Peter M. Kroopnick scite author profile

Atmospheric oxygen has been found to be enriched in oxygen-18 by 23.5 +/- 0.3 per mil relative to average ocean water (SMOW). Oxygen dissolved in seawater is further enriched in oxygen-18 by 0.85 per mil at 0 degrees C. The temperature dependence of the solubility enrichment is given by epsilon (per mil) = 0.85- 0.010 t ( degrees C). This result is in good agreement with earlier measurements of the solubility effect in distilled water.

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Primary productivity and particle fluxes on a transect of the equator at 153°W in the Pacific Ocean

Betzer

Showers

Laws

et al. 1984

Deep Sea Research Part A. Oceanographic Research Papers

397

133

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The distribution of13C in the Atlantic Ocean

Kroopnick

1980

Earth and Planetary Science Letters

232

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Oxygen isotope fractionation in dissolved oxygen in the deep sea

Kroopnick

Craig

1976

Earth and Planetary Science Letters

101

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