Oxygen isotope fractionation in divalent metal carbonates
January 1, 1969
Equilibrium fractionation factors for the distribution of 18O between alkaline‐earth carbonates and water have been measured over the temperature range 0–500°C. The fractionation factors α">αα can be represented by the equations
|
CaCO3–H2O, 1000lnα = 2.78(106T−2)− 3.39,">CaCO3–H2O, 1000lnα = 2.78(106T−2)− 3.39,CaCO3–H2O, 1000lnα = 2.78(106T−2)− 3.39,
|
|
SrCO3–H2O, 1000lnα = 2.69(106T−2)− 3.74,">SrCO3–H2O, 1000lnα = 2.69(106T−2)− 3.74,SrCO3–H2O, 1000lnα = 2.69(106T−2)− 3.74,
|
|
BaCO3–H2O, 1000lnα = 2.57(106T−2)− 4.73.">BaCO3–H2O, 1000lnα = 2.57(106T−2)− 4.73.BaCO3–H2O, 1000lnα = 2.57(106T−2)− 4.73.
|
Measurements on MnCO3, CdCO3, and PbCO3 were made at isolated temperatures. A statistical‐mechanical calculation of the isotopic partition function ratios gives reasonably good agreement with experiment. Both cationic size and mass are important in isotopic fractionation, the former predominantly in its effect on the internal vibrations of the anion, the latter in its effect on the lattice vibrations.
Citation Information
| Publication Year | 1969 |
|---|---|
| Title | Oxygen isotope fractionation in divalent metal carbonates |
| DOI | 10.1063/1.1671982 |
| Authors | J. R. O'Neil, R.N. Clayton, T.K. Mayeda |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Journal of Chemical Physics |
| Index ID | 70011501 |
| Record Source | USGS Publications Warehouse |