Abstract
This paper deals with some chemical reactions that may justify the presence of the more common gas species and their relative abundance in the geothermal fluids (i.e. H 2O, H 2S, NH 3, N 2, CO 2, CH 4). These reactions are used as geothermometers for individuating the deep temperatures in the main geothermal reservoir and applied as an example to Larderello field. Preliminary results indicate that a “mosaic model” may be used to interpret the behaviour of a geothermal system.
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