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Published in Soil Sci Soc Am J 26:552-556 (1962)
© 1962 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Organic Matter Decomposition as Influenced by Oxygen Level and Flow Rate of Gases in the Constant Aeration Method1

J. F. Parr and H. W. Reuszer2

ABSTRACT

Laboratory experiments were conducted to determine the rate of decomposition of wheat straw added to soil when continuous aeration was conducted with N2-O2 gas mixtures containing 0, 0.5, 1.0, 2.5, 5.0, and 21% oxygen at flow rates of 1/8, 1/4, 1/2, 1, and 2 liters per hour. Rates of decomposition and total decomposition were followed by determination of wheat straw carbon evolved as CO2.

Total decomposition at all oxygen levels varied directly with aeration flow rate, except for the 0% level where an inverse relationship was observed.

Microbial activity at the 21% oxygen level was greatly stimulated as flow rate increased from 1/8 through 2 liters per hour.

A rapid increase in microbial activity occurred for the 0.5, 1.0, 2.5, and 5.0% oxygen levels as flow rate increased from 1/8 through 1/2 liters per hour, however, little increase in CO2 production was observed at higher flow rates.


NOTES

1 Journal Paper No. 1864 Purdue University Agr. Exp. Sta., Lafayette, Ind. Contribution from the Dept. of Agronomy. Part of a thesis submitted by the senior author in partial fulfillment of the requirements of the Ph.D. degree.

2 Research Associate, Plant Nutrition Laboratory, The University of Michigan, Ann Arbor, formerly Instructor, Purdue University Agr. Exp. Sta.; and Associate Microbiologist, respectively.

Received for publication January 9, 1962. Accepted for publication March 29, 1962.







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