| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8365233 | Soil Biology and Biochemistry | 2013 | 4 Pages |
Abstract
⺠CH4 and N2O production show negative temperature response in a humic podzol. ⺠Differences between coarse surface organic matter and underlying peat exist for CH4, but not for N2O. ⺠Temperature sensitivity of intact cores opposes in-situ field observations.
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Authors
R.T.E. Mills, N. Dewhirst, A. Sowerby, B.A. Emmett, D.L. Jones,