SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 60:1283-1290 (1996)
© 1996 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wu, L.
Right arrow Articles by Johnsen, K. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wu, L.
Right arrow Articles by Johnsen, K. E.
Agricola
Right arrow Articles by Wu, L.
Right arrow Articles by Johnsen, K. E.

Model Sensitivity to Measured and Estimated Hydraulic Properties of a Zimmerman Fine Sand

L. Wu*

Dep. of Soil and Environmental Sciences, Univ. of California at Riverside, CA 92521

R. R. Allmaras

USDA-ARS and Dep. of Soil, Water, and Climate, Univ. of Minn., St. Paul, MN 55108

J. B. Lamb

Dep. of Soil, Water, and Climate, Univ. of Minn., St. Paul, MN 55108

K. E. Johnsen

USDA-ARS/GPSR, For Collins, CO 80522

*Corresponding author (laowu{at}mail.ucr.edu).

ABSTRACT

Water retention and hydraulic conductivity are necessary for simulating solute transport in process-oriented models because of the fundamental role of water flow. Accuracy and extension of soil hydraulic properties are crucial for using models to give site-specific predictions, yet these evaluations are infrequent and often lack rigor. The objectives of this study were to compare measured and estimated hydraulic properties and their effects on simulation of field soil-water regime. Water contents ({theta}) and hydraulic conductivities (K) at specific matric potentials ({psi}) alternatively measured in the laboratory and field or estimated from other soil properties were fitted to water retention and hydraulic conductivity functions to obtain parameters according to the van Genuchten formulation. The estimated parameters were inputs for the Root Zone Water Quality Model to simulate water movement in a Zimmerman fine sand (mixed, frigid Argic Udipsamment). Simulated and in situ measured water contents were compared to assess methods used for measuring or estimating hydraulic properties. Simulation using hydraulic functions generated from field-measured {theta}({psi}) and K({psi}) was closest to measured total water depth in the 1.5-m profile as well as water contents at the 0.2-m depth. Arbitrary variations of {alpha} and n in the van Genuchten equations had larger effects on {theta}({psi}) and K({psi}) functions compared with variations caused by methods to measure and estimate hydraulic functions. This test demonstrated the crucial role and importance of soil hydraulic properties in simulating water storage and movement even in a sandy soil.


NOTES

Joint contribution of the Minnesota Agric. Exp. Stn. and USDA-ARS. Minnesota Paper no. 21695.

Received for publication January 18, 1995.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1996 by the Soil Science Society of America.