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Title: Methane Hydrate Formation in Thick Sandstones by Free Gas Flow

Abstract

We show with a two-dimensional multiphase flow and multicomponent transport model that free gas flow is a viable mechanism to form concentrated methane hydrate in meter-scale, dipping sandstones far above the base of the hydrate stability zone (BHSZ). In this model, gas preferentially flows updip along the top of sandstone due to buoyancy. This drives hydrate formation, increasing the local salinity to the stability limit and developing three-phase (gas, liquid, and hydrate) equilibrium above the BHSZ. With time, the gas and the hydrate solidification front (HSF) advance together updip. Behind the HSF, hydrate continues to form as the elevated salinity diffuses away. High hydrate saturations reduce the sediment permeability significantly. As a result, as the gas and HSF move updip, they are also pushed perpendicularly from the top to the base of the sandstone. The hydrate system ultimately self-seals itself due to reduced permeability across the entire thickness of the sandstone. Gas starts to retreat downdip and accumulates below the BHSZ. With this model high hydrate saturations form far above the BHSZ at high methane supply rates while hydrate is concentrated at the BHSZ or no hydrate forms at low methane supply rates. This study provides further insights into hydratemore » formation by free gas flow, which can be used to design the best strategies for economic and environmental production of methane from hydrate reservoirs.« less

Authors:
ORCiD logo [1];  [1]
  1. Univ. of Texas, Austin, TX (United States)
Publication Date:
Research Org.:
Univ. of Texas, Austin, TX (United States)
Sponsoring Org.:
USDOE Office of Fossil Energy (FE)
OSTI Identifier:
1539753
Alternate Identifier(s):
OSTI ID: 1454905
Grant/Contract Number:  
FE0010406
Resource Type:
Journal Article: Accepted Manuscript
Journal Name:
Journal of Geophysical Research. Solid Earth
Additional Journal Information:
Journal Volume: 123; Journal Issue: 6; Journal ID: ISSN 2169-9313
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; Geochemistry & Geophysics

Citation Formats

You, Kehua, and Flemings, Peter B. Methane Hydrate Formation in Thick Sandstones by Free Gas Flow. United States: N. p., 2018. Web. doi:10.1029/2018jb015683.
You, Kehua, & Flemings, Peter B. Methane Hydrate Formation in Thick Sandstones by Free Gas Flow. United States. https://doi.org/10.1029/2018jb015683
You, Kehua, and Flemings, Peter B. Wed . "Methane Hydrate Formation in Thick Sandstones by Free Gas Flow". United States. https://doi.org/10.1029/2018jb015683. https://www.osti.gov/servlets/purl/1539753.
@article{osti_1539753,
title = {Methane Hydrate Formation in Thick Sandstones by Free Gas Flow},
author = {You, Kehua and Flemings, Peter B.},
abstractNote = {We show with a two-dimensional multiphase flow and multicomponent transport model that free gas flow is a viable mechanism to form concentrated methane hydrate in meter-scale, dipping sandstones far above the base of the hydrate stability zone (BHSZ). In this model, gas preferentially flows updip along the top of sandstone due to buoyancy. This drives hydrate formation, increasing the local salinity to the stability limit and developing three-phase (gas, liquid, and hydrate) equilibrium above the BHSZ. With time, the gas and the hydrate solidification front (HSF) advance together updip. Behind the HSF, hydrate continues to form as the elevated salinity diffuses away. High hydrate saturations reduce the sediment permeability significantly. As a result, as the gas and HSF move updip, they are also pushed perpendicularly from the top to the base of the sandstone. The hydrate system ultimately self-seals itself due to reduced permeability across the entire thickness of the sandstone. Gas starts to retreat downdip and accumulates below the BHSZ. With this model high hydrate saturations form far above the BHSZ at high methane supply rates while hydrate is concentrated at the BHSZ or no hydrate forms at low methane supply rates. This study provides further insights into hydrate formation by free gas flow, which can be used to design the best strategies for economic and environmental production of methane from hydrate reservoirs.},
doi = {10.1029/2018jb015683},
url = {https://www.osti.gov/biblio/1539753}, journal = {Journal of Geophysical Research. Solid Earth},
issn = {2169-9313},
number = 6,
volume = 123,
place = {United States},
year = {2018},
month = {5}
}

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Works referenced in this record:

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    Works referencing / citing this record:

    Mechanisms of Methane Hydrate Formation in Geological Systems
    journal, October 2019


    Factors Controlling Short‐Range Methane Migration of Gas Hydrate Accumulations in Thin Coarse‐Grained Layers
    journal, August 2019


    High‐Saturation Gas Hydrate Reservoirs—A Pore Scale Investigation of Their Formation From Free Gas and Dissociation in Sediments
    journal, December 2019