Abstract
The results of a comparison of two models of the motion of soil moisture are presented. It is shown that under certain conditions one of them describes the motion of moisture in the direction of a moisture gradient.
Similar content being viewed by others
References
E. S. Romm, Filtration Properties of Fissured Rocks [in Russian], Nedra, Moscow, 1966.
V. A. Yangarber, “Combined problem for the modified equation of moisture transport,” PMTF [Journal of Applied Mechanics and Technical Physics], no. 1, 1967.
Author information
Authors and Affiliations
Additional information
In conclusion, we note that, knowing the parameters of problem (1) and measuring λ, we can determine the coefficienta −2 in Eq. (1) from (3) (or (4)).
Rights and permissions
About this article
Cite this article
Yangarber, V.A. Comparison of two linear models of soil moisture dynamics. J Appl Mech Tech Phys 10, 323–326 (1969). https://doi.org/10.1007/BF00913125
Issue Date:
DOI: https://doi.org/10.1007/BF00913125