Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02

Understanding how effectively methane can be extracted from a gas hydrate reservoir requires knowing how compressible, permeable, and strong the overlying seal sediment is. This data release provides results for flow-through permeability, consolidation, and direct shear measurements made on fine-gra...

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Main Authors: Jang, Junbong, Dai, Sheng, Yoneda, Jun, Waite, William F., Collett, Timothy S., Kumar, Pushpendra
Format: Dataset
Language:unknown
Published: U.S. Geological Survey 2018
Subjects:
Online Access:https://dx.doi.org/10.5066/p91xj7dp
https://www.sciencebase.gov/catalog/item/5b645dffe4b006a11f72ed13
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spelling ftdatacite:10.5066/p91xj7dp 2023-05-15T17:58:06+02:00 Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02 Jang, Junbong Dai, Sheng Yoneda, Jun Waite, William F. Collett, Timothy S. Kumar, Pushpendra 2018 https://dx.doi.org/10.5066/p91xj7dp https://www.sciencebase.gov/catalog/item/5b645dffe4b006a11f72ed13 unknown U.S. Geological Survey dataset Dataset 2018 ftdatacite https://doi.org/10.5066/p91xj7dp 2021-11-05T12:55:41Z Understanding how effectively methane can be extracted from a gas hydrate reservoir requires knowing how compressible, permeable, and strong the overlying seal sediment is. This data release provides results for flow-through permeability, consolidation, and direct shear measurements made on fine-grained seal sediment from Site NGHP-02-08 offshore eastern India. The sediment was collected in a pressure core from the Krishna-Godavari Basin during the 2015 Indian National Gas Hydrate Program Expedition 2 (NGHP-02). Gas hydrate is a crystalline solid that forms naturally in the sediment of certain marine and permafrost environments where pressure is relatively high (equivalent to the pressure measured ~300 meters water depth or more) and temperature is relatively low (but generally above freezing). The concentration of methane can be high enough to make certain gas hydrate occurrences potentially relevant as energy resources. To extract methane from gas hydrate, the in situ formation (generally a coarse-grained, gas-hydrate-bearing sediment interval) can be depressurized by drawing pore water out through a production well. As the pore pressure falls below the gas hydrate stability limit, the solid gas hydrate breaks down, releasing gas and water that migrate toward the production well for collection. How effectively the production well can depressurize the gas-hydrate-bearing interval depends on how permeable the overlying seal sediment is. If the seal is permeable, depressurizing the reservoir to extract methane causes water to flow out of the seal and into the reservoir. This can limit the ability of the production well to maintain the low reservoir pressure required to break down gas. Dataset permafrost DataCite Metadata Store (German National Library of Science and Technology) Indian
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description Understanding how effectively methane can be extracted from a gas hydrate reservoir requires knowing how compressible, permeable, and strong the overlying seal sediment is. This data release provides results for flow-through permeability, consolidation, and direct shear measurements made on fine-grained seal sediment from Site NGHP-02-08 offshore eastern India. The sediment was collected in a pressure core from the Krishna-Godavari Basin during the 2015 Indian National Gas Hydrate Program Expedition 2 (NGHP-02). Gas hydrate is a crystalline solid that forms naturally in the sediment of certain marine and permafrost environments where pressure is relatively high (equivalent to the pressure measured ~300 meters water depth or more) and temperature is relatively low (but generally above freezing). The concentration of methane can be high enough to make certain gas hydrate occurrences potentially relevant as energy resources. To extract methane from gas hydrate, the in situ formation (generally a coarse-grained, gas-hydrate-bearing sediment interval) can be depressurized by drawing pore water out through a production well. As the pore pressure falls below the gas hydrate stability limit, the solid gas hydrate breaks down, releasing gas and water that migrate toward the production well for collection. How effectively the production well can depressurize the gas-hydrate-bearing interval depends on how permeable the overlying seal sediment is. If the seal is permeable, depressurizing the reservoir to extract methane causes water to flow out of the seal and into the reservoir. This can limit the ability of the production well to maintain the low reservoir pressure required to break down gas.
format Dataset
author Jang, Junbong
Dai, Sheng
Yoneda, Jun
Waite, William F.
Collett, Timothy S.
Kumar, Pushpendra
spellingShingle Jang, Junbong
Dai, Sheng
Yoneda, Jun
Waite, William F.
Collett, Timothy S.
Kumar, Pushpendra
Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02
author_facet Jang, Junbong
Dai, Sheng
Yoneda, Jun
Waite, William F.
Collett, Timothy S.
Kumar, Pushpendra
author_sort Jang, Junbong
title Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02
title_short Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02
title_full Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02
title_fullStr Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02
title_full_unstemmed Pressure Core Characterization Tool Measurements of Compressibility, Permeability, and Shear Strength of Fine-Grained Sediment Collected from Area C, Krishna-Godavari Basin, during India's National Gas Hydrate Program Expedition NGHP-02
title_sort pressure core characterization tool measurements of compressibility, permeability, and shear strength of fine-grained sediment collected from area c, krishna-godavari basin, during india's national gas hydrate program expedition nghp-02
publisher U.S. Geological Survey
publishDate 2018
url https://dx.doi.org/10.5066/p91xj7dp
https://www.sciencebase.gov/catalog/item/5b645dffe4b006a11f72ed13
geographic Indian
geographic_facet Indian
genre permafrost
genre_facet permafrost
op_doi https://doi.org/10.5066/p91xj7dp
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