Mathematical and computational modelling of vegetated soil incorporating hydraulically-driven finite strain deformation

被引:13
|
作者
Woodman, N. D. [1 ]
Smethurst, J. A. [1 ]
Roose, T. [1 ]
Powrie, W. [1 ]
Meijer, G. J. [2 ]
Knappett, J. A. [2 ]
Dias, T. [1 ]
机构
[1] Univ Southampton, Fac Engn & Phys Sci, Southampton SO17 1BJ, Hants, England
[2] Univ Dundee, Sch Sci & Engn, Dundee DD1 4HN, Scotland
基金
英国工程与自然科学研究理事会; 英国生物技术与生命科学研究理事会;
关键词
Slope; Vegetated soil; Roots; Landslide; Large-strain; ROOT WATER-UPTAKE; NUTRIENT-UPTAKE; PLANT-ROOT; SLOPE; ARCHITECTURE; REINFORCEMENT; VALIDATION; RESISTANCE; STABILITY; MOVEMENT;
D O I
10.1016/j.compgeo.2020.103754
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
In this paper a new model for the hydro-mechanical behaviour of rooted soils is developed. It is a physically-based model that couples finite strain soil deformation with unsaturated water and air flow, while improving on existing cohesion-based approaches to mechanical root reinforcement and empirical soil water-uptake approaches typically used to deal with rooted slopes. The model is used to show that the dynamics of soil-water pressure and soil deformation depend strongly on the physics of the root-water uptake and the elasto-plastic soil mechanics. Root water uptake can cause suctions and corresponding soil shrinkage sufficiently large to necessitate a finite-strain approach. Although this deformation can change the intrinsic permeability, hydraulic conductivity remains dominated by the water content. The model incorporates simultaneous air-flow, but this is shown to be unimportant for soil-water dynamics under the conditions assumed in example simulations. The mechanical action of roots is incorporated via a root stress tensor and a simulation is used to show how root tension is mobilised within a swelling soil. The developed model may be used to simulate both laboratory experiments and full-scale vegetated slopes.
引用
收藏
页数:12
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