Gas Hydrate Stability Zone in Offshore Southern Taiwan

Methane hydrates are considered a major potential source of hydrocarbon energy and could be important in meeting natural gas demand in the future. To study the feasibility of recovering methane from the offshore southern Taiwan region and its impact on many geological processes, it is necessary to k...

Full description

Bibliographic Details
Main Authors: Wu-Cheng Chi, Donald L. Reed, Chih-Chin Tsai
Format: Article
Language:English
Published: Springer 2006-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v174p829.pdf
_version_ 1828365687326769152
author Wu-Cheng Chi
Donald L. Reed
Chih-Chin Tsai
author_facet Wu-Cheng Chi
Donald L. Reed
Chih-Chin Tsai
author_sort Wu-Cheng Chi
collection DOAJ
description Methane hydrates are considered a major potential source of hydrocarbon energy and could be important in meeting natural gas demand in the future. To study the feasibility of recovering methane from the offshore southern Taiwan region and its impact on many geological processes, it is necessary to know the total amount of hydrate in the region; something that is still unclear. Here we take the first step using a bottom-simulating reflector (BSR) to estimate the total volume of the stability field that can hold hydrates in the sediments offshore of southern Taiwan. We used a dense grid of 6-channel and 120-channel reflection profiles to study the distribution and sub-bottom depth of a BSR. BSRs are marked by a reversed polarity reflector that increases in sub-bottom depth with increasing water depth, suggesting that BSRs mark the base of methane hydrate stability zones. For offshore Taiwan a BSR is located in offscraped sediments derived from the Taiwan orogen and the Chinese continental margin. These sediments may have high amounts of organic carbon, thereby providing a source for the methane. We document the areal extent and subbottom depth of BSRs covering a 45000 km2-wide region. The BSRs were classified into three categories based on how well they fit the seismic characteristics of the BSR associated with hydrates. Q1 BSR fits with all the expected seismic attributes to be found at the base of a hydrate boundary, while Q2 and Q3 BSRs are possible and probable reflectors resulting from such a boundary. We then estimate the volume of the hydrate stability zone bounded between the seafloor and the mapped BSRs in the offshore region. At least 1023 km3 of the hydrate stability field is underlain by the highest quality BSRs while as much as 11522 km3 is underlain by all mapped BSRs. We then speculated on the total amount of hydrate stored in the region using published regional porosity-depth relations and assuming a range of saturation values of hydrates in the pore spaces. Hydrate storage can be better estimated once additional porosity and saturation information becomes available.
first_indexed 2024-04-14T05:34:20Z
format Article
id doaj.art-fe340c874e4642caa378259cc210cb95
institution Directory Open Access Journal
issn 1017-0839
2311-7680
language English
last_indexed 2024-04-14T05:34:20Z
publishDate 2006-01-01
publisher Springer
record_format Article
series Terrestrial, Atmospheric and Oceanic Sciences
spelling doaj.art-fe340c874e4642caa378259cc210cb952022-12-22T02:09:42ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802006-01-0117482910.3319/TAO.2006.17.4.829(GH)Gas Hydrate Stability Zone in Offshore Southern TaiwanWu-Cheng ChiDonald L. ReedChih-Chin TsaiMethane hydrates are considered a major potential source of hydrocarbon energy and could be important in meeting natural gas demand in the future. To study the feasibility of recovering methane from the offshore southern Taiwan region and its impact on many geological processes, it is necessary to know the total amount of hydrate in the region; something that is still unclear. Here we take the first step using a bottom-simulating reflector (BSR) to estimate the total volume of the stability field that can hold hydrates in the sediments offshore of southern Taiwan. We used a dense grid of 6-channel and 120-channel reflection profiles to study the distribution and sub-bottom depth of a BSR. BSRs are marked by a reversed polarity reflector that increases in sub-bottom depth with increasing water depth, suggesting that BSRs mark the base of methane hydrate stability zones. For offshore Taiwan a BSR is located in offscraped sediments derived from the Taiwan orogen and the Chinese continental margin. These sediments may have high amounts of organic carbon, thereby providing a source for the methane. We document the areal extent and subbottom depth of BSRs covering a 45000 km2-wide region. The BSRs were classified into three categories based on how well they fit the seismic characteristics of the BSR associated with hydrates. Q1 BSR fits with all the expected seismic attributes to be found at the base of a hydrate boundary, while Q2 and Q3 BSRs are possible and probable reflectors resulting from such a boundary. We then estimate the volume of the hydrate stability zone bounded between the seafloor and the mapped BSRs in the offshore region. At least 1023 km3 of the hydrate stability field is underlain by the highest quality BSRs while as much as 11522 km3 is underlain by all mapped BSRs. We then speculated on the total amount of hydrate stored in the region using published regional porosity-depth relations and assuming a range of saturation values of hydrates in the pore spaces. Hydrate storage can be better estimated once additional porosity and saturation information becomes available. http://tao.cgu.org.tw/images/attachments/v174p829.pdf Bottom-simulating reflectorMethane hydrateTaiwan
spellingShingle Wu-Cheng Chi
Donald L. Reed
Chih-Chin Tsai
Gas Hydrate Stability Zone in Offshore Southern Taiwan
Terrestrial, Atmospheric and Oceanic Sciences
Bottom-simulating reflector
Methane hydrate
Taiwan
title Gas Hydrate Stability Zone in Offshore Southern Taiwan
title_full Gas Hydrate Stability Zone in Offshore Southern Taiwan
title_fullStr Gas Hydrate Stability Zone in Offshore Southern Taiwan
title_full_unstemmed Gas Hydrate Stability Zone in Offshore Southern Taiwan
title_short Gas Hydrate Stability Zone in Offshore Southern Taiwan
title_sort gas hydrate stability zone in offshore southern taiwan
topic Bottom-simulating reflector
Methane hydrate
Taiwan
url http://tao.cgu.org.tw/images/attachments/v174p829.pdf
work_keys_str_mv AT wuchengchi gashydratestabilityzoneinoffshoresoutherntaiwan
AT donaldlreed gashydratestabilityzoneinoffshoresoutherntaiwan
AT chihchintsai gashydratestabilityzoneinoffshoresoutherntaiwan