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Title: Flow rate decline and pressure transient in the Larderello geothermal field

Conference ·
OSTI ID:887214

The production history of most of the Larderello wells, both the older ones and the recent ones, that we have produced at constant pressure, is characterised by a rapid initial decline. In this study such a decline is interpreted as the consequence of an original flow regime of the “depletion” type being followed by a “diffusion” type regime. Such an interpretation, which does prove consistent with the phenomenology of the geothermal field, was suggested by the results of the analyses of the well-closure tests carried out in the North zone of Larderello and in the Travale field.

Research Organization:
ENEL - UNG, Pisa, IT
Sponsoring Organization:
USDOE
DOE Contract Number:
AS07-84ID12529
OSTI ID:
887214
Report Number(s):
SGP-TR-113-26
Resource Relation:
Conference: Proceedings, thirteenth workshop on geothermal reservoir engineering, Stanford University, Stanford, CA, January 19-21, 1988
Country of Publication:
United States
Language:
English

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