THE INFLUENCE OF HEMATITE ON THE SORPTION OF URANIUM(VI) ONTO GRANITE FILLING FRACTURES

被引：25

作者：

CASAS, I

CASABONA, D

DURO, L

DEPABLO, J

机构：

[1] Chemical Engineering Department, Universitat Politècnica de Catalunya, 08028 Barcelona

来源：

CHEMICAL GEOLOGY | 1994年 / 113卷 / 3-4期

关键词：

D O I：

10.1016/0009-2541(94)90073-6

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Continuous flow-through column experiments have been performed to determine the sorption of uranium in granite-hematite mixtures. The results obtained have shown the importance that oxy-hydroxy iron compounds present as fracture fillings can have in the uranium retardation in its migration through the geosphere. The experimental results showed the reversibility of the sorption process and have been successfully fitted with a model combining both thermodynamic and kinetic terms.

引用

页码：319 / 326

页数：8

共 15 条

[1]

BRUNO J, 1991, SKB9020 TECH REP

[2] CONVECTIVE-DISPERSIVE SOLUTE TRANSPORT WITH A COMBINED EQUILIBRIUM AND KINETIC ADSORPTION MODEL [J].