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Rainfall infiltration into bare soils

Morin, Joseph, Benyamini, Yoram·1977·Water Resources Research

Abstract

Raindrop impact destroys the surface aggregates of soils and gradually forms a continuous crust. Infiltration rates of bare soils are determined by this process. A theoretical model presented previously was tested under field conditions with a sandy loam soil. The effect of the crust's structure was tested under three rainfall intensities and in wetting and drying cycles. The results of the tests confirmed the theoretical model. According to the model potential infiltration rates, in bare soils, can be predicted by the equation It = (Ii ‐ If) ·e−γ ptl + If. The study demonstrated quantitatively that the major factor determining the reduction of infiltration rates is crust formation and not moisture regime.

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Metadata

Authors
Morin, J., & Benyamini, Y.
Venue
Water Resources Research
Published
1977-10
Volume
13
Issue
5
Pages
813-817
ISSN
  • 0043-1397 (ISSN-L)
  • 1944-7973
OpenAlex
W2010010111
Cited by
316
References
0
FWCI
12.10
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Rainfall infiltration into bare soils. https://app.cochat.ai/papers/10.1029/wr013i005p00813
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Morin, J., & Benyamini, Y. (1977). Rainfall infiltration into bare soils. Water Resources Research. https://doi.org/10.1029/wr013i005p00813

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.