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Published in Soil Sci Soc Am J 48:119-125 (1984)
© 1984 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Analysis of Long-Term Water Table Depth Records from a Hydrosequence of Soils in Central Ohio1

T. M. Zobeck and A. Ritchie, Jr.2

ABSTRACT

Water table depths and precipitation were measured over a 10-yr period on four adjacent forested soils in central Ohio. The soils included a hydrosequence of well, moderately well, poorly, and very poorly drained fine-textured soils. Graphs describing the probability of observing water tables during consecutive 2-week (semi-monthly) intervals, by soil depth class, were compared with estimates reported on USDA-Soil Conservation Service forms SOIL-SOI-5 and a method proposed in the Soil Survey Manual. All soils had a probability of an observed water table within 50 cm of the soil surface. Water tables were observed in all soils, with the exception of the well drained soil, within 25 cm of the surface, 10% of the time or more, over a 12- or 14-week period in the late winter and spring.


NOTES

1 Contribution from the Dep. of Agronomy, Ohio State University, Columbus, and Ohio Agric. Res. & Development Center, Columbus, OH 43210. Salaries and research support provided by State and Federal Funds appropriated to the Ohio Agric. Res. & Development Center, The Ohio State University. Approved for publication as Journal Article no. 65-83 OARDC, Wooster, OH 44691.

2 Assistant Professor, Ohio Agric. Res. & Dev. Center, Ohio State University, and Soil Survey Coordinator, Ohio Dep. of Natural Resources, Div. of Soil & Water Conservation.

Received for publication May 17, 1983. Accepted for publication August 15, 1983.




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C. P. Morgan and M. H. Stolt
Soil Morphology-Water Table Cumulative Duration Relationships in Southern New England
Soil Sci. Soc. Am. J., March 29, 2006; 70(3): 816 - 824.
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Copyright © 1984 by the Soil Science Society of America.