Answers are grounded in this paper and cite their sources.
Economic development of shale gas resources requires successful hydraulic fracture stimulation of the gas-bearing shale utilizing significant volumes of water. The availability, treatment and disposal of this water are significant non-technical risks and can be important factors impacting the viability of shale gas opportunities. A typical Haynesville hydraulic fracturing job requires ~11,000 barrels of water and a total of ~350,000 lbs of proppant. The water initially injected into the subsurface is fresh, typically with a TDS content of 1 to 5 kppm (TDS = Total Dissolved Solids). However, clean up and recovery of the fracture fluids prior to bringing gas on stream typically recovers only ~5 to 10% of the originally injected volume of water. This water tends to be highly saline, often with TDS contents of ~200 kppm. Similar observations have been reported from other shale gas plays such as the Barnett and Marcellus. This begs the obvious question “Where did all the water go?”.
No takes yet. Share an insight, caveat, or question.
L. Taras Bryndzia (2012) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: