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dc.contributor.authorKoch, Timo-
dc.contributor.authorHeck, Katharina-
dc.contributor.authorSchröder, Natalie-
dc.contributor.authorClass, Holger-
dc.contributor.authorHelmig, Rainer-
dc.date.accessioned2019-02-13T11:25:14Z-
dc.date.available2019-02-13T11:25:14Z-
dc.date.issued2018de
dc.identifier.issn1539-1663-
dc.identifier.other517767511-
dc.identifier.urihttp://nbn-resolving.de/urn:nbn:de:bsz:93-opus-ds-102589de
dc.identifier.urihttp://elib.uni-stuttgart.de/handle/11682/10258-
dc.identifier.urihttp://dx.doi.org/10.18419/opus-10241-
dc.description.abstractWe 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 DuMux 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.en
dc.language.isoende
dc.relation.uridoi:10.2136/vzj2017.12.0210de
dc.rightsinfo:eu-repo/semantics/openAccessde
dc.subject.ddc624de
dc.titleA new simulation framework for soil-root interaction, evaporation, root growth, and solute transporten
dc.typearticlede
ubs.fakultaetBau- und Umweltingenieurwissenschaftende
ubs.fakultaetFakultätsübergreifend / Sonstige Einrichtungde
ubs.institutInstitut für Wasser- und Umweltsystemmodellierungde
ubs.institutFakultätsübergreifend / Sonstige Einrichtungde
ubs.publikation.seiten21de
ubs.publikation.sourceVadose zone journal 17 (2018), No. 170210de
ubs.publikation.typZeitschriftenartikelde
Enthalten in den Sammlungen:02 Fakultät Bau- und Umweltingenieurwissenschaften

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