Geochemical Changes in Response to CO<sub>2</sub> Injection in a CO<sub>2</sub>-EOR Complex in Northern Michigan. Volume II.1 [electronic resource]

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Tác giả:

Ngôn ngữ: eng

Ký hiệu phân loại: 543.8 Chromatography

Thông tin xuất bản: Washington, D.C. : Oak Ridge, Tenn. : United States. Office of the Assistant Secretary of Energy for Fossil Energy ; Distributed by the Office of Scientific and Technical Information, U.S. Dept. of Energy, 2020

Mô tả vật lý: Size: 84 p. : , digital, PDF file.

Bộ sưu tập: Metadata

ID: 267887

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 The Midwest Regional Carbon Sequestration Partnership (MRCSP) was founded in 2003 as part of the U.S. Department of Energy?s (DOE?s) Regional Carbon Sequestration Partnership initiative. Since its founding, MRCSP has made significant strides toward making CCUS a viable option for states in the region. The public/private consortium, funded through the DOE Regional Carbon Sequestration Initiative, brings together nearly 40 industry partners and 10 states. Battelle, as the project lead, oversees research, development and operations and coordinates activities among the partners. The incremental, phased approach has built a valuable knowledge base for the industry and paved the way for commercial-scale adoption of CCUS technologies. From 2008 to 2020, MRCSP Phase III focused on the development of large-scale injection projects. This report is part of a series of reports prepared under the Midwestern Regional Carbon Sequestration Partnership (MRCSP) Phase III (Development Phase). These reports summarize and detail the findings of the work conducted under the Phase III project.<
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  The report describes the geochemical monitoring program under MRCSP to use stable and radiogenic isotope geochemistry in concert with analysis of general geochemical parameters of fluids and gases and analysis of core samples to determine geochemical processes occurring in the reef structure because of CO<
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  injection. Specifically, brine and gas samples were collected and analyzed to determine changes occurring between reefs prior to and following CO<
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 2<
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  injection. The analytical results for general geochemical parameters were modeled with chemical equilibrium models to determine if the injection of CO<
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 2<
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  resulted in the mineral dissolution or precipitation. Finally, core samples were collected and analyzed to determine if there was evidence of dissolution features or mineral precipitation.<
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