1966
DOI: 10.1080/00028896609342838
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Toxicity Studies on 1,1,2,2-Tetrachloro-1,2-Difluoroethane and 1,1,1,2-Tetrachloro-2,2-Difluoroethane

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Cited by 14 publications
(2 citation statements)
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“…Common isotopic processes that affect the relationship between δD and δ 18 O are evaporation from open water and exchange with rock minerals (Fontes, 1980). δD is generally unaffected by reaction with aquifer (Clayton et al, 1966). Whenever the interaction between rock and water leads to the alteration of feldspars to clay minerals, the latter go into isotopic equilibrium with the water leading to a shift in the δ 18 O of the water.…”
Section: Resultsmentioning
confidence: 98%
“…Common isotopic processes that affect the relationship between δD and δ 18 O are evaporation from open water and exchange with rock minerals (Fontes, 1980). δD is generally unaffected by reaction with aquifer (Clayton et al, 1966). Whenever the interaction between rock and water leads to the alteration of feldspars to clay minerals, the latter go into isotopic equilibrium with the water leading to a shift in the δ 18 O of the water.…”
Section: Resultsmentioning
confidence: 98%
“…Stable oxygen and hydrogen isotopes of formation water will help characterize the fluids in different formations. In the midcontinent basins, the isotopic composition of the bedrock fluids shows characteristic deviations from the global meteoric water line (Graf et al, 1965, Clayton et al, 1966. If fluids from deeper formations began to mix with shallower units, oxygen and hydrogen isotope 18 O could identify such mixing.…”
Section: Geochemical Parametersmentioning
confidence: 99%