Research Article
Jun 1976
Saturated and Unsaturated Flow to Parallel Drains
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VIEW THE REPLYAuthors: R. Wayne Skaggs and Yau-K. TangAuthor Affiliations
Publication: Journal of the Irrigation and Drainage Division
Volume 102, Issue 2
Abstract
Richards equation for transient two-dimensional flow during drainage was solved using numerical methods and the solutions compared to solutions of the more approximate Boussinesq equation. The effect of field variability of the soil properties on solutions to the Richards equation was also examined. For the cases studied, the hydraulic head distributions predicted by the Richards equation were in general agreement with the D-F assumptions except for times near t = 0. Convergence near drainage ditches is more critical immediately after drainage begins than for latter times. It results in a surface of seepage for ditches and water standing over the drain for drain tubes. When convergence near the drain is accounted for, solutions to the Boussinesq equation can be used to adequately predict drawdown for design purposes. Unless enough measurements are made to define field-effective values of the unsaturated soil-water properties, there is little to be gained by solving the Richards equation rather than using simpler approximate methods for drawdown prediction.
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Published In
Journal of the Irrigation and Drainage Division
Volume 102 • Issue 2 • June 1976
Pages: 221 - 238
Copyright
© 1976 American Society of Civil Engineers.
History
Published in print: Jun 1976
Published online: Feb 11, 2021
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Affiliations
R. Wayne Skaggs
Assoc. Prof., Dept. of Biological and Agr. Engrg, North Carolina State Univ., Raleigh, N.C.
Yau-K. Tang
Grad. Asst., Dept. of Biological and Agr. Engrg., North Carolina State Univ., Raleigh, N.C.
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