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利用水化学相态演化图研究海水界面动力学。

Dynamic of sea water interface using hydrochemical facies evolution diagram.

机构信息

Instituto Geolóógico y Minero de España (IGME) - Geological Survey of Spain, Department of Research in Geological Resources, Ríos Rosas 23, 28003 Madrid, Spain.

出版信息

Ground Water. 2010 Mar-Apr;48(2):212-6. doi: 10.1111/j.1745-6584.2009.00649.x.

Abstract

assignment of hydrochemical facies identifies whether the aquifer is in the phase of sea water intrusion or freshening, indicating the status of the aquifer in terms of the advance or regression of the saline front. A new multi-rectangular diagram is proposed that aids interpretation of these important processes through the representation and evolution of hydrochemical facies (hydrochemical facies evolution diagram, HFE-D). As an example, the HEF-D is applied to an alluvial aquifer in the Vinaroz-Peñíscola Plain (Spain), where Ca-Cl facies characterize the sea water intrusion phase, while Na-MixHCO(3)/MixSO(4) facies characterize a freshening stage.

摘要

水化学相的分配可以确定含水层是处于海水入侵还是淡化阶段,从而表明含水层中咸水前缘的前进还是后退状况。提出了一种新的多矩形图,通过水化学相的表示和演化(水化学相演化图,HFE-D)来辅助解释这些重要过程。作为一个例子,HFE-D 被应用于比那罗斯-佩尼斯科拉平原(西班牙)的冲积含水层,其中 Ca-Cl 相特征表明处于海水入侵阶段,而 Na-MixHCO(3)/MixSO(4)相特征表明处于淡化阶段。

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