Abstract
One of the major mechanisms for N loss in these systems is through biological oxidation and reduction of N species in the aerobic and anaerobic sediment zones, coupled with exchange processes between these zones. These mechanisms were measured using flooded, intact sediment columns and batch incubations with bulk sediments collected from a hypereutrophic lake. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1156-1163 |
| Number of pages | 8 |
| Journal | Soil Science Society of America Journal |
| Volume | 57 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1993 |
ASJC Scopus subject areas
- Soil Science