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 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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Auteurs principaux: Soracco, Carlos Germán, Villarreal, Rafael, Melani, Esteban, Oderiz, Juan Agustin, Salazar, María Paz, Otero, María Florencia, Irizar, Alicia Beatriz, Lozano, Luis Alberto
Format: info:ar-repo/semantics/artículo biblioteca
Langue:eng
Publié: Elsevier 2019-03-01
Sujets: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,
Accès en ligne: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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