Can fill-and-spill subsurface flow be represented by a moisture-dependent anisotropic permeability tensor in Richards equation-based models with coarse spatial resolution?

Esther Xu Fei; Ciaran Harman

doi:https://doi.org/10.5194/egusphere-egu21-6094

[Back] [Session HS8.3.1]

EGU21-6094, updated on 04 Mar 2021

https://doi.org/10.5194/egusphere-egu21-6094

EGU General Assembly 2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Can fill-and-spill subsurface flow be represented by a moisture-dependent anisotropic permeability tensor in Richards equation-based models with coarse spatial resolution?

Esther Xu Fei¹ and Ciaran Harman^1,2

Esther Xu Fei and Ciaran Harman

¹Environmental Health and Engineering, Johns Hopkins University, Baltimore, Maryland, United States of America
²Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland, United States of America

How to cite: Xu Fei, E. and Harman, C.: Can fill-and-spill subsurface flow be represented by a moisture-dependent anisotropic permeability tensor in Richards equation-based models with coarse spatial resolution?, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-6094, https://doi.org/10.5194/egusphere-egu21-6094, 2021.

This abstract has been withdrawn on 27 Apr 2021.