2023
DOI: 10.1016/j.catena.2023.107066
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Changes in soil hydrodynamic parameters during intermittent rainfall following tillage

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Cited by 7 publications
(3 citation statements)
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“…An influence of the season on the reliability of soil loss prediction models has already been observed by Todisco et al [43], which attributed this to the different conditions of the soil surface. The climatic conditions (particularly precipitation and air temperature) roughly described by the variable "period" can affect the dynamics of various soil properties such as roughness [44], infiltration and bulk density [45,46], and hydraulic conductivity [47]. Therefore, even if the RF model already explicitly considers essential features such as Q R and R, the "period" becomes important to allow the model to evaluate the seasonal variability of their effect on soil loss.…”
Section: Discussionmentioning
confidence: 99%
“…An influence of the season on the reliability of soil loss prediction models has already been observed by Todisco et al [43], which attributed this to the different conditions of the soil surface. The climatic conditions (particularly precipitation and air temperature) roughly described by the variable "period" can affect the dynamics of various soil properties such as roughness [44], infiltration and bulk density [45,46], and hydraulic conductivity [47]. Therefore, even if the RF model already explicitly considers essential features such as Q R and R, the "period" becomes important to allow the model to evaluate the seasonal variability of their effect on soil loss.…”
Section: Discussionmentioning
confidence: 99%
“…There have four frequently-used empirical models, including Brooks-Corey model, Gardner model, Van-Genuchten model (VG model for short) and Gardner-Russo model. Others researched on domestic and overseas soil hydrodynamic parameters and found that VG model have not only better fitting effect but also can link with the mechanical composition and bulk density of soil [18].…”
Section: One-dimensional Consolidation Theory Of Unsaturated Soilmentioning
confidence: 99%
“…The BEST method is widely used [15] due to its simplicity, robustness, accuracy and versatility of application since it enables the estimate of soil hydraulic proprieties (water retention curve and hydraulic conductivity function) based on simple field infiltration measurements, information on the soil particlesize distribution and a few physical parameters. Specifically, the comparative analysis between different types of soil and crop management systems was based on the following parameters, all derived from the hydraulic characterisation obtained by the BEST method: saturated hydraulic conductivity (K S ), sorptivity (S), scale parameter of the Van Genuchten retention curve (h g ), two soil porosity indicators [i.e., the flow-weighted mean pore size (λ m ) and the numbers of pores per unit area (N 0 )] and four capacity-based indicators [i.e., macroporosity (P MAC ), air capacity (A C ), relative filed capacity (R FC ) and plant available water content (AWC)] [16][17][18]. The main goal was to identify whether the different LTAEs considered have relevant roles in conditioning the soil's physical-hydraulic properties in the specific climatic and pedological conditions of the study area.…”
Section: Introductionmentioning
confidence: 99%