Direct measurements of D/H and 18O/l6O fractionation factors between vapor and liquid water in the temperature range from 10 to 40°C

53Citations
Citations of this article
21Readers
Mendeley users who have this article in their library.

Abstract

Vapor phase was separately collected without liquid condensate by raising the temperature of the container of vapor phase by 7°C higher than that of the interface of vapor-liquid equilibrium. D/H and 18O/16O measurements were done for the identical aliquot of vapor samples in equilibrium with the liquid water in the temperature range from 10 to 40°C. The empirical relationships between α D, α18O and the temperature of equilibration were obtained to be, 103lnα D = 2.408 × 106T-2 + 6.455 × 104T-1 - 168.7, 103lnα 18O = 5.9702 × 106T-2 - 3.2801 × 104T-1 + 52.227. © 1979, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved.

Cite

CITATION STYLE

APA

Kakiuchi, M., & Matsuo, S. (1979). Direct measurements of D/H and 18O/l6O fractionation factors between vapor and liquid water in the temperature range from 10 to 40°C. Geochemical Journal, 13(6), 307–311. https://doi.org/10.2343/geochemj.13.307

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free