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
Similar Records
Hydrothermal metamorphism in the Larderello Geothermal Field
CORRELATIONS BETWEEN VAPOR SATURATION, FLUID COMPOSITION, AND WELL DECLINE IN LARDERELLO
Formation of authigenic minerals and their use as indicators of the physicochemical parameters of the fluid in the Larderello-Travale geothermal field
Journal Article
·
Tue Jan 01 00:00:00 EST 1980
· Geothermics; (United States)
·
OSTI ID:887214
CORRELATIONS BETWEEN VAPOR SATURATION, FLUID COMPOSITION, AND WELL DECLINE IN LARDERELLO
Conference
·
Tue Jan 22 00:00:00 EST 1985
·
OSTI ID:887214
Formation of authigenic minerals and their use as indicators of the physicochemical parameters of the fluid in the Larderello-Travale geothermal field
Journal Article
·
Sun Aug 01 00:00:00 EDT 1982
· Econ. Geol.; (United States)
·
OSTI ID:887214