TY - JOUR
T1 - Preinjection reservoir fluid characterization at a CCS demonstration site
T2 - 11th International Conference on Greenhouse Gas Control Technologies, GHGT 2012
AU - Locke, Randall
AU - Larssen, David
AU - Salden, Walter
AU - Patterson, Christopher
AU - Kirksey, Jim
AU - Iranmanesh, Abbas
AU - Wimmer, Bracken
AU - Krapac, Ivan
N1 - Funding Information:
Staff of the Illinois State Geological Survey contributed to field sampling efforts (Peter Berger, Jacquelyn Hurry, Charles Monson, David Ussiri, Lo is Yoksoulian), initial data interpretations (Keith Hackley, Sam Panno), cheical analyses (Sm hari Fanta), and data am nagement (Damon Garner.) Chemical analyses were also performed by the Illinois State Water Survey – Public Service Laboratory (Dan Webb, Manager). This research was funded by the U.S. Department of Energy through the National Energy Technology Laboratory N( ETL) eR gional Carbon Sequestration Partnership Program (contract nubm er DE-FC26-05NT42588) and by a cost share agreement with the Illinois Department of Commerce and Economic Opportunity, Office of Coal Development through the Illinois Clean Coal Institute.
PY - 2013
Y1 - 2013
N2 - The Midwest Geological Sequestration Consortium is conducting the Illinois Basin - Decatur Project (IBDP), a large-scale carbon capture and storage (CCS) project in Decatur, Illinois, USA. An extensive Monitoring, Verification, and Accounting (MVA) program has been implemented, and a deep monitoring well, VW#1, was drilled to a depth of 2,201 m (7,264 ft). The well was perforated in eleven zones ranging in depth from 1,499 to 2,153 m (4917 to 7061 ft.). Fluid samples were collected during three sampling events using two different sampling methods. This paper describes the well construction, well completion, sample collection procedures, and selected preinjection sampling results from VW#1. Prior to sampling, particular care was taken to remove non-native fluids from each of the sampling zones. Density, specific conductance, bromide concentrations, and bromide-chloride ratios have been used as indicators of sample representativeness. Fluid compositional data and formation pressure data have been collected from VW#1. These high-quality, fieldbased data are essential to establish hydrochemical conditions in and above the storage reservoir prior to CO2 injection, indicate the response of the reservoir to injection, provide detailed geochemical model inputs, and provide insights for on-going work at the Illinois State Geological Survey about the origin of Illinois Basin brines. Primary brine constituents are chloride, sodium, and calcium with average total dissolved solids concentrations of 190,000 mg/L in the Mt. Simon Sandstone and 65,600 mg/L in Ironton-Galesville Formation (above the injection reservoir).
AB - The Midwest Geological Sequestration Consortium is conducting the Illinois Basin - Decatur Project (IBDP), a large-scale carbon capture and storage (CCS) project in Decatur, Illinois, USA. An extensive Monitoring, Verification, and Accounting (MVA) program has been implemented, and a deep monitoring well, VW#1, was drilled to a depth of 2,201 m (7,264 ft). The well was perforated in eleven zones ranging in depth from 1,499 to 2,153 m (4917 to 7061 ft.). Fluid samples were collected during three sampling events using two different sampling methods. This paper describes the well construction, well completion, sample collection procedures, and selected preinjection sampling results from VW#1. Prior to sampling, particular care was taken to remove non-native fluids from each of the sampling zones. Density, specific conductance, bromide concentrations, and bromide-chloride ratios have been used as indicators of sample representativeness. Fluid compositional data and formation pressure data have been collected from VW#1. These high-quality, fieldbased data are essential to establish hydrochemical conditions in and above the storage reservoir prior to CO2 injection, indicate the response of the reservoir to injection, provide detailed geochemical model inputs, and provide insights for on-going work at the Illinois State Geological Survey about the origin of Illinois Basin brines. Primary brine constituents are chloride, sodium, and calcium with average total dissolved solids concentrations of 190,000 mg/L in the Mt. Simon Sandstone and 65,600 mg/L in Ironton-Galesville Formation (above the injection reservoir).
KW - Fluid chemistry
KW - Groundwater monitoring
KW - Illinois basin - Decatur project
KW - Midwest geological sequestration consortium
KW - Sample integrity
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U2 - 10.1016/j.egypro.2013.06.572
DO - 10.1016/j.egypro.2013.06.572
M3 - Conference article
AN - SCOPUS:84898723738
SN - 1876-6102
VL - 37
SP - 6424
EP - 6433
JO - Energy Procedia
JF - Energy Procedia
Y2 - 18 November 2012 through 22 November 2012
ER -