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HESS | Articles | Volume 22, issue 7
Hydrol. Earth Syst. Sci., 22, 3639-3662, 2018
https://doi.org/10.5194/hess-22-3639-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Hydrol. Earth Syst. Sci., 22, 3639-3662, 2018
https://doi.org/10.5194/hess-22-3639-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 06 Jul 2018

Research article | 06 Jul 2018

Ecohydrological particle model based on representative domains

Conrad Jackisch and Erwin Zehe
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Cited articles  
Allroggen, N., Jackisch, C., and Tronicke, J.: Four-dimensional gridding of time-lapse GPR data, in: IEEE 9th International Workshop on Advanced Ground Penetrating Radar (IWAGPR), 28–30 June 2017, Edinburgh, UK, 1–4, https://doi.org/10.1109/IWAGPR.2017.7996067, 2017. a
Bashford, K. E., Beven, K. J., and Young, P. C.: Observational data and scale-dependent parameterizations: explorations using a virtual hydrological reality, Hydrol. Process., 16, 293–312, https://doi.org/10.1002/hyp.339, 2002. a
Bear, J.: Dynamics of Fluids in Porous Media, in: Vol. 120, Dover Publications, Dover, https://doi.org/10.1097/00010694-197508000-00022, 1975. a
Berkowitz, B., Cortis, A., Dentz, M., and Scher, H.: Modeling non-Fickian transport in geological formations as a continuous time random walk, Rev. Geophys., 44, RG2003, https://doi.org/10.1029/2005RG000178, 2006. a
Beucher, S. and Lantuejoul, C.: Use of Watersheds in Contour Detection, in: International Workshop on Image Processing: Real-time Edge and Motion Detection/Estimation, September 1979, Rennes, France, http://cmm.ensmp.fr/~beucher/publi/watershed.pdf (last access: 3 July 2018), 1979. a
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We present a Lagrangian model for non-uniform soil water dynamics. It handles 2-D diffusion (based on a spatial random walk and implicit pore space redistribution) and 1-D advection in representative macropores (as film flow with dynamic interaction with the soil matrix). The interplay between the domains is calculated based on an energy-balance approach which does not require any additional parameterisation. Model tests give insight into the evolution of the non-uniform infiltration patterns.
We present a Lagrangian model for non-uniform soil water dynamics. It handles 2-D diffusion...
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