Isotopes in groundwater as indicators of climate changes

被引：26

作者：

Negrel, Philippe ^{[1
]}

Petelet-Giraud, Emmanuelle ^{[1
]}

机构：

[1] Bur Rech Geol & Minieres, Metrol Monitoring Anal Div, F-45060 Orleans 02, France

来源：

TRAC-TRENDS IN ANALYTICAL CHEMISTRY | 2011年 / 30卷 / 08期

关键词：

Aquifer; Climate change; European waters; Groundwater; Hydrogeology; Isotope; Rainwater infiltration; Recharge; Stable isotope; Water-rock interaction; BRITISH-ISLES; CHALK AQUIFER; FRESH-WATERS; GERMAN BASIN; PARIS BASIN; NOBLE-GAS; PRECIPITATION; PALAEORECHARGE; GEOCHEMISTRY; LONDON;

D O I：

10.1016/j.trac.2011.06.001

中图分类号：

O65 [分析化学];

学科分类号：

070302 ; 081704 ;

摘要：

Isotopes of the water molecule (delta O-18 and delta H-2) are a well-used tool for investigating groundwater origin and history (i.e. tracing the recharge conditions over time, processes occurring during infiltration of rainwater towards aquifers and those involved in the water-rock interaction, and mixing of different waters). This review covers several large European aquifers (Portugal, France, UK, Switzerland, Germany, Hungary, and Poland), which were investigated in terms of their recharge conditions, and the story of the groundwater at a large scale, involving recent, Holocene and Pleistocene components and their eventual mixing. (C) 2011 Elsevier Ltd. All rights reserved.

引用

页码：1279 / 1290

页数：12

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