T320 Fracture, Faulting, and Reactive Fluid Flow in Tight Rocks: Coupled Processes in Shale, CO2 Sequestration, and Geothermal Energy (Posters)
Wednesday, 28 September 2016
9:00 AM - 6:30 PM
Exhibit Hall E/F
VISUALIZING AND QUANTIFYING BIOMINERALIZATION IN A WELLBORE ANALOG REACTOR
Paper number: T320-4
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Robin GerlachMontana State University, Bozeman, MT
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Joe EldringMontana State University, Bozeman, MT
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Abby ThaneMontana State University, Bozeman, MT
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Randy HiebertMontana Emergent Technologies, Butte, MT
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Al CunninghamMontana State University, Bozeman, MT
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Lee SpanglerMontana State University, Bozeman, MT
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Adrienne PhillipsMontana State University, Bozeman, MT
Abstract
In the MICP process, ureolytic microorganisms hydrolyze urea into carbonate and ammonia. When this process occurs in the presence of fluids rich in calcium, the carbonate can react with calcium ions to form calcium carbonate. This calcium carbonate can then precipitate and form a seal that is capable of bridging small fluid migration pathways. To better understand the capability of MICP in the subsurface, an analog reactor modeled closely after an injection well used for MICP field demonstrations was developed to simulate the downhole geometry and flow dynamics seen in the wellbore. Defects of 0.2 mm to 1.5 mm can be created in the cement annulus and a transparent outer casing allows for visual observation of calcium carbonate formation in the annulus during experiments. Recent MICP treatments performed in this analog reactor resulted in a three order of magnitude permeability reduction of a flow channel approximately 25.4 mm in width and 0.8 mm in depth due to the creation of a calcium carbonate seal. Our results show the promise of the MICP technology to complement existing well-cement remediation technologies, sealing small defects and improving the integrity of down-hole gas storage systems.
Geological Society of America Abstracts with Programs. Vol. 48, No. 7
doi: 10.1130/abs/2016AM-278156
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