TY - JOUR
T1 - Absorption of water by soil
T2 - the constant flux boundary condition.
AU - White, I.
AU - Smiles, D. E.
AU - Perroux, K. M.
PY - 1979
Y1 - 1979
N2 - Experiments for a fine sand show that the surface water content, movement of the wetting front, and the water content profiles may be predicted from the soil water diffusivity function using the notion of the flux-concentration relation of Philip (1973). Reduced space and time variables are introduced. Use of these variables greatly simplifies treatment of the system.- from Author
AB - Experiments for a fine sand show that the surface water content, movement of the wetting front, and the water content profiles may be predicted from the soil water diffusivity function using the notion of the flux-concentration relation of Philip (1973). Reduced space and time variables are introduced. Use of these variables greatly simplifies treatment of the system.- from Author
UR - http://www.scopus.com/inward/record.url?scp=0018650846&partnerID=8YFLogxK
U2 - 10.2136/sssaj1979.03615995004300040006x
DO - 10.2136/sssaj1979.03615995004300040006x
M3 - Article
AN - SCOPUS:0018650846
SN - 0361-5995
VL - 43
SP - 659
EP - 664
JO - Soil Science Society of America, Journal
JF - Soil Science Society of America, Journal
IS - 4
ER -