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 36:644-648 (1972)
© 1972 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 Boersma, L.
Right arrow Articles by Watts, D. G.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Boersma, L.
Right arrow Articles by Watts, D. G.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Boersma, L.
Right arrow Articles by Watts, D. G.

Soil Morphology and Water Table Relations: I. Annual Water Table Fluctuations1

L. Boersma, G. H. Simonson and D. G. Watts2

ABSTRACT

Water table positions with respect to the soil surface and precipitation were measured daily over a 2-year period at representative sites of five soil series comprising the Willamette association of nearly level soils with good to poor natural drainage. All soils had water tables present for some period during the winter. Perched water tables were present near the surface of the two most poorly-drained series most of the winter.

A mathematical model was developed for predicting water table positions on the basis of rainfall input and soil physical characteristics. The model was calibrated with measurements made during the 2 years and then used with rainfall data from the previous 29 years, to reconstruct water table positions as they had occurred in the past. The computer procedure did not apply to the two poorly-drained series because of the presence of an impermeable soil horizon (clay B) near the surface. However, water table positions of these series were estimated satisfactorily by correlation with water table positions on the better-drained series. The average percent of time the water table was above a given level during each month, calculated for the period of 1929 to 1957 showed that for a specific depth and month, the percent of time the water table was above a given level increased as the natural drainage conditions became poorer. The percentages for the 30.4-cm depth during April for example were 1.8, 15.4, 66.7, 81.5, and 92.0, respectively, for the five series. Thus, particular water table regimes are associated with drainage conditions of specific soil series.


NOTES

1 Technical paper 3272 Oregon Agr. Exp. Sta., Corvallis. Contribution from the Dep. of Soil Sci. The information contained in this report was developed during the course of work under Contract no. DA-22-079-eng-356 with the US Army Engineer Waterways Exp. Sta., Vicksburg, Mississippi.

2 Professors, Dep. of Soil Sci., and former Assistant Professor, respectively, Dep. of Agr. Eng., Oregon State Univ., Corvallis, Oregon 97331. Present address of D. G. Watts: Dep. of Agr. Eng., Utah State Univ., Logan, Utah 84321.

Received for publication February 14, 1972. Accepted for publication April 17, 1972.







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 © 1972 by the Soil Science Society of America.