“…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.…”