Permeability and Compressibility of “Seal” Sediment Overlying the B1 Sand Gas Hydrate Reservoir: Hydrate 02 Geo Data Well, Prudhoe Bay Unit, Alaska North Slope

Abstract An important element in evaluating the viability of extracting methane from a gas hydrate-bearing reservoir is establishing the effectiveness of the overlying bounding sediment as a seal to prevent gas loss, to enable effective depressurization, and to prevent fluid from entering the reservoir during production. This laboratory study presents results for index properties (e.g., grain density, grain size, and liquid limit), compressibility and swelling indices, and permeability measurements on sediment overlying the gas hydrate-bearing reservoir that was the target of the recent JOGMEC-DOE-USGS collaborative gas hydrate production testing project on the Alaska North Slope (ANS). Sediment analyzed in this study was collected during pressure coring operations in the HYDRATE 02 Geo Data Well (GDW). The ∼6.1 m sediment interval recovered in Cores 13P and 14P (878.74–884.88 m measured depth, MD) exhibited heterogeneous sedimentologic characteristics at the centimeter scale, with sediments ranging from clay to thin silty-sand lithologies. Permeability measurements and index-property correlations indicate the interval’s overall in situ vertical permeability ranges from 0.2 to 3.6 microdarcy (μD). Results for compressibility (CC = 0.255 ± 0.02) and swelling index (CS = 0.04 ± 0.01) are consistent with estimates based on mineralogy and liquid limit correlations. Based on the measured compressibility, the ∼3 MPa increase in effective stress during the stable phase of depressurization-induced production is anticipated to have imposed 2.43 cm of compaction per meter in the reservoir overburden, reducing permeability by ∼36%. The overburden sediment’s low in situ permeability (3 to 4 orders of magnitude below permeabilities measured in the gas hydrate-bearing part of the B1 sand (unit B)) suggests the B1 sand′s overburden provides an effective seal. Such a seal promotes efficient production by limiting fluid flow into the reservoir during depressurization-induced gas hydrate dissociation.

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Publication Details

Journal
Energy & Fuels
Published
2026-09-10
DOI
https://doi.org/10.1021/acs.energyfuels.5c04831
Primary Topic
Methane Hydrates and Related Phenomena
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article
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article

Permeability and Compressibility of “Seal” Sediment Overlying the B1 Sand Gas Hydrate Reservoir: Hydrate 02 Geo Data Well, Prudhoe Bay Unit, Alaska North Slope

Jun Yoneda, Akihiro Hiruta, Stephen C. Phillips, Timothy S. Collett et al.
Energy & Fuels
Methane Hydrates and Related Phenomena
article

Permeability and Compressibility of “Seal” Sediment Overlying the B1 Sand Gas Hydrate Reservoir: Hydrate 02 Geo Data Well, Prudhoe Bay Unit, Alaska North Slope

Jun Yoneda, Akihiro Hiruta, Stephen C. Phillips, Timothy S. Collett, William F. Waite, Adrian V. Garcia
article en

Abstract

Abstract An important element in evaluating the viability of extracting methane from a gas hydrate-bearing reservoir is establishing the effectiveness of the overlying bounding sediment as a seal to prevent gas loss, to enable effective depressurization, and to prevent fluid from entering the reservoir during production. This laboratory study presents results for index properties (e.g., grain density, grain size, and liquid limit), compressibility and swelling indices, and permeability measurements on sediment overlying the gas hydrate-bearing reservoir that was the target of the recent JOGMEC-DOE-USGS collaborative gas hydrate production testing project on the Alaska North Slope (ANS). Sediment analyzed in this study was collected during pressure coring operations in the HYDRATE 02 Geo Data Well (GDW). The ∼6.1 m sediment interval recovered in Cores 13P and 14P (878.74–884.88 m measured depth, MD) exhibited heterogeneous sedimentologic characteristics at the centimeter scale, with sediments ranging from clay to thin silty-sand lithologies. Permeability measurements and index-property correlations indicate the interval’s overall in situ vertical permeability ranges from 0.2 to 3.6 microdarcy (μD). Results for compressibility (CC = 0.255 ± 0.02) and swelling index (CS = 0.04 ± 0.01) are consistent with estimates based on mineralogy and liquid limit correlations. Based on the measured compressibility, the ∼3 MPa increase in effective stress during the stable phase of depressurization-induced production is anticipated to have imposed 2.43 cm of compaction per meter in the reservoir overburden, reducing permeability by ∼36%. The overburden sediment’s low in situ permeability (3 to 4 orders of magnitude below permeabilities measured in the gas hydrate-bearing part of the B1 sand (unit B)) suggests the B1 sand′s overburden provides an effective seal. Such a seal promotes efficient production by limiting fluid flow into the reservoir during depressurization-induced gas hydrate dissociation.

Energy & Fuels
United States Geological Survey (US), National Institute of Advanced Industrial Science and Technology (JP)
Life below water
Openalex Percentile: Top 18%
Methane Hydrates and Related Phenomena
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