文摘
Integrating the isotopic fractionation processes with separate E and T for simulating dynamics (δET and δL,b). In situ measurements of isotopic water vapor with the flux-gradient approach and robust EC data were used to evaluate daily and seasonal variations of Iso-SPAC model output. The steady-state assumption is a better approximation for estimating δL,b and δT in the daytime over the growing season. Consideration of the extra resistance of bare soil from film coverage is necessary for estimating E, and 5 cm is a reasonable depth for soil water sampling for estimating δE.