Effect of temperature and humic acid on the U(VI) diffusion in compacted opalinus clay

0Citations
Citations of this article
3Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The diffusion of 233U(VI) in compacted Opalinus Clay from the Mont Terri test site, Switzerland was studied in the absence and presence of humic acid for two different temperatures (25, 60°C). The diffusion experiments were carried out under anaerobic conditions and a synthetic Opalinus Clay pore water (pH 7.6, I = 0.36 M) as background electrolyte was used. At 25°C as well as at 60°C humic acid has no influence on 233U(VI) diffusion. In addition, the results showed that the interaction of 233U(VI) with the clay is stronger at 60°C.

Cite

CITATION STYLE

APA

Joseph, C., Van Loon, L. R., Jakob, A., Schmeide, K., Sachs, S., & Bernhard, G. (2012). Effect of temperature and humic acid on the U(VI) diffusion in compacted opalinus clay. In Springer Geology (pp. 617–626). Springer. https://doi.org/10.1007/978-3-642-22122-4_71

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free