Influence of hydrodynamics on saline intrusion in coastal karstic aquifers.

被引:20
作者
Arfib, Bruno
Cavalera, Thomas
Gilli, Eric
机构
[1] Univ Aix Marseille 1, Lab Chim & Environm, Geol Lab, F-13331 Marseille 3, France
[2] Soc Eaux Marseille, F-13254 Marseille, France
[3] Univ Paris 08, Dept Geog, F-93526 St Denis, France
[4] UMR Espace 6012, F-06204 Nice, France
关键词
karst; saline intrusion; spring; salinity; hysteresis; almyros; Port-Miou; France;
D O I
10.1016/j.crte.2006.07.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
A new method of interpretation of the Q-C hysteresis (discharge-salinity) during high water is proposed using the data recorded on coastal brackish karstic springs with salinity inversely proportional to the discharge. The method, based on the Q(mer)-CT (seawater discharge-salinity) hysteresis, identifies the effect of the hydrodynamic changes on the flow and transport. Three phenomena are characterized: the emptying of the karstic conduit, the dilution by freshwater and the control of the seawater intrusion in the conduit by the hydraulic head variations.
引用
收藏
页码:757 / 767
页数:11
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