Geothermal fluids have a different composition and gas content depending on the geological formation of the reservoir, geographical location, fluid temperature and depth. The most common compounds present in the gases of geothermal fluids are CO2, H2S, H2, Ar, NH3, N2 and CH4. Degassing from geothermal plants occurs when a fraction of these gasses can not be reinjected into the reservoir and, therefore, is emitted in the air. The largest fraction of emissions is mainly associated with utilization (if a proper treatment system, like AMIS plant in Italy is not equipped), or maintenance operations phases and partially with the well testing/drilling. However, some low temperature geothermal systems – especially in sedimentary basins where natural gas reservoirs and the geothermal aquifers may be in hydraulic connections - can also produce thermal water with significant gas content. Therefore, degassing and its consequences are not restricted to plant emissions, but are general effects of geothermal operations. Ref Geoenvi D2,1
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