Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH

A comparative study of the reservoir fluid characteristics calculation of ten production wells of Los Azufres, Los Humeros and Cerro Prieto geothermal fields using two computer codes GeoChem (GeoSys.Chem) and WATCH is presented. GeoSys.Chem estimates the reservoir temperature and vapor fraction through quartz geothermometry and assuming enthalpy conservation, while the average temperature of quartz and Na/K geothermometers is employed in WATCH and vapor fraction is also calculated through enthalpy conservation. Both programs use the conservation of alkalinity (i.e., proton balance) for pH calculations. The difference in temperature (pressure) causes considerable effects on the calculated geothermal reservoirfluid characteristics of high enthalpy wells and negative (or near to zero) vapor fraction for low enthalpy wells. The calculated high concentration of CO2 in the secondary vapor discharged in the atmosphere at the weir box (up to 11,719 mmole/kg) suggests that the analysis of carbonic species in the geothermal waters is crucial. In the absence ofgood quality analysis of carbonic species it is suggested to consider the CO2 in the vapor sample at the separator and the total dissolved carbonic species concentration in the water sample (i.e., without considering the liberation of CO2 in the atmospheric vapor at the weir box) for the calculation of geothermal reservoir fluid composition.

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Main Authors: Torres-Alvarado,Ignacio Salvador, Verma,Mahendra P., Opondo,Kizito, Nieva,David, Haklidir,Füsun Tut, Santoyo,Edgar, Barragán,Rosa María, Arellano,Víctor
Format: Digital revista
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geología 2012
Online Access:http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S1026-87742012000300014
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spelling oai:scielo:S1026-877420120003000142013-05-23Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCHTorres-Alvarado,Ignacio SalvadorVerma,Mahendra P.Opondo,KizitoNieva,DavidHaklidir,Füsun TutSantoyo,EdgarBarragán,Rosa MaríaArellano,Víctor GeoSys.Chem GeoChem WATCH geochemical modeling geothermal system A comparative study of the reservoir fluid characteristics calculation of ten production wells of Los Azufres, Los Humeros and Cerro Prieto geothermal fields using two computer codes GeoChem (GeoSys.Chem) and WATCH is presented. GeoSys.Chem estimates the reservoir temperature and vapor fraction through quartz geothermometry and assuming enthalpy conservation, while the average temperature of quartz and Na/K geothermometers is employed in WATCH and vapor fraction is also calculated through enthalpy conservation. Both programs use the conservation of alkalinity (i.e., proton balance) for pH calculations. The difference in temperature (pressure) causes considerable effects on the calculated geothermal reservoirfluid characteristics of high enthalpy wells and negative (or near to zero) vapor fraction for low enthalpy wells. The calculated high concentration of CO2 in the secondary vapor discharged in the atmosphere at the weir box (up to 11,719 mmole/kg) suggests that the analysis of carbonic species in the geothermal waters is crucial. In the absence ofgood quality analysis of carbonic species it is suggested to consider the CO2 in the vapor sample at the separator and the total dissolved carbonic species concentration in the water sample (i.e., without considering the liberation of CO2 in the atmospheric vapor at the weir box) for the calculation of geothermal reservoir fluid composition.info:eu-repo/semantics/openAccessUniversidad Nacional Autónoma de México, Instituto de GeologíaRevista mexicana de ciencias geológicas v.29 n.3 20122012-12-01info:eu-repo/semantics/articletext/htmlhttp://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S1026-87742012000300014en
institution SCIELO
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country México
countrycode MX
component Revista
access En linea
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region America del Norte
libraryname SciELO
language English
format Digital
author Torres-Alvarado,Ignacio Salvador
Verma,Mahendra P.
Opondo,Kizito
Nieva,David
Haklidir,Füsun Tut
Santoyo,Edgar
Barragán,Rosa María
Arellano,Víctor
spellingShingle Torres-Alvarado,Ignacio Salvador
Verma,Mahendra P.
Opondo,Kizito
Nieva,David
Haklidir,Füsun Tut
Santoyo,Edgar
Barragán,Rosa María
Arellano,Víctor
Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH
author_facet Torres-Alvarado,Ignacio Salvador
Verma,Mahendra P.
Opondo,Kizito
Nieva,David
Haklidir,Füsun Tut
Santoyo,Edgar
Barragán,Rosa María
Arellano,Víctor
author_sort Torres-Alvarado,Ignacio Salvador
title Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH
title_short Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH
title_full Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH
title_fullStr Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH
title_full_unstemmed Estimates of geothermal reservoir fluid characteristics: GeoSys.Chem and WATCH
title_sort estimates of geothermal reservoir fluid characteristics: geosys.chem and watch
description A comparative study of the reservoir fluid characteristics calculation of ten production wells of Los Azufres, Los Humeros and Cerro Prieto geothermal fields using two computer codes GeoChem (GeoSys.Chem) and WATCH is presented. GeoSys.Chem estimates the reservoir temperature and vapor fraction through quartz geothermometry and assuming enthalpy conservation, while the average temperature of quartz and Na/K geothermometers is employed in WATCH and vapor fraction is also calculated through enthalpy conservation. Both programs use the conservation of alkalinity (i.e., proton balance) for pH calculations. The difference in temperature (pressure) causes considerable effects on the calculated geothermal reservoirfluid characteristics of high enthalpy wells and negative (or near to zero) vapor fraction for low enthalpy wells. The calculated high concentration of CO2 in the secondary vapor discharged in the atmosphere at the weir box (up to 11,719 mmole/kg) suggests that the analysis of carbonic species in the geothermal waters is crucial. In the absence ofgood quality analysis of carbonic species it is suggested to consider the CO2 in the vapor sample at the separator and the total dissolved carbonic species concentration in the water sample (i.e., without considering the liberation of CO2 in the atmospheric vapor at the weir box) for the calculation of geothermal reservoir fluid composition.
publisher Universidad Nacional Autónoma de México, Instituto de Geología
publishDate 2012
url http://www.scielo.org.mx/scielo.php?script=sci_arttext&pid=S1026-87742012000300014
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