Unintentional aquifer inter-connection (originally separated by impermeable layers) via the wellbore or disturbance of non-targeted aquifers with fluid intrusion (geothermal fluid, testing fluid, drilling mud, etc.) is a risk that can appear when drilling wells. The consequences of this phenomenon may include potential aquifer and freshwater resource contamination and depletion, loss in geothermal potential, affect other underground uses, ground elevation at surface from formation swelling, collapse or landslides from formation dissolutions. The phenomena are driven by differential pressures between layered aquifers and can be caused by well barrier and integrity failures due to poor cementation practices, mechanical damage during well development, corrosion and scaling, geo-mechanical disturbances, thermal stress and material failure or degradation, and aging over the life cycle of operations. It can be triggered during the drilling process and through all life stages of a geothermal project. It can also result from improper reinjection applications. Ref: Geoenvi D2,1
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