1991
DOI: 10.1524/ract.1991.5253.2.367
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The Distribution of Natural Radionuclides on Fracture Surfaces in Palmottu Analogue Study Site in SW Finland

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Cited by 19 publications
(11 citation statements)
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“…This was not expected because the easily dissolvable phase that covered the mixture of kaolinite and quartz separated from the U containing calcite (sample 221/DH331) the 234 U/ 238 U activity ratio was 6.05. The amounts of easily dissolvable U in these samples were 2626 and 398 μg/g, respectively [15].…”
Section: Core Sample 103/r346mentioning
confidence: 91%
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“…This was not expected because the easily dissolvable phase that covered the mixture of kaolinite and quartz separated from the U containing calcite (sample 221/DH331) the 234 U/ 238 U activity ratio was 6.05. The amounts of easily dissolvable U in these samples were 2626 and 398 μg/g, respectively [15].…”
Section: Core Sample 103/r346mentioning
confidence: 91%
“…The residue left after the extractions was dissolved in a HF-HN0 3 -HC1 mixture. The extraction procedure has been described earlier [15].…”
Section: Radiochemical Analysesmentioning
confidence: 99%
“…Absolute concentrations and activity ratios for the source phase and target phase. Numbers in parentheses are laboratory codes and refer to the same samples in other publications [4,8] …”
Section: Samplesmentioning
confidence: 99%
“…Isotopie fractionation of U, resulting in U-234 enrichment takes place in natural waters, and it has been universally linked to α-recoil effects in the natural radioactive decay series [1,2], Similar enrichment has also been observed across phase boundaries in rock material [1,3,4,5], of which good experimental evidence can be found in [3]. In contrast, clear U-234 depletion was observed in a deposited U-rich phases at the natural analogue site at Palmottu [6], As compared to waters, recoil transfer within rock material has been much less discussed, and discussions have been mostly qualitative.…”
Section: Introductionmentioning
confidence: 99%
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