Application of smoothed particle hydrodynamics (SPH) and pore morphologic model to predict saturated water conductivity from X-ray CT imaging in a silty loam Cambisol

被引:22
作者
Dal Ferro, N. [1 ]
Strozzi, A. G. [2 ]
Duwig, C. [3 ]
Delmas, P. [4 ]
Charrier, P. [5 ]
Morari, F. [1 ]
机构
[1] Univ Padua, Dept Agron Food Nat resources Anim & Environm, Agripolis, I-35020 Padua, Italy
[2] Ciudad Univ, CCADET, UNAM, Mexico City, DF, Mexico
[3] UJF Grenoble 1, IRD, CNRS, G INP,LTHE,UMR 5564, F-38041 Grenoble 9, France
[4] Univ Auckland, Dept Comp Sci, Auckland 1, New Zealand
[5] UJF, Lab 3SR, CNRS, UMR,INP, F-38041 Grenoble 9, France
基金
欧盟地平线“2020”;
关键词
X-ray computed microtomography; Saturated hydraulic conductivity; Soil structure; Pore size distribution; PEDOTRANSFER FUNCTIONS; HYDRAULIC CONDUCTIVITY; SOLUTE TRANSPORT; 3D SHAPES; COMPACTNESS; FLOW; PERMEABILITY; TOMOGRAPHY; MACROPORES; PHYSICS;
D O I
10.1016/j.geoderma.2015.04.019
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
This study aims to estimate saturated hydraulic conductivity in a silty loam soil and-compare modelled data with experimental ones. The flow characteristics of twelve undisturbed soil cores (5 cm in diameter x 6 cm high) were measured in the laboratory after performing X-ray computed microtomography (microCT) analysis. MicroCT 3D imaging was integrated with an existing pore morphologic model and a numerical simulation based on mesh-free smoothed particle hydrodynamics (SPH) to calculate the water flow through the macropore network (pores >40 mu m). Results showed that the proposed SPH method was able to predict hydraulic conductivity of large-sized samples as falling in the range of the experimental ones. By contrast the morphologic model generally underestimated the water flow and was slightly affected by the pore shape. Increasing microCT imaging resolution and expanding the variability with other soil types will improve the understanding of the role of micropore size and morphology on water conductivity. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:27 / 34
页数:8
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