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ABSTRACT
A field plot of Hanford sandy loam was ponded for 2 weeks with a solution of KNO3 and Ca(NO3)2 containing 100 ppm NO3-N in order to measure short term denitrification rates as well as growth and distribution of bacteria capable of reducing nitrate to nitrite and/or N2O and N2.
Denitrifying bacteria (101–2.9 x 104/g soil) generally decreased in number with depth and time and were not as numerous as nitrate reducers (101–6.9 x 105/g soil).
In the top 60 cm of soil, the concentration of NO2–-N in soil solution corresponded to minima in NO3–-N, suggesting that NO3– reduction gave rise to the NO2–. Denitrification rates calculated for the top 16 cm of water-saturated soil were estimated to range from 0.013 to 0.046 µg N/hour g–1. The highest value was about 80% of that measured in a laboratory soil column studied previously. This difference in denitrification rates may be due to lower soil carbon content in the field.
Key Words: denitrifiers ammonium oxidizers nitrite oxidizers microbial ecology
1 Contribution from the College of Natural Resources, University of California, Berkeley. Supported by NSF-RANN Grant No. GI 34733X, Nitrate in effluents from irrigated lands, and the Kearney Foundation of Soil Science.
2 Assistant Research Biochemist, Staff Research Associate, Assistant Research Chemist, and Professor of Soil Biology, respectively, Dept. of Soils & Plant Nutrition, Univ. of Calif., Berkeley, 94720.
Received for publication March 13, 1974.
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