Skip to main content
Book Chapter

Effects Of Freeze-Thaw Cycling On Soil Erosion

  • Gatto L
  • Halvorson J
  • McCool D
  • et al.
Springer US, (2001), 29-55
DOI: 10.1007/978-1-4615-0575-4_3
N/ACitations
Citations of this article
25Readers
Mendeley users who have this article in their library.
Get full text

Abstract

Landscapes evolve as a result of the interactions of topography, climate, hydrology, vegetation conditions, rock-weathering processes, soil conditions, sediment transport and deposition processes, and land use. An integral part of understanding and modeling that evolution must be a knowledge of the spatial and temporal dynamics in soil erodibility and runoff erosivity and how these dynamics affect the mechanics of soil erosion.

Cite

CITATION STYLE

APA

Gatto, L. W., Halvorson, J. J., McCool, D. K., & Palazzo, A. J. (2001). Effects Of Freeze-Thaw Cycling On Soil Erosion. In Landscape Erosion and Evolution Modeling (pp. 29–55). Springer US. https://doi.org/10.1007/978-1-4615-0575-4_3

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free