ESTIMATING UNSATURATED SOIL HYDRAULIC-PROPERTIES FROM TENSION DISC INFILTROMETER DATA BY NUMERICAL INVERSION

Citation
J. Simunek et Mt. Vangenuchten, ESTIMATING UNSATURATED SOIL HYDRAULIC-PROPERTIES FROM TENSION DISC INFILTROMETER DATA BY NUMERICAL INVERSION, Water resources research, 32(9), 1996, pp. 2683-2696
Citations number
42
Categorie Soggetti
Limnology,"Environmental Sciences","Water Resources
Journal title
ISSN journal
00431397
Volume
32
Issue
9
Year of publication
1996
Pages
2683 - 2696
Database
ISI
SICI code
0043-1397(1996)32:9<2683:EUSHFT>2.0.ZU;2-A
Abstract
Tension disc infiltrometers are becoming increasingly popular devices for in situ measurement of the unsaturated hydraulic properties of soi l. Tension infiltration data are generally used to evaluate the parame ters K-s and alpha in Gardner's exponential model of the unsaturated h ydraulic conductivity. Either two measurements using different disc di ameters or measurements with a single disc but using multiple pressure heads are then used. In this paper we describe a parameter estimation procedure which combines the Levenberg-Marquardt nonlinear parameter optimization method involving weighted least squares, with a quasi-thr ee-dimensional numerical model which solves the variably saturated flo w equation. By numerical inversion of Richards' equation the unknown p arameters in van Genuchten's model of the unsaturated soil-hydraulic p roperties are estimated from observed cumulative infiltration data dur ing transient water flow. Additional measurements of the pressure head or water content, as well as a penalty function for constraining the unknown parameters to remain in some feasible region (Bayesian estimat ion), can be optionally included into the parameter estimation procedu re. The problem of optimal sampling design, that is, selecting the bes t points in space and time for making measurements, is addressed by st udying the sensitivity of the objective function to changes in the opt imized hydraulic parameters. We calculate objective functions based on available cumulative infiltration, pressure head, and water content m easurements and also on several combinations of these data. The behavi or of the objective function in three-dimensional parameter space is e valuated by means of a series of two-dimensional response surfaces. Th e utility of the parameter estimation procedure is demonstrated using numerically generated data. The sensitivity of the procedure to differ ent initial estimates of the model parameters is also discussed.