| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6335403 | Applied Geochemistry | 2012 | 7 Pages |
Abstract
⺠We present a stable isotopic method for determining the water salinisation mechanism. ⺠We show the relation between deuterium excess and the residual fraction during evaporation. ⺠The mineral dissolution and/or transpiration contributes most salinity in groundwaters in the Tarim River Basin.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Tianming Huang, Zhonghe Pang,