Abstract
A similarity solution exists in two-dimension when a constant flux is imposed along a line source. Following the R. R. Bruce and A. Klute method in one-dimension, this similarity solution can be used to determine the soil-water diffusivity. The application of the method is illustrated for a sandy loam. The advantage of the method is that the slope of the moisture profile is finite and easily measured, even close to the source.
Original language | English |
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Pages (from-to) | 387-390 |
Number of pages | 4 |
Journal | Soil Science Society of America Proceedings |
Volume | 39 |
Issue number | 3 |
Publication status | Published - May 1975 |
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TWO-DIMENSIONAL SIMILARITY SOLUTION : THEORY AND APPLICATION TO THE DETERMINATION OF SOIL-WATER DIFFUSIVITY. / Turner, Neil C.; Parlange, Jean Yves.
In: Soil Science Society of America Proceedings, Vol. 39, No. 3, 05.1975, p. 387-390.Research output: Contribution to journal › Article
TY - JOUR
T1 - TWO-DIMENSIONAL SIMILARITY SOLUTION
T2 - THEORY AND APPLICATION TO THE DETERMINATION OF SOIL-WATER DIFFUSIVITY.
AU - Turner, Neil C.
AU - Parlange, Jean Yves
PY - 1975/5
Y1 - 1975/5
N2 - A similarity solution exists in two-dimension when a constant flux is imposed along a line source. Following the R. R. Bruce and A. Klute method in one-dimension, this similarity solution can be used to determine the soil-water diffusivity. The application of the method is illustrated for a sandy loam. The advantage of the method is that the slope of the moisture profile is finite and easily measured, even close to the source.
AB - A similarity solution exists in two-dimension when a constant flux is imposed along a line source. Following the R. R. Bruce and A. Klute method in one-dimension, this similarity solution can be used to determine the soil-water diffusivity. The application of the method is illustrated for a sandy loam. The advantage of the method is that the slope of the moisture profile is finite and easily measured, even close to the source.
UR - http://www.scopus.com/inward/record.url?scp=0016508579&partnerID=8YFLogxK
M3 - Article
VL - 39
SP - 387
EP - 390
JO - Soil Science Society of America Proceedings
JF - Soil Science Society of America Proceedings
SN - 0038-0776
IS - 3
ER -