Experimental Investigation of Gas Flow and Hydrate Formation Within the Hydrate Stability Zone
Abstract
Abstract We form methane hydrate by injecting methane gas into a brine‐saturated, coarse‐grained sample under hydrate‐stable thermodynamic conditions. Hydrate forms to a saturation of 11%, which is much lower than that predicted assuming three‐phase (gas‐hydrate‐brine) thermodynamic equilibrium (67%). During hydrate formation, there are temporary flow blockages. We interpret that a hydrate skin forms a physical barrier at the gas‐brine interface. The skin fails periodically when the pressure differential exceeds the skin strength. Once the skin is present, further hydrate formation is limited by the rate that methane can diffuse through the solid skin. This process produces distinct thermodynamic states on either side of the skin that allows gas to flow through the sample. This study illuminates how gas can be transported through the hydrate stability zone and thus provides a mechanism for the formation of concentrated hydrate deposits in sand reservoirs. It also illustrates that models that assume local equilibrium at the core‐scale and larger may not capture the fundamental behaviors of these gas flow and hydrate formation processes.
- Authors:
-
- The Univ. of Texas at Austin, Austin, TX (United States)
- Petroleum and Geosystems Engineering, The University of Texas at Austin, Austin TX USA
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States). Advanced Light Source (ALS)
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Fossil Energy (FE)
- OSTI Identifier:
- 1477334
- Alternate Identifier(s):
- OSTI ID: 1461561
- Grant/Contract Number:
- AC02-05CH11231; DE‐FE0010406; DE‐FE0028967; DE‐FE0023919; DE‐AC02‐05CH11231
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Volume: 123; Journal Issue: 7; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; methane hydrate formation; free gas migration; nonequilibrium; computed tomography
Citation Formats
Meyer, Dylan W., Flemings, Peter B., DiCarlo, David, You, Kehua, Phillips, Stephen C., and Kneafsey, Timothy J. Experimental Investigation of Gas Flow and Hydrate Formation Within the Hydrate Stability Zone. United States: N. p., 2018.
Web. doi:10.1029/2018JB015748.
Meyer, Dylan W., Flemings, Peter B., DiCarlo, David, You, Kehua, Phillips, Stephen C., & Kneafsey, Timothy J. Experimental Investigation of Gas Flow and Hydrate Formation Within the Hydrate Stability Zone. United States. https://doi.org/10.1029/2018JB015748
Meyer, Dylan W., Flemings, Peter B., DiCarlo, David, You, Kehua, Phillips, Stephen C., and Kneafsey, Timothy J. Sun .
"Experimental Investigation of Gas Flow and Hydrate Formation Within the Hydrate Stability Zone". United States. https://doi.org/10.1029/2018JB015748. https://www.osti.gov/servlets/purl/1477334.
@article{osti_1477334,
title = {Experimental Investigation of Gas Flow and Hydrate Formation Within the Hydrate Stability Zone},
author = {Meyer, Dylan W. and Flemings, Peter B. and DiCarlo, David and You, Kehua and Phillips, Stephen C. and Kneafsey, Timothy J.},
abstractNote = {Abstract We form methane hydrate by injecting methane gas into a brine‐saturated, coarse‐grained sample under hydrate‐stable thermodynamic conditions. Hydrate forms to a saturation of 11%, which is much lower than that predicted assuming three‐phase (gas‐hydrate‐brine) thermodynamic equilibrium (67%). During hydrate formation, there are temporary flow blockages. We interpret that a hydrate skin forms a physical barrier at the gas‐brine interface. The skin fails periodically when the pressure differential exceeds the skin strength. Once the skin is present, further hydrate formation is limited by the rate that methane can diffuse through the solid skin. This process produces distinct thermodynamic states on either side of the skin that allows gas to flow through the sample. This study illuminates how gas can be transported through the hydrate stability zone and thus provides a mechanism for the formation of concentrated hydrate deposits in sand reservoirs. It also illustrates that models that assume local equilibrium at the core‐scale and larger may not capture the fundamental behaviors of these gas flow and hydrate formation processes.},
doi = {10.1029/2018JB015748},
journal = {Journal of Geophysical Research. Solid Earth},
number = 7,
volume = 123,
place = {United States},
year = {Sun Jul 01 00:00:00 EDT 2018},
month = {Sun Jul 01 00:00:00 EDT 2018}
}
Web of Science
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