Seasonal and annual changes in soil respiration in relation to soil temperature, water potential and trenching

Soil respiration (r(s)), soil temperature (T-s) and volumetric soil water content were measured in a balsam fir (Abies balsamea (L.) Mill.) ecosystem from 1998 to 2001. Seasonal variation in root and microbial respiration, and covariation in abiotic factors confounded interpretation of the effects of T-s and soil water potential (Psi(s)) on r(s). To minimize the confounding effect of temperature, we analyzed the effect of Psi(s) on r(s) during the summers of 1998-2000 when changes in T-s were slight. Soil respiration declined 25-50% in response to modest water stress (minimum Psi(s) of -0.6 to -0.2 MPa), and between years, there was substantial variation in the relationship between r(s) and Psi(s). In the summer of 2000, 2-m(2) plots were subjected to drought for 1 month and other plots were irrigated. The relationship between summertime r(s) and Psi(s) in the experimental plots was similar to that estimated from the survey data obtained during the same summer. In late spring and early autumn of 2001, 2-m(2) trenched and untrenched plots were subjected to drought or exposed to rainfall. It was dry in the early autumn and there was severe soil drying (Psi(s) of -10 MPa in untrenched plots and -2 MPa in trenched plots). In spring, r(s) in untrenched plots responded more to modest water stress than rs in trenched plots, indicating that root respiration is more sensitive than microbial respiration to water stress at this time of year. The response to abiotic factors differed significantly between spring and autumn in untrenched plots but not in trenched plots, indicating that root activity was greater in early autumn than in late spring, and that roots acclimated to the sustained, severe water stress experienced before and during the autumn.