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 59:344-351 (1995)
© 1995 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 Leummens, H.
Right arrow Articles by Booltink, H. W. G.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Leummens, H.
Right arrow Articles by Booltink, H. W. G.
Agricola
Right arrow Articles by Leummens, H.
Right arrow Articles by Booltink, H. W. G.

Interpreting Differences among Hydraulic Parameters for Different Soil Series by Functional Characterization

H. Leummens, J. Bouma* and H. W. G. Booltink

Department of Soil Science and Geology, Agricultural Univ., P.O. Box 37, 6700 AA Wageningen, the Netherlands

* Corresponding author ( booltink{at}rcl.wau.nl).

ABSTRACT

Using soil survey data for simulation modeling of water regimes and crop growth requires characteristic expressions for hydraulic characteristics of major soil horizons and soil series. It is unclear at present whether: (i) hydraulic functions based on parameter estimation techniques are adequate for simulations in macroporous soils, and (ii) to what extent different soil horizons and series can be pooled to reduce input data in simulation models. These questions were examined using two methods of expressing measured hydraulic conductivity data in computer simulations with previously validated crop models. Both hydraulic conductivity expressions used parameterized equations derived from one-step outflow data for the –5.0 to –60.0 kPa pressure range. For the 0 to –5.0 kPa range, one method used hydraulic conductivities estimated by extrapolating the parameterized functions, whereas the second method used actual crust test data to account for macropore flow. Differences between the two methods were functionally tested by simulating maize (Zea mays L.) yields and fluxes below the root zone in three Costa Rican soil series, using the SWACROP model. Yields were significantly higher when considering structural porosity (Method 2), while fluxes were significantly lower. Thus, extrapolation of one-step outflow data to conditions near saturation seems to be questionable. Using Method 2, maize yields and fluxes below the root zone were compared for three representative soil series to test whether they could be considered as one functional group of soils. Yield data indicated that two rather than one functional group should be distinguished. Flux data were similar for all three series, indicating that only one functional group was necessary.

Received for publication October 28, 1993.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1995 by the Soil Science Society of America.