To understand sulfuric acid speleogenesis (SAS) it is of upmost importance to know how fast H2S is oxidised to sulfuric acid by bacteria when the upwelling water rich in H2S encounters water from the surface that contains oxygen. It is also important to know where this happens and what are the concentrations ofH2S in the upwelling waters. It is possible that bacteria exist in narrow fracture with about a few hundred µm aperture width?

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