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LATERAL MOVEMENT AT THE PERIPHERY OF A ONE-DIMENSIONAL FLOW OF WATER
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LATERAL MOVEMENT AT THE PERIPHERY OF A ONE-DIMENSIONAL FLOW OF WATER
LATERAL MOVEMENT AT THE PERIPHERY OF A ONE-DIMENSIONAL FLOW OF WATER
NT
N. C. Turner
N. C. Turner
JP
J.-Y. Parlange
J.-Y. Parlange
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1 August 1974
journal article
research article
Published by
Wolters Kluwer Health
in
Soil Science
Vol. 118
(2)
,
70-77
https://doi.org/10.1097/00010694-197408000-00002
Abstract
An approximate analytical solution for the lateral movement at the periphery of a one-dimensional flow of water without gravity is derived for a source that is a semi-infinite plane. The solution is shown to be valid experimentally for relatively long times for a source with finite length. The theory can be utilized to calculate, and correct for, the additional infiltration due to lateral movement in measurements of water intake in the field; when gravity is present, however, the correction is valid only for short times. An approximate analytical solution for the lateral movement at the periphery of a one-dimensional flow of water without gravity is derived for a source that is a semi-infinite plane. The solution is shown to be valid experimentally for relatively long times for a source with finite length. The theory can be utilized to calculate, and correct for, the additional infiltration due to lateral movement in measurements of water intake in the field; when gravity is present, however, the correction is valid only for short times. © Williams & Wilkins 1974. All Rights Reserved.
Keywords
GRAVITY
PERIPHERY
LATERAL MOVEMENT
DIMENSIONAL FLOW
FLOW OF WATER
SOLUTION
ANALYTICAL
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Open Access
Cited by 19 articles