The transfer of uranium isotopes 234U and 238U to the waters interacting with carbonates from Mendip Hills area (England)

Author:

Bonotto D.M,Andrews J.N

Publisher

Elsevier BV

Subject

Radiation

Reference30 articles.

1. Mechanism of radon release in rock matrices and entry into groundwaters;Andrews;Inst. Mineral. Metal. Trans. B,1972

2. 238U/238U activity ratios of dissolved uranium in groundwaters from a Jurassic Limestone aquifer in England;Andrews;Earth Planet. Sci. Lett.,1982

3. Diffusive flow and conduit flow in limestone terrain in the Mendip Hills, Somerset, Great Britain;Atkinson;J. Hydrol.,1977

4. The mechanism of 238U/238U activity ratio enhancement in karstic limestone groundwater;Bonotto;Chem. Geol. (Isot. Geosci. Sec.),1993

5. Brown, H., Silver, L.T., 1955. The possibilities of obtaining long-term supplies of uranium, thorium and other substances of uranium from igneous rocks. In: Peaceful Uses of Atomic Energy, Conference Proceedings, IAEA, Geneva, pp. 91-95.

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