Abstract
All the major physiographic features in the mire - a raised bog, spring fen, and intervening water track - are zones of groundwater discharge during parts of the year. Acidic bog waters are neutralized below 0.5 m in the peat profile. A small change in the volume of groundwater discharge in the peatland may therefore be sufficient to neutralize the acidic waters on the bog surface and greatly affect the vegetation.-from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 743-754 |
| Number of pages | 12 |
| Journal | Journal of Ecology |
| Volume | 75 |
| Issue number | 3 |
| DOIs | |
| State | Published - 1987 |