Abstract
The 169 forested plots across Minnesota, Wisconsin and Michigan were geographically stratified into 5 zones, with wet sulfate deposition increasing from 156 (zone 1) to 380 (zone 5) equiv..ha-1.yr-1. Total S concentrations, adjusted for N levels, indicated higher concentrations in E than in W zones in both the upper mineral soil (c. 0.0152 and 0.0133% S, respectively) and forest floor (c. 0.124 and 0.113% S, respectively), ie forest soil S levels reflect geographic gradients in atmospheric sulfate deposition. Total C and N concentrations and C:N and C:S ratios were affected by vegetation type. Jack pine Pinus banksiana and red pine P. resinosa mineral soil had lower concentrations of C and N compared with balsam fir Abies balsamea, maple Acer spp and aspen Populus tremuloides. Forest floor C and N showed no clear pattern. -Authors
Original language | English (US) |
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Pages (from-to) | 1386-1391 |
Number of pages | 6 |
Journal | Canadian Journal of Forest Research |
Volume | 18 |
Issue number | 11 |
DOIs | |
State | Published - 1988 |
ASJC Scopus subject areas
- Global and Planetary Change
- Forestry
- Ecology