Depressurization-Induced Fines Migration in Sediments Containing Methane Hydrate: X-Ray Computed Tomography Imaging Experiments

Han, Gyeol; Kwon, Tae-Hyuk; Lee, Joo Yong; Kneafsey, Timothy J.

doi:10.1002/2017JB014988

Title: Depressurization-Induced Fines Migration in Sediments Containing Methane Hydrate: X-Ray Computed Tomography Imaging Experiments

Journal Article · Sat Mar 24 00:00:00 EDT 2018 · Journal of Geophysical Research. Solid Earth

DOI:https://doi.org/10.1002/2017JB014988· OSTI ID:1477278

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Korea Advanced Institute of Science and Technology (KAIST), Daejeon (South Korea). Department of Civil and Environmental Engineering
Korea Institute of Geoscience and Mineral Resources (KIGAM), Daejeon (South Korea). Oil and Gas Research Center
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Hydrocarbon Resources Program Head

Depressurization of hydrate-bearing sediments (HBS) can cause the movement of fine particles, and in turn, such fines migration affects fluid flow and mechanical behavior of sediments, ultimately affecting long-term hydrocarbon production and wellbore stability. In this work, we investigate how and to what extent depressurization of HBS causes fines migration using X-ray computed tomography (CT) imaging. Methane hydrate was synthesized in sediments with 10% fines content (FC), composed of sands with silt and/or clay, and the hydrate-bearing samples were stepwisely depressurized while acquiring CT images. The CT images were analyzed to quantify the spatial changes in FC in the host sediment and thus to capture the fines migration during depressurization. It was found that the FC changes began occurring from the hydrate dissociation regions. This confirms that the multiphase flow caused by depressurization accompanies fines migration. Depressurization of HBS with a hydrate saturation of ~20–40% caused FC reduction from ~10% to ~6–9%, and the extent of fines migration differed with the particle sizes of the host sands and the types of fines. It was found that fines migration was more pronounced with coarse sands and with silty fines. Such observed level of FC reduction is estimated to increase sediment permeability by several factors based on the Kozeny-type permeability model. In conclusion, our results support the notion that the extent of fines migration and its effect on fluid flow behavior need to be assessed in consideration of physical properties of host sediment and fine particles to identify optimum depressurization strategies.

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Research Organization:: Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

Grant/Contract Number:: AC02-05CH11231

OSTI ID:: 1477278

Journal Information:: Journal of Geophysical Research. Solid Earth, Vol. 123, Issue 4; ISSN 2169-9313

Publisher:: American Geophysical UnionCopyright Statement

Country of Publication:: United States

Language:: English

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Cited by: 39 works

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