TRACING GROUNDWATER WITH CHLORIDE IONS AND TRITIUM THROUGH ACID KAOLINITIC SOIL

被引：5

作者：

COREY, JC

FENIMORE, JW

机构：

[1] Savannah River Laboratory, E. I. du Pont de Nemours and Co., Aiken

来源：

INTERNATIONAL JOURNAL OF APPLIED RADIATION AND ISOTOPES | 1968年 / 19卷 / 10期

关键词：

D O I：

10.1016/0020-708X(68)90111-7

中图分类号：

TL [原子能技术]; O571 [原子核物理学];

学科分类号：

0827 ; 082701 ;

摘要：

Chloride ions and tritium were compared as groundwater tracers for acid soils containing kaolinitic clays in laboratory and field tests. The breakthrough for chloride was retarded more than that for tritium, which indicated that chloride ions interacted with the acid soils. Thus chloride and other negatively charged ions have limited usefulness as water tracers in acid soils. © 1968.

引用

页码：741 / +

页数：1

共 13 条

[1]

BERG WILLIAM A., 1959, SOIL SCI SOC AMER PROC, V23, P348

[2]

BIGGAR J. W., 1962, SOIL SCI SOC AMER PROC, V26, P125

[3]

CHANG MONICA L., 1963, SOIL SCI SOC AMER PROC, V27, P281

[4]

COREY JOHN C., 1963, SOIL SCI SOC AMER PROC, V27, P258