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Determination of the natural circulation speeds in the well drill hole at Chassole

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Abstract

Aquifer natural flow speeds in Chassolle well drill hole (France) are studied: determination of the order of magnitude of the underground circulation in porous areas in order to state precisely the regional hydrodynamical model; evaluation of the vertical circulations which are developed in the well caused by natural convection due to variations of fluid density with temperature and to hydraulic load heterogeneities between different permeability zones.
Authors:
Publication Date:
Dec 31, 1989
Product Type:
Technical Report
Report Number:
AFME-87-07-0007
Reference Number:
SCA: 150200; PA: FRC-92:000396; SN: 92000678235
Resource Relation:
Other Information: PBD: 1989
Subject:
15 GEOTHERMAL ENERGY; AQUIFERS; FLUID FLOW; GEOTHERMAL WELLS; HYDROTHERMAL SYSTEMS; NATURAL CONVECTION; HYDRAULICS; 150200; GEOLOGY AND HYDROLOGY OF GEOTHERMAL SYSTEMS
OSTI ID:
10125408
Research Organizations:
Agence Francaise pour la Maitrise de l`Energie, 75 - Paris (France)
Country of Origin:
France
Language:
French
Other Identifying Numbers:
Other: ON: DE92779999; TRN: FR9200396
Availability:
OSTI; NTIS (US Sales Only)
Submitting Site:
FR
Size:
20 p.
Announcement Date:
Jul 04, 2005

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Citation Formats

Sauvagnac, S, and Ledoux, E. Determination of the natural circulation speeds in the well drill hole at Chassole. France: N. p., 1989. Web.
Sauvagnac, S, & Ledoux, E. Determination of the natural circulation speeds in the well drill hole at Chassole. France.
Sauvagnac, S, and Ledoux, E. 1989. "Determination of the natural circulation speeds in the well drill hole at Chassole." France.
@misc{etde_10125408,
title = {Determination of the natural circulation speeds in the well drill hole at Chassole}
 author = {Sauvagnac, S, and Ledoux, E}
 abstractNote = {Aquifer natural flow speeds in Chassolle well drill hole (France) are studied: determination of the order of magnitude of the underground circulation in porous areas in order to state precisely the regional hydrodynamical model; evaluation of the vertical circulations which are developed in the well caused by natural convection due to variations of fluid density with temperature and to hydraulic load heterogeneities between different permeability zones.}
 place = {France}
 year = {1989}
 month = {Dec}
 }