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Water Movement in a Finite Layer: Absorption for Constant Water Content at the Surfaces1

✍ Scribed by Hornung, U.; Parlange, J.-Y.; Hogarth, W.L.; Connell, L.D.; Peters, R.

Book ID
121520168
Publisher
The American Society of Agronomy
Year
1987
Tongue
English
Weight
176 KB
Volume
51
Category
Article
ISSN
0361-5995

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Here &) = e. (Jay = 0 as desired; and the result of Tosun and Willis, more properly noted as (d.$ # ($), is also obtained. Thus it can be seen that the phase and intrinsic phase averages of the a-phase deviation are zero independently of the definition used for this deviation at a point in the P-pha