Thermodynamics and kinetics of the isotopic equilibration of nitrogen gas (N2) in water: Implications for biological N2 fixation experiments

Better characterization of biological N2 fixation along with its controlling factors is needed for improved projections of the feedbacks between nitrogen cycling, ecosystems productivity, and climate dynamics. Building on an ongoing community effort to refine estimates of biological N2 fixation, we outline several considerations aimed at improving ¹⁵N2 incubation measurements. We first show based on a theoretical analysis that the bias associated with equilibrium isotopic fractionation is within the uncertainty of ¹⁵N2 incubation experiments, even under conditions with a large headspace to aqueous ratio, such as in soil or sediment incubations. Second, we empirically determine the effects of temperature and agitation on the equilibration kinetics. Shaking intensity seems to be a dominant control on the kinetics of equilibration. Our results show that nearly complete equilibration of dissolved ¹⁵N2 is achieved within 4 min of vigorous shaking at 20°C at atmospheric pressure, but significantly slower at lower temperatures. The equations presented in our study are adaptable to varying ¹⁵N2 incubation conditions and other trace gas isotope addition experiments.

Duke Scholars

Author Nicolas Cassar Earth and Climate Sciences