Cited by 45Geological and Geochemical AnalysisGroundwater and Isotope GeochemistryGeochemistry and Elemental Analysis

The DOI matches its Crossref record; 2 of the 2 references it cites were found in a registry or an index.

Oxygen Isotope Fractionation in the System Calcium Carbonate-Water

Clayton, Robert N.·1959·The Journal of Chemical Physics

Abstract

The oxygen isotope exchange reaction between water and calcium carbonate has been studied over the temperature range 190°C to 750°C. Equilibrium constants for the reaction have been measured and fit the equation: lnK=2725T−2for all temperatures above 0°C. The implications to geological thermometry are discussed.

Overview

Integrity signals

Registry

Crossref · 10.1063/1.1730165

Cites

2 of 2 references verified0 citation errors · 0 not checkable

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  • Experimental studies on equilibrium fractionation in the CaCO3-H2O system indicate that dissolution-reprecipitation controls the rate of isotope exchange between finely dispersed calcium carbonate and aqueous solutions.

    “Experimental studies on equilibrium fractionation in the CaCO₃-H2O system indicate that dissolution-reprecipitation controls the rate of isotope exchange between finely dispersed calcium carbonate and aqueous solutions (Clayton, 1959; Northrop and Clayton, 1966; O'Neil et al., 1969).”

    From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Clayton, 1959

  • Clayton (1959) observed that the calcium carbonate in the high temperature experiments underwent recrystallization during polymorphic transition from aragonite to calcite and hence achieved new calcite-water isotope equilibrium under the hydrothermal conditions.

    “Clayton (1959) observed that the calcium carbonate in the high temperature experiments underwent recrystallization during polymorphic transition from aragonite to calcite and hence achieved new calcite-water isotope equilibrium under the hydrothermal conditions.”

    From Oxygen isotope fractionation in carbonate and sulfate minerals. (1999) · cites this paper as Clayton (1959)

Citations

Cites

Flagged first, then by citations

Research works printed but not linked: 8

  1. 1950, Rev. Sci. Instr., 21, 724, 10.1063/1.1745698 · DOI
  2. 1958, J. Geol., 66, 352
  3. 1950, J. Chem. Phys., 18, 849, 10.1063/1.1747785 · DOI · Paper page
  4. 1953, Geochim. et Cosmochim. Acta, 4, 213, 10.1016/0016-7037(53)90051-9 · DOI
  5. 1949, Bull. Geol. Soc. Am., 60, 1727
  6. 1947, Rev. Sci. Instr., 18, 389, 10.1063/1.1740959 · DOI
  7. 1957, Geochim. et Cosmochim. Acta, 12, 133, 10.1016/0016-7037(57)90024-8 · DOI · Paper page
  8. 1947, J. Chem. Phys., 15, 261, 10.1063/1.1746492 · DOI · Paper page

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Metadata

Authors
Clayton, R. N.
Affiliations
Pennsylvania State University (US)
Corresponding author
Clayton, Robert N.
Venue
The Journal of Chemical Physics
Published
1959-05-01
Volume
30
Issue
5
Pages
1246-1250
ISSN
  • 0021-9606 (ISSN-L)
  • 1089-7690
OpenAlex
W2007205102
Cited by
45
References
2
Citations by year
2026: 1 · 2024: 1 · 2021: 2 · 2020: 1 · 2018: 1 · 2015: 2 · 2013: 2
FWCI
1.95
Type
journal article
Language
en
Open access
closed
Locations
The Journal of Chemical Physics (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
Keywords
oxygen isotope fractionation, calcium carbonate, water, isotope exchange, equilibrium constants, temperature dependence

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