A New Simulation Framework for Soil-Root Interaction, Evaporation, Root Growth, and Solute Transport

被引:34
|
作者
Koch, Timo [1 ]
Heck, Katharina [1 ]
Schroeder, Natalie [1 ,2 ,3 ]
Class, Holger [1 ]
Helmig, Rainer [1 ]
机构
[1] Univ Stuttgart, Dept Hydromech & Modelling Hydrosyst, Pfaffenwaldring 61, D-70569 Stuttgart, Germany
[2] Voith Paper GmbH & Co KG, St Poltener Str 43, D-89522 Heidenheim, Germany
[3] Forschungszentrum Julich, Inst Bio & Geosci Agrosphere IBG 3, D-52425 Julich, Germany
关键词
Abbreviations: DUNE; Distributed Unified Numerics Environment; PDE; partial differential equation; MULTIPHASE MULTICOMPONENT PROCESSES; GENERIC GRID INTERFACE; HYDRAULIC CONDUCTIVITY; POROUS-MEDIA; WATER TRANSPORT; NUMERICAL-SIMULATION; NEUTRON-RADIOGRAPHY; MATHEMATICAL-MODELS; FLOW; ARCHITECTURE;
D O I
10.2136/vzj2017.12.0210
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We have developed a general model concept and a flexible software framework for the description of plant-scale soil-root interaction processes including the essential fluid mechanical processes in the vadose zone. The model was developed in the framework of non-isothermal, multiphase, multicomponent flow and transport in porous media. The software is an extension of the open-source porous media flow and transport simulator DuMu(x) to embedded mixed-dimensional coupled schemes. Our coupling concept allows us to describe all processes in a strongly coupled form and adapt the complexity of the governing equations in favor of either accuracy or computational efficiency. We have developed the necessary numerical tools to solve the strongly coupled nonlinear partial differential equation systems that arise with a locally mass conservative numerical scheme even in the context of evolving root architectures. We demonstrate the model concept and its features, discussing a virtual hydraulic lift experiment including evaporation, root tracer uptake on a locally refined grid, the simultaneous simulation of root growth and root water uptake, and an irrigation scenario comparing different models for flow in unsaturated soil. We have analyzed the impact of evaporation from soil on the soil water distribution around a single plant's root system. Moreover, we have shown that locally refined grids around the root system increase computational efficiency while maintaining accuracy. Finally, we demonstrate that the assumptions behind the Richards equation may be violated under certain conditions.
引用
收藏
页数:21
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