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Estimation of original reservoir fluid composition prior to aquifer boiling induced by well discharge. Kieki niso ryunyu ni okeru choryu sonai futto izen no chinetsu ryutai no kagaku soshiki no suiteiho

Abstract

A method for estimating chemical composition of original fluid before boiling from the composition of whole fluid flowing into a well is described for the case where an aquifer boiling has begun in a reservoir bed associated with discharge of geothermal fluid from the well (the enthalpy of fluid flowing into the well is larger than an enthalpy possessed by a hot fluid-phase saturated by steam at measured temperatures at flowing point). In this case, it is especially pointed out that the gas-liquid ratio at the well flow-in point becomes larger than the one at boiling. The boiling in the reservoir bed is modelled into two types. One is for larger coefficient of permeation in the reservoir bed where the discharge flow at the well is large, the temperature drop around the well is small, and the boiling is in single stage. The other is for smaller coefficient of permeation in the reservoir bed where the discharge flow and temperature drop are contrastive to the former case, and the boiling is in multi-stage. Calculation processes based on this boiling model are explained with calculation examples. 8 refs.,7 figs.
Authors:
Seki, Y [1] 
  1. Geological Survey of Japan, Tsukuba (Japan)
Publication Date:
Jul 29, 1991
Product Type:
Journal Article
Reference Number:
NEDO-91-930253; EDB-92-032723
Resource Relation:
Journal Name: Chishitsu Chosajo Geppo (Bulletin of the Geological Survey of Japan); (Japan); Journal Volume: 42:6,7
Subject:
15 GEOTHERMAL ENERGY; BOILING; MATHEMATICAL MODELS; RESERVOIR ROCK; GEOTHERMAL FLUIDS; CHEMICAL COMPOSITION; GEOTHERMAL WELLS; TWO-PHASE FLOW; ENTHALPY; PERMEABILITY; STOICHIOMETRY; FLUID FLOW; FLUIDS; PHASE TRANSFORMATIONS; PHYSICAL PROPERTIES; THERMODYNAMIC PROPERTIES; WELLS; 150904* - Geothermal Engineering- Geothermal Reservoir & Well Performance
OSTI ID:
5922112
Country of Origin:
Japan
Language:
Japanese
Other Identifying Numbers:
Journal ID: ISSN 0016-7665; CODEN: CHCGA
Submitting Site:
NEDO
Size:
Pages: 337-346
Announcement Date:
Mar 15, 1992

Citation Formats

Seki, Y. Estimation of original reservoir fluid composition prior to aquifer boiling induced by well discharge. Kieki niso ryunyu ni okeru choryu sonai futto izen no chinetsu ryutai no kagaku soshiki no suiteiho. Japan: N. p., 1991. Web.
Seki, Y. Estimation of original reservoir fluid composition prior to aquifer boiling induced by well discharge. Kieki niso ryunyu ni okeru choryu sonai futto izen no chinetsu ryutai no kagaku soshiki no suiteiho. Japan.
Seki, Y. 1991. "Estimation of original reservoir fluid composition prior to aquifer boiling induced by well discharge. Kieki niso ryunyu ni okeru choryu sonai futto izen no chinetsu ryutai no kagaku soshiki no suiteiho." Japan.
@misc{etde_5922112,
title = {Estimation of original reservoir fluid composition prior to aquifer boiling induced by well discharge. Kieki niso ryunyu ni okeru choryu sonai futto izen no chinetsu ryutai no kagaku soshiki no suiteiho}
author = {Seki, Y}
abstractNote = {A method for estimating chemical composition of original fluid before boiling from the composition of whole fluid flowing into a well is described for the case where an aquifer boiling has begun in a reservoir bed associated with discharge of geothermal fluid from the well (the enthalpy of fluid flowing into the well is larger than an enthalpy possessed by a hot fluid-phase saturated by steam at measured temperatures at flowing point). In this case, it is especially pointed out that the gas-liquid ratio at the well flow-in point becomes larger than the one at boiling. The boiling in the reservoir bed is modelled into two types. One is for larger coefficient of permeation in the reservoir bed where the discharge flow at the well is large, the temperature drop around the well is small, and the boiling is in single stage. The other is for smaller coefficient of permeation in the reservoir bed where the discharge flow and temperature drop are contrastive to the former case, and the boiling is in multi-stage. Calculation processes based on this boiling model are explained with calculation examples. 8 refs.,7 figs.}
journal = []
volume = {42:6,7}
journal type = {AC}
place = {Japan}
year = {1991}
month = {Jul}
}