The Frasch sulfur process works best on either salt domes or bedded evaporite deposits, where sulfur is found in
permeable rock layers trapped in between impermeable layers. Bacterial alteration of
anhydrite or
gypsum, in the presence of hydrocarbons, produces limestone and
hydrogen sulfide in the
sulfur cycle. The hydrogen sulfide then oxidizes into sulfur, from percolating water, or through the action of anaerobic, sulfur-reducing bacteria In the Frasch process, three concentric tubes are introduced into the sulfur deposit.
Superheated water (165 °C, 2.5-3 MPa) is injected into the deposit via the outermost tube. Sulfur (m.p. 115 °C) melts and flows into the middle tube. Water pressure alone is unable to force the sulfur into the surface due to the molten sulfur's greater density, so hot air is introduced via the innermost tube to froth the sulfur, making it less dense, and pushing it to the surface. The Frasch process can be used for deposits 50–800 meters deep. 3-38 cubic meters of superheated water are required to produce every tonne of sulfur, and the associated energy cost is significant. ==Economic impact==