Control on (U-234/U-238) in lake water:A study in the Dry Valleys of Antarctica

The (U-234/U-238) ratio in surface waters is generally higher than secular equilibrium due to nuclide recoil during alpha-decay of U-238. The size of the deviation from secular equilibrium contains information about the environment in which the water is found. This potential tool for environmental r...

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Bibliographic Details
Published in:Chemical Geology
Main Authors: Henderson, G M, Hall, B L, Smith, A, Robinson, L F
Format: Article in Journal/Newspaper
Language:English
Published: 2006
Subjects:
Online Access:https://hdl.handle.net/1983/181e6b9a-c636-4a4f-9c27-d95554b79ff9
https://research-information.bris.ac.uk/en/publications/181e6b9a-c636-4a4f-9c27-d95554b79ff9
https://doi.org/10.1016/j.chemgeo.2005.09.026