Disposal and temporary surface storage of spent geothermal fluids and surface subsidence and faulting are the major environmental problems that could arise from geopressured geothermal water production. Geopressured geothermal fluids are moderately to highly saline (8,000 to 72,000 parts per million total dissolved solids) and may contain significant amounts of boron (19 to 42 parts per million). Disposal of hot saline geothermal water in subsurface saline aquifers will present the least hazard to the environment. It is not known, however, whether the disposal of as much as 54,000 m3 (310,000 barrels) of spent fluids perday into saline aquifers at the production site is technically or economically feasible. If saline aquifers adequate for fluid disposal cannot be found, geothermal fluids may have to be disposed of by open watercourses, canals, and pipelines to coastal bays on the Gulf of Mexico. Overland flow or temporary storage of geothermal fluids may cause negative environmental impacts. As the result of production of large volumes of geothermal fluid, reservoir pressuredeclines may cause compaction of sedimentswithin and adjacent to the reservoir. The amountof compaction depends on pressure decline, reservoirthickness, and reservoir compressibility. Atpresent, these parameters can only be estimated.Reservoir compaction may be translated in part tosurface subsidence. When differential compaction occurs across a subsurface fault, fault activationmay occur and be manifested as differential subsidence across the surface trace of the fault or as anactual rupture of the land surface.The magnitude of environmental impact of subsidence and fault activation varies with currentland use ; the greatest impact would occur in urban areas, whereas relatively minor impacts would occur in rural, undeveloped agricultural areas. Geothermal resource production facilities on the Gulf Coast of Texas could be subject to a series of natural hazards: (1) hurricane- or storm-induced flooding, (2) winds from tropical storms, (3) coastal erosion, or (4) expansive soils. None of these hazards is generated by geothermal resource production, but each has potential for damaging geothermal production and disposal facilities that could, in time, result in leakage of hot saline geothermal fluids.
Gustavson, T. C., and Kreitler, C. W., 1976, Geothermal Resources of the Texas Gulf Coast: Environmental Concerns Arising from the Production and Disposal of Geothermal Waters: The University of Texas at Austin, Bureau of Economic Geology, Geological Circular 76-7, 35 p. doi.org/10.23867/gc7607D.