Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9465473 | Waste Management | 2005 | 8 Pages |
Abstract
The characteristics of each of the two composting processes are discussed in detail. Very different mechanisms for emission of CH4 and N2O are proposed for each system. For the windrow system, development of anaerobic zones were thought to be responsible for CH4 release. High N2O emission rates from vermicomposting were ascribed to strongly nitrifying conditions in the processing beds combined with the presence of de-nitrifying bacteria within the worm gut.
Related Topics
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Geotechnical Engineering and Engineering Geology
Authors
A.M. Hobson, J. Frederickson, N.B. Dise,