Sequential infiltration analysis of infiltration curves measured with disc infiltrometer in layered soils

JOURNAL OF HYDROLOGY

卷:600

Article

Moret-Fernandez, D.^1,2  Latorre, B.¹  Lassabatere, L.³  Di Prima, S.⁴  Castellini, M.⁵  Yilmaz, D.⁶  Angulo-Jaramilo, R.³ 

[1] CSIC, Estn Expt Aula, Dept Suelo & Agua Dei, POB 13034, Zaragoza 50080, Spain

[2] CSIC, Inst Pirenaico Ecol, Av Montanana 1005,POB 13034, Zaragoza 50080, Spain

[3] Univ Claude Bernard Lyon 1, Univ Lyon, CNRS, ENTPE,UMR5023 LEHNA, F-69518 Vaulx En Velin, France

[4] Univ Sassari, Dept Agr Sci, Viale Italia 39, I-07100 Sassari, Italy

[5] Council Agr Res & Econ, Res Ctr Agr & Environm CREA AA, Rome, Italy

[6] Munzur Univ, Engn Fac, Civil Engn Dept, TR-62000 Tunceli, Turkey

关键词: Sorptivity;    Hydraulic conductivity;    Infiltration;    Heterogeneous soil profiles;   

DOI  :  10.1016/j.jhydrol.2021.126542

来源: Elsevier

【 摘 要 】

The soil sorptivity, S, and saturated hydraulic conductivity, K-s, can be estimated from the inverse analysis of a cumulative infiltration curve using the quasi-exact implicit (QEI) formulation or its corresponding 4-Terms (4T) approximation. Although these models consider the soil as homogeneous media, there is no information about how heterogeneous profiles can affect the inferred soil properties. This work analyzes the influence of layered soils on K-s and S estimates using QEI and 4T models, and designs a new procedure for treating infiltration curves measured on layered soil profiles. The Sequential Infiltration Analysis (SIA) method considers a sequence of increasing time series from the cumulative infiltration data to estimate K-s and S, and its corresponding RMSE as a function of the number of samples used. A procedure to estimate the thickness of the upper uniform soil layer from the estimated wetting front advance (WFA) is also reported. The SIA method was applied on: (i) synthetic homogeneous profiles of loam soil and six layered profiles involving a 1, 2 and 3 cm thickness loam layer over silty or sandy loam soils, respectively, (ii) stratified laboratory soil columns, and (iii) 20 experimental infiltrations performed in a semiarid region of North-Eastern Spain. Similar results were found between QEI and 4T models for all cases. Erroneous estimates of K-s and S were observed when the total infiltration time series was considered for the analysis, regardless of the presence of soil layering. In opposite, estimates improved when the SIA method was applied to the layered systems. The SIA method exploits the fact that the RMSE increases when the wetting front reaches the interface between the soil layers. Such increase allows: (i) detection of the soil heterogeneity, (ii) determination of the infiltration time, t(o), required for the wetting front to reach the lower layer, and, (iii) accurate estimates of the upper layer K-s and S along with its thickness. Laboratory experiments on layered soils and field measurements demonstrated that the SIA method could be satisfactorily applied on different curves with contrasting shapes and magnitudes. Although soil layering encountered on most field samplings restricted the treatment of the observed infiltrations to short-medium times, the SIA method allowed robust estimates of K-s and S. These results indicate that the proposed method is a promising tool for characterizing the hydraulic properties of layered and heterogeneous soil profiles.

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