Dynamic coupling between soil properties and water content in shrink-swell soils: Effects on surface hydrologic partitioning-Reference-Cited by-同舟云学术

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Dynamic coupling between soil properties and water content in shrink-swell soils: Effects on surface hydrologic partitioning

Published:2024-02 Issue: Volume:184 Page:104630
ISSN:0309-1708
Container-title:Advances in Water Resources
language:en
Short-container-title:Advances in Water Resources

Author:

Souza Rodolfo^ORCID,Ghannam Khaled^ORCID,Calabrese Salvatore^ORCID

Publisher

Elsevier BV

Reference46 articles.

1. Evaporation from soil shrinkage cracks;Adams;Soil Sci. Am. J.,1964

2. Dual-permeability model improvements for representation of preferential flow in fractured clays;Aguilar-López;Water Resour. Res.,2020

3. An analysis of the soil moisture feedback on convective and stratiform precipitation;Alfieri;J. Hydrometeorol.,2008

4. Macropores and water flow in soils revisited;Beven;Water Resour. Res.,2013

5. Shrinkage geometry of a heavy clay soil at various stresses;Bronswijk;Soil Sci. Am. J.,1990

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