SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 56:1267-1271 (1992)
© 1992 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Rasiah, V.
Right arrow Articles by Kohl, R. A.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Rasiah, V.
Right arrow Articles by Kohl, R. A.
Agricola
Right arrow Articles by Rasiah, V.
Right arrow Articles by Kohl, R. A.

Assessment of Functions and Parameter Estimation Methods in Root Water Uptake Simulation

V. Rasiah*

Dep. of Land Resource Science, Univ. of Guelph, Guelph, Ontario, N1G 2W1, Canada

G. C. Carlson and R. A. Kohl

Dep. of Plant Science, South Dakota State Univ., Brookings, SD 57007

*Corresponding author.

ABSTRACT

Limited information is available on the influence of estimates of parameters of the root water uptake (RWU) function on RWU simulation in macroscopic RWU modeling. This study was conducted to assess the influence of (i) parameter estimation methods, linear vs. nonlinear, and (ii) the type of RWU functions, continuous vs. discontinuous, on the estimates of RWU parameters and RWU simulation. The model calibration and validation were carried out using the data for soybean [Glycine max (L.) Merr.] grown in large soil columns. The estimates of the RWU parameters varied with the estimation method used or the type of function used. The simulations in soil water content ({theta}v) and RWU distribution across space and time varied with the estimates of the parameters used in the flow model. The simulations in {theta}v produced with the estimates from the nonlinear estimation method agreed more closely with the corresponding measured values than did those produced with the estimates from the linear method. A similar trend was observed for the discontinuous vs. continuous functions. The differences in residual sum of squares between the linear vs. nonlinear estimation methods, and that between the continuous vs. discontinuous functions, were significant. The accuracy of the simulations in {theta}v and RWU increased significantly using the nonlinear parameter estimation method and a discontinuous RWU function.


NOTES

Contribution from the Dep. of Plant Science and South Dakota Agric. Exp. Stn.

Received for publication June 29, 1990.


This article has been cited by other articles:


Home page
Vadose Zone JHome page
H. Fujimaki, Y. Ando, Y. Cui, and M. Inoue
Parameter Estimation of a Root Water Uptake Model under Salinity Stress
Vadose Zone J., January 23, 2008; 7(1): 31 - 38.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
J. A. Vrugt and W. Bouten
Validity of First-Order Approximations to Describe Parameter Uncertainty in Soil Hydrologic Models
Soil Sci. Soc. Am. J., November 1, 2002; 66(6): 1740 - 1751.
[Abstract] [Full Text] [PDF]




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 © 1992 by the Soil Science Society of America.