1979
DOI: 10.2343/geochemj.13.307
|View full text |Cite
|
Sign up to set email alerts
|

Direct measurements of D/H and 18O/16O fractionation factors between vapor and liquid water in the temperature range from 10 to 40.DEG.C.

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

3
26
1

Year Published

1981
1981
2018
2018

Publication Types

Select...
6
2

Relationship

1
7

Authors

Journals

citations
Cited by 58 publications
(32 citation statements)
references
References 13 publications
3
26
1
Order By: Relevance
“…It is interesting to note that analogous y values for partial molar enthalpies and partial molar volumes are also in the range 1.90 to 1.95 (FENBY and CHAND, 1978;DUTTA-CHOUDHURY and VAN HOOK, 1980). We conclude that the results of KAKIUCHI and MATSUO (1979) are in satisfactory agreement with the available vapor pressure data on D2O and with the statistical theory of isotope effects in condensed phases.…”
Section: Comparison With Experimentssupporting
confidence: 78%
See 2 more Smart Citations
“…It is interesting to note that analogous y values for partial molar enthalpies and partial molar volumes are also in the range 1.90 to 1.95 (FENBY and CHAND, 1978;DUTTA-CHOUDHURY and VAN HOOK, 1980). We conclude that the results of KAKIUCHI and MATSUO (1979) are in satisfactory agreement with the available vapor pressure data on D2O and with the statistical theory of isotope effects in condensed phases.…”
Section: Comparison With Experimentssupporting
confidence: 78%
“…For 180/160 effects the calculated difference at 32°, 6 ± 2 X 10-4 unit, is in satisfactory agreement with the observed differences between the smoothed lna measurements of KAKIUCHI and MATSUO (1979) or M AJOUBE (1971) (which are within 0.0001 unit of each other) and the JAKLI and STASCHEWSKI (1977) or SZAPIRO and STECKEL (1967) In R measurements; (lna 1nR)exptl = 4 ± 1 X 10-4 unit.…”
Section: Comparison With Experimentssupporting
confidence: 69%
See 1 more Smart Citation
“…For instance, variations of 18 O/ 16 O and D/H in water and ice cores are important indicators of present and past hydrologic processes and climate [1]. Between pure liquid water and its vapour in equilibrium, the heavier isotopes of oxygen, 18 O, and hydrogen, D, are both preferentially fractionated into the liquid phase and the lighter ones, 16 O and H, into the vapour (vapour pressure isotope effects of water) [2,3]. Even if salt is added to the liquid phase, the direction of the 18 O/ 16 O and D/H isotope fractionations does not change, but the degrees of the fractionation change depending on the kind of salt added and its concentration (isotope salt effects) [4 -7].…”
Section: Introductionmentioning
confidence: 99%
“…Between pure liquid water and its vapour in equilibrium, the heavier isotopes of oxygen, 18 O, and hydrogen, D, are both preferentially fractionated into the liquid phase and the lighter ones, 16 O and H, into the vapour (vapour pressure isotope effects of water) [1,2]. Even if salt is added to the liquid phase, the direction of the 18 O/ 16 O and D/H isotope fractionations does not change, but the degrees of the fractionation change depending on the kind of salt added and its concentration (isotope salt effects) [3 -6].…”
Section: Introductionmentioning
confidence: 99%