Fig. 2From: Response of soil respiration to changes in soil temperature and water table level in drained and restored peatlands of the southeastern United StatesPower-transformed total soil respiration as a function of water table (a) and soil temperature (b) measured in drained and restored peatlands. Total soil respiration, depth to water table, and soil temperature were measured in drained and restored peatlands at four locations in eastern North Carolina and southeastern Virginia from 2007 to 2017. All coefficients are significant at P < 0.0001Back to article page