Coprecipitation of radionuclides with calcite: estimation of partition coefficients based on a review of laboratory investigations and geochemical data

Author:

Curti Enzo

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference52 articles.

1. Thorium to uranium ratios as indicators of sedimentary processes: example of concept of geological facies;Adams;Bull. Am. Assoc. Petrol. Geol.,1958

2. Baranov, V. I., Ronov, A. B., Kunashova, K. G., 1956. Geochemistry of dispersed thorium and uranium in clays and carbonate rock of the russian platform. Geochem. (3), 227-235.

3. Berner, U., 1995. KRISTALLIN I: Estimates of solubility limits for safety relevant radionuclides. PSI Report Nr. 95-07, Paul Scherrer Institute, Villigen, Switzerland. Also published as Nagra Technical Report NTB 94-08 by the National Cooperative for the Disposal of Radioactive Waste (Nagra), Wettingen, Switzerland.

4. Experimental study and modeling of the U(VI)-Fe(OH)3 surface precipitation/ coprecipitation equilibria;Bruno;Geochim. Cosmochim. Acta,1995

5. Bruno, J., Sandino, A., 1988. The thermodynamics and kinetics of coprecipitation and its effect on radionuclide solubility. Radiochim. Acta 44/45, 17–21.

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