water can move through a porous space and its determination is important because it controls many soil hydrological processes. The objectives of this work were: i - to assess the suitability of lab tension mini-infiltrometry to meas...

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Autores principales: Soracco, Carlos Germán, Villarreal, Rafael, Melani, Esteban, Oderiz, Juan Agustin, Salazar, María Paz, Otero, María Florencia, Irizar, Alicia Beatriz, Lozano, Luis Alberto
Formato: Artículo
Lenguaje:Inglés
Publicado: Elsevier 2019
Materias:
Acceso en línea:https://www.sciencedirect.com/science/article/pii/S0016706118314769
http://hdl.handle.net/20.500.12123/5187
https://doi.org/10.1016/j.geoderma.2018.10.045
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author Soracco, Carlos Germán
Villarreal, Rafael
Melani, Esteban
Oderiz, Juan Agustin
Salazar, María Paz
Otero, María Florencia
Irizar, Alicia Beatriz
Lozano, Luis Alberto
author_browse Irizar, Alicia Beatriz
Lozano, Luis Alberto
Melani, Esteban
Oderiz, Juan Agustin
Otero, María Florencia
Salazar, María Paz
Soracco, Carlos Germán
Villarreal, Rafael
author_facet Soracco, Carlos Germán
Villarreal, Rafael
Melani, Esteban
Oderiz, Juan Agustin
Salazar, María Paz
Otero, María Florencia
Irizar, Alicia Beatriz
Lozano, Luis Alberto
author_sort Soracco, Carlos Germán
collection INTA Digital
description Soil hydraulic conductivity is a property that describes how easily water can move through a porous space and its determination is important because it controls many soil hydrological processes. The objectives of this work were: i - to assess the suitability of lab tension mini-infiltrometry to measure hydraulic conductivity, by comparing with field tension disc infiltrometer data; and ii - to assess the effect of different tillage practices on hydraulic conductivity values and pore network in three different soils from Argentinean Pampas Region. Additionally, three analytical approaches to obtain K from mini-infiltrometry data were compared. Field infiltration with tension disc infiltrometer (TI) and laboratory infiltration with a proposed mini-infiltrometer (MI) were conducted in three different textured soils of Argentinian Pampas Region (loam, silty loam and sandy loam) in long-term experiments under no-tillage (NT) and conventional tillage (CT). Hydraulic conductivity (K) at different tensions (h) (6, 3 and 0 cm), namely K6, K3 and K0, and soil pore connectivity were estimated. There was no significant difference between K (h) values obtained from TI and MI, ranging between 0.47 and 2.36 cm h−1 and 0.52 and 1.77 and cm h−1, respectively. We concluded that NT reduces soil hydraulic conductivity, affecting soil pore connectivity, especially in fine textured soils. CT showed higher total pore connectivity in all studied sites. The proposed laboratory mini-infiltrometry method allows determining soil hydraulic conductivity function and pore connectivity in a simple, fast and inexpensive way.
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spelling INTA51872019-05-22T13:54:57Z Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device Soracco, Carlos Germán Villarreal, Rafael Melani, Esteban Oderiz, Juan Agustin Salazar, María Paz Otero, María Florencia Irizar, Alicia Beatriz Lozano, Luis Alberto Porosidad del Suelo Conductividad Hidráulica Propiedades Hidráulicas del Suelo Labranza Convencional Labranza Agua de Infiltración Soil Porosity Hydraulic Conductivity Soil Hydraulic Properties Conventional Tillage Tillage Infiltration Water cientifico Soil hydraulic conductivity is a property that describes how easily water can move through a porous space and its determination is important because it controls many soil hydrological processes. The objectives of this work were: i - to assess the suitability of lab tension mini-infiltrometry to measure hydraulic conductivity, by comparing with field tension disc infiltrometer data; and ii - to assess the effect of different tillage practices on hydraulic conductivity values and pore network in three different soils from Argentinean Pampas Region. Additionally, three analytical approaches to obtain K from mini-infiltrometry data were compared. Field infiltration with tension disc infiltrometer (TI) and laboratory infiltration with a proposed mini-infiltrometer (MI) were conducted in three different textured soils of Argentinian Pampas Region (loam, silty loam and sandy loam) in long-term experiments under no-tillage (NT) and conventional tillage (CT). Hydraulic conductivity (K) at different tensions (h) (6, 3 and 0 cm), namely K6, K3 and K0, and soil pore connectivity were estimated. There was no significant difference between K (h) values obtained from TI and MI, ranging between 0.47 and 2.36 cm h−1 and 0.52 and 1.77 and cm h−1, respectively. We concluded that NT reduces soil hydraulic conductivity, affecting soil pore connectivity, especially in fine textured soils. CT showed higher total pore connectivity in all studied sites. The proposed laboratory mini-infiltrometry method allows determining soil hydraulic conductivity function and pore connectivity in a simple, fast and inexpensive way. EEA Cuenca del Salado Fil: Soracco, Carlos Germán. Universidad Nacional de La Plata. Facultad de Ciencias Agrarias y Forestales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Villarreal, Rafael. Universidad Nacional de La Plata. Facultad de Ciencias Agrarias y Forestales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Melani, Esteban. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Cuenca del Salado. Agencia de Extensión Rural Chascomus; Argentina Fil: Oderiz, Juan Agustin. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Anguil; Argentina Fil: Salazar, María Paz. Universidad Nacional de La Plata. Facultad de Ciencias Agrarias y Forestales; Argentina Fil: Otero, María Florencia. Universidad Nacional de La Plata. Facultad de Ciencias Agrarias y Forestales; Argentina Fil: Irizar, Alicia Beatriz. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Pergamino; Argentina Fil: Lozano, Luis Alberto. Universidad Nacional de La Plata. Facultad de Ciencias Agrarias y Forestales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina 2019-05-22T13:53:11Z 2019-05-22T13:53:11Z 2019-03-01 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion https://www.sciencedirect.com/science/article/pii/S0016706118314769 http://hdl.handle.net/20.500.12123/5187 0016-7061 1872-6259 https://doi.org/10.1016/j.geoderma.2018.10.045 eng info:eu-repo/semantics/restrictedAccess application/pdf Elsevier Geoderma 337 : 1236-1244 (March 2019)
spellingShingle Porosidad del Suelo
Conductividad Hidráulica
Propiedades Hidráulicas del Suelo
Labranza Convencional
Labranza
Agua de Infiltración
Soil Porosity
Hydraulic Conductivity
Soil Hydraulic Properties
Conventional Tillage
Tillage
Infiltration Water
cientifico
Soracco, Carlos Germán
Villarreal, Rafael
Melani, Esteban
Oderiz, Juan Agustin
Salazar, María Paz
Otero, María Florencia
Irizar, Alicia Beatriz
Lozano, Luis Alberto
Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device
title Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device
title_full Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device
title_fullStr Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device
title_full_unstemmed Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device
title_short Hydraulic conductivity and pore connectivity. Effects of conventional and no-till systems determined using a simple laboratory device
title_sort hydraulic conductivity and pore connectivity effects of conventional and no till systems determined using a simple laboratory device
topic Porosidad del Suelo
Conductividad Hidráulica
Propiedades Hidráulicas del Suelo
Labranza Convencional
Labranza
Agua de Infiltración
Soil Porosity
Hydraulic Conductivity
Soil Hydraulic Properties
Conventional Tillage
Tillage
Infiltration Water
cientifico
url https://www.sciencedirect.com/science/article/pii/S0016706118314769
http://hdl.handle.net/20.500.12123/5187
https://doi.org/10.1016/j.geoderma.2018.10.045
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