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On Fluid and Heat Transfer in Deep Zones of Vapor-Dominated Geothermal Reservoirs

Conference ·
OSTI ID:888506
We have presented a preliminary analysis of permeability structure and fluid and heat flow conditions in the deeper horizons of the Larderello geothermal system. Our main observations and findings are: (1) Measurements in deep Larderello wells have indicated formation temperatures near 300 º C at 3000 m depth, and even higher temperatures at greater depth. (2) From an analysis of heat transfer mechanisms we suggest that a transition from vapor-dominated to liquid-dominated conditions must have been present in the natural state of the Larderello geothermal system. No reliable determination of the depth at which this transition occurred has yet been made, but a depth of approximately 2000 m or more appears most likely. (3) From temperature-depth data in two-phase reservoirs it is in principle possible to estimate vertical permeability. (4) For exploited reservoirs such as Larderello, reconstruction of permeability and temperature trends with depth can be made indirectly, using numerical simulation. Our preliminary results indicate that production of high-enthalpy fluids can be explained from two-phase flow effects in a fractured-porous medium. 18 refs., 2 tabs., 7 figs.
Research Organization:
Earth Sciences Division, Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA; Istituto Internazionale per le Ricerche Geotermiche, Pisa, Italy; ENEL, Unita Nazionale Geotermica, Pisa Italy
Sponsoring Organization:
USDOE
DOE Contract Number:
AT03-80SF11459; AS07-84ID12529
OSTI ID:
888506
Report Number(s):
SGP-TR-109-13
Country of Publication:
United States
Language:
English

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