87Sr/86Sr in Saxon mineral and spa waters

被引：0
|
作者：
Trettin, R
Von Storch, K
Haase, G
Gerstenberger, H
机构：
[1] UFZ Helmholtz Ctr Environm Res, Sekt Hydrogeol, D-06120 Halle, Germany
[2] GeoForsch Zentrum Potsdam, Potsdam, Germany
来源：
ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES | 1999年 / 35卷 / 03期
关键词：
groundwater; hydrochemistry; mineral water; natural variations; strontium isotope ratio; strontium; 87; 87/strontium; 86; water/rock interaction;
D O I：
10.1080/10256019908234095
中图分类号：
O61 [无机化学];
学科分类号：
070301 ; 081704 ;
摘要：
Understanding and preserving the genesis of natural mineral and spa waters is a matter of keen interest. Under a complex analysis programme, Sr-87/Sr-86 ratios (as well as other isotopes) were measured in such waters at various sites in Saxony, producing values ranging between 0.708 and 0.731. The strontium isotope ratio was found to be closely linked to the flow patterns and variations in the chemical composition of water. The Sr-87/Sr-86 ratio can thus be used as an indicator to characterize groundwater-rock interaction and hence the variation of flow paths. It is especially useful for differentiating waters in a lithologically heterogeneous aquifer system. However, it haste be applied together with other methods and different samples from the same area should be compared.
引用
收藏
页码：221 / 235
页数：15
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