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Published in Soil Sci Soc Am J 35:316-319 (1971)
© 1971 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Soil Structure and Hydraulic Conductivity of Adjacent Virgin and Cultivated Pedons at two Sites: A Typic Argiudoll (silt loam) and a Typic Eutrochrept (clay)1

J. Bouma and F. D. Hole2

ABSTRACT

Soil morphology and hydraulic conductivity (K) of principal soil horizons of paired virgin and cultivated soil pedons were studied at two sites: a Tama silt loam (Typic Argiudoll) and an Oshkosh clay (Typic Eutrochrept). About a century of cultivation had led to reduction of K (measured by the Bouwer double-tube method) in the upper part of the solum below the Ap. Corresponding changes in soil morphology are noted. The reductions in K are paralleled by increases in bulk density and decreases in porosity and organic matter content in the soil horizons. At a depth of 80 to 90 cm in the clay soil, K increased apparently as a result of formation of interpedal voids as the alfalfa crop (Medicago sativa L.) extracted moisture.


NOTES

1 Contribution from the Soil Survey Div., Wisconsin Geol. & Natural History Survey, Univ. Ext., and the Dept. of Soil Sci., Univ, of Wisconsin, Madison. This project was supported by the Geol. & Natural History Survey and by the Wisconsin State Dept. of Nat. Res., in cooperation with the Dept. of Soil Sci. Published with the approval of the Director of the Wisconsin Geol. & Natural History Survey and the Director of the Wis. Agr. Exp. Sta.

2 Visiting Assistant Professor and Professor of Soil Science, respectively, Wisconsin Geol. & Natural History Survey, and Dept. of Soil Science.

Received for publication April 24, 1970. Accepted for publication December 1, 1970.




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A. Rachman, S. H. Anderson, C. J. Gantzer, and E. E. Alberts
Soil Hydraulic Properties Influenced by Stiff-Stemmed Grass Hedge Systems
Soil Sci. Soc. Am. J., July 1, 2004; 68(4): 1386 - 1393.
[Abstract] [Full Text] [PDF]




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Copyright © 1971 by the Soil Science Society of America.