Abstract
An attempt is made to study the localization of radioelements in different mineral phases of pelagic clay sediments. The results so far obtained indicate that the ionium supported radium is redistributed by diffusion through the interstitial solution and that the authigenic zeolite phillipsite plays an important role as a scavenger of radioelements within the deposit. The mechanism of transfer of radioelements from the ocean to pelagic deposits is discussed, and points of uncertainty in the interpretation of the distribution of gross beta-activity are indicated.
DOI: https://doi.org/10.3402/tellusa.v7i2.8785 | Journal eISSN: 3035-9554
Language: English
Page range: 226 - 231
Published on: Jan 1, 1955
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1955 Gustaf Arrhenius, Edward D. Goldberg, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.