Table 1.
Response to chronic N deposition | % change | Reference(s) |
---|---|---|
Plant | ||
NPP | +10 | 7 |
Leaf litter production | 0 | 7 |
Leaf litter N concn | +25 | 3 |
Fine root litter | 0 | 4 |
Fine root N concn | 0 | 4 |
Biogeochemical | ||
Forest floor mass | +51 | 3 |
Forest floor turnover | −60 | 3 |
Soil organic matter content | +18 | 3 |
Soil solution NO3− concn | +288 | 3 |
NO3− leaching | +680 | 5 |
Dissolved organic matter leaching | +26 | 5 |
Microbial | ||
Soil respiration | −15 | 4 |
Active microbial biomass (PLFAb) | +23 | 36, 59 |
Phenol oxidase activity | −33 | 36, 59 |
Peroxidase activity | −30 | 36, 59 |
Basidiomycete laccase copy no. | −5 to −8 | 16 |
Eighteen years of experimental N deposition have increased the storage and slowed the cycling of C in forest floor and surface mineral soil. With the exception of the laccase copy number, all of these responses are statistically significant.
PLFA, phospholipid fatty acid analysis.