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Geochemical study of Dogger near the injection well. Final report

Technical Report:

Abstract

The Dogger aquifer, in the Paris area, is utilized for 10 years with doublet systems for district heating. Temperature is about 70 C. Injection of cold water is likely to lead to geochemical reactions (dissolution-precipitation). The objective of this work was to quantify those reactions in the nearly of the cold water injection well, and especially through the calco-carbon system reaction dynamics modelization. The CHIMERE and STELE mathematical models are used.
Publication Date:
Dec 31, 1990
Product Type:
Technical Report
Report Number:
AFME-89-92-0001-Pt.1
Reference Number:
SCA: 152000; 150200; PA: FRC-91:003657; SN: 92000620783
Resource Relation:
Other Information: PBD: 1990
Subject:
15 GEOTHERMAL ENERGY; AQUIFERS; GEOCHEMISTRY; MATHEMATICAL MODELS; CHEMICAL REACTIONS; DISSOLUTION; PRECIPITATION; FLUID INJECTION; 152000; 150200; GEOTHERMAL DATA AND THEORY; GEOLOGY AND HYDROLOGY OF GEOTHERMAL SYSTEMS
OSTI ID:
10117783
Research Organizations:
Agence Francaise pour la Maitrise de l`Energie, 75 - Paris (France)
Country of Origin:
France
Language:
French
Other Identifying Numbers:
Other: ON: DE92743181; TRN: FR9103657
Availability:
OSTI; NTIS (US Sales Only)
Submitting Site:
FR
Size:
75 p.
Announcement Date:
Jun 30, 2005

Technical Report:

Citation Formats

Coudrain-Ribstein, A, and Iris, P. Geochemical study of Dogger near the injection well. Final report. France: N. p., 1990. Web.
Coudrain-Ribstein, A, & Iris, P. Geochemical study of Dogger near the injection well. Final report. France.
Coudrain-Ribstein, A, and Iris, P. 1990. "Geochemical study of Dogger near the injection well. Final report." France.
@misc{etde_10117783,
title = {Geochemical study of Dogger near the injection well. Final report}
author = {Coudrain-Ribstein, A, and Iris, P}
abstractNote = {The Dogger aquifer, in the Paris area, is utilized for 10 years with doublet systems for district heating. Temperature is about 70 C. Injection of cold water is likely to lead to geochemical reactions (dissolution-precipitation). The objective of this work was to quantify those reactions in the nearly of the cold water injection well, and especially through the calco-carbon system reaction dynamics modelization. The CHIMERE and STELE mathematical models are used.}
place = {France}
year = {1990}
month = {Dec}
}