Continuous and simultaneous measurement of triple-oxygen and hydrogen isotopes of liquid and vapor during evaporation experiments.

Abstract

RATIONALE\nOxygen and hydrogen isotopes are important tools for studying modern and past hydrological cycle. Previous evaporation experiments use episodic measurement of liquid and/or vapor or have not measured all isotopologues of water. Here, we describe an evaporation experimental system that allows all isotopologues of liquid and water vapor to be measured simultaneously and near-continuously at high-precision using cavity ring-down laser spectroscopy (CRDS).\n\n\nMETHODS\nEvaporating liquid is periodically sampled from a closed recirculating loop by a syringe pump that delivers a constant supply of water to the vaporizer, achieving a water vapor concentration of 20,000 ppmV H2 O (±132, 1σ). Vapor is sampled directly from the evaporation chamber. Isotope ratios are measured simultaneously with a Picarro L2140-I CEDS instrument.\n\n\nRESULTS\nFor liquid measurements, Allan variance analysis indicates an optimum data collection window of 34 minutes for oxygen isotopes and 27 minutes for hydrogen isotopes. During these periods, the mean standard error is ±0.0081 ‰ for δ17 O values, ±0.0081 ‰ for δ18 O values, and ±0.019 ‰ for δ2 H values. For the derived parameters 17 O-excess and d-excess, the standard error of the mean is 5.8 per meg and 0.07 ‰, respectively. For the vapor phase a 12.5-minute data window for all isotopologues results in a mean standard error of ±0.012 ‰ for δ17 O values, ±0.011 ‰ for δ18 O values, and ±0.023 ‰ for δ2 H values. For the derived parameters, the standard error of the mean is 9.2 per meg for 17 O-excess and 0.099 ‰ for d-excess. These measurements result in consistently narrow 95% confidence limits for the slopes of ln(δ17 O+1) vs ln(δ18 O+1) and ln(δ2 H +1) vs ln(δ18 O+1).\n\n\nCONCLUSIONS\nThe experimental method permits measurement of fractionation of triple-oxygen and hydrogen isotopes of evaporating water under varying controlled conditions at high precision. Application of this method will be useful for testing theoretical models of evaporation and conducting experiments to simulate evaporation and isotopic equilibration in natural systems.