Interpretation of activity ratios in groundwaters-Reference-Cited by-同舟云学术

Interpretation of activity ratios in groundwaters

Published:1985-12 Issue:1-2 Volume:58 Page:83-88
ISSN:0168-9622
Container-title:Chemical Geology: Isotope Geoscience section
language:en
Short-container-title:Chemical Geology: Isotope Geoscience section

Author:

Dickson B.L.,Davidson M.R.

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference27 articles.

1. Radionuclide migration around uranium ore bodies — analogue of radioactive waste repositories;Airey;U.S. Nucl. Reg. Comm. Contract NRC-04-81-172, 2nd Annu. Rep., AAEC (Aust. At. Energy Comm.), Rep. C40,1984

2. Sorption behaviour of long-lived radionuclides in igneous rocks;Andersson,1982

3. The evolution of enhanced 234U238U activity ratios for dissolved uranium and groundwater dating;Andrews,1978

4. 234U238U activity ratios of dissolved uranium in groundwaters from a Jurassic limestone aquifer in England;Andrews;Earth Planet. Sci. Lett.,1982

5. The U contents and 234U238U activity ratios of dissolved uranium in groundwaters from some Triassic sandstones in England;Andrews;Isot. Geosci.,1983

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2. Uranium series disequilibria in ground waters from a fractured bedrock aquifer (Morungaba Granitoids—Southern Brazil): Implications to the hydrochemical behavior of dissolved U and Ra;Applied Radiation and Isotopes;2008-10

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