Fault damage zone volume and initial salinity distribution determine intensity of shallow aquifer salinisation in subsurface storage

Injection of fluids into deep saline aquifers causes a pore pressure increase in the storage formation, and thus displacement of resident brine. Via hydraulically conductive faults, brine may migrate upwards into shallower aquifers and lead to unwanted salinisation of potable groundwater resources....

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Bibliographic Details
Main Authors: E. Tillner, M. Langer, T. Kempka, M. Kühn
Format: Article
Language:English
Published: Copernicus Publications 2016-03-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/20/1049/2016/hess-20-1049-2016.pdf