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Published in J Environ Qual 3:14-17 (1974)
© 1974 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Soil Profile Conditions of Cattle Feedlots1

Lloyd N. Mielke, Norris P. Swanson and Thomas M. McCalla2

ABSTRACT

Characterization of the conditions that exist in the feedlot surface and soil profile is important to evaluation of the potentials for soil and water pollution. Cattle action and management activities create a dynamic condition in the feedlot. The organic matter surface causes physical and biochemical changes in the soil that are unlike natural or cultivated soils. The feedlot profile can be described as three layers: the organic matter, the interface, and the underlying soil. Measurable characteristics include bulk density, infiltration, and content of organic matter, water, and nitrate-N. Generally, the surface 15.2-cm depth of feedlot soils is compacted and has a high bulk density. Infiltration into the feedlot surface layers is essentially zero. There is no transpiration, and the soilwater content is more uniform through the profile than on cropped land.

Key Words: infiltration • layered soils • organic content


NOTES

1 Contribution from the North Central Region, ARS, USDA, in cooperation with the Nebraska Agr. Exp. Sta., Lincoln. Published as Paper No. 3411, Journal Series, Nebraska Agricultural Experiment Station. A portion of the funds for this research was provided by the Environmental Protection Agency.

2 Soil Scientist, Agricultural Engineer, and Microbiologist, respectively, USDA, Lincoln, Nebraska.

Received for publication February 23, 1973.


This article has been cited by other articles:


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J. J. Miller, T. Curtis, F. J. Larney, T. A. McAllister, and B. M. Olson
Physical and Chemical Properties of Feedlot Pen Surfaces Located on Moderately Coarse- and Moderately Fine-Textured Soils in Southern Alberta
J. Environ. Qual., June 23, 2008; 37(4): 1589 - 1598.
[Abstract] [Full Text] [PDF]




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Copyright © 1974 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.