|
|
||||||||
ABSTRACT
A method using an interfaced gas chromatograph-mass spectrometer (GC-MS) is described for measuring the amount of N2O and N2 derived during denitrification from tagged 15NO3– and from 14NO3–, the latter of which is produced during mineralization of soil organic matter. More mineralization and less denitrification was noted with the respective order related to air-filled pore content: 10%, 5%, 0 (saturated). Denitrification measured directly from the cumulative emissions of N2O and N2 was considerably underestimated by comparison to measuring denitrification by loss of 15NO3–.
Key Words: nitrate 15N nitrous oxide soil gases
1 Contribution of the Dep. of Soil and Environ. Sci., Univ. of California, Riverside, CA 92521. This research was supported by the Natl. Sci. Found. RANN, Grant no. GI-34733X.
2 Associate Professor of Soil Science, Staff Research Associate, and Professor of Soil Physics, respectively.
Received for publication August 15, 1978.
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Soil Science Society of America Journal | Journal of Plant Registrations | The Plant Genome | |||