我国冻土区天然气水合物长期观测基地建设必要性
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- 论文作者：庞守吉 ; 祝有海 ; 王平康 ; 黄霞 ; 张帅
- 年：2013
- 作者机构：中国地质调查局油气资源调查中心;
- 会议召开时间：2013-04-16
- 会议录名称：第一届全国青年地质大会论文集
- 语种：中文
- 分类号：P618.13
- 学会代码：DXHD
- 会议名称：第一届全国青年地质大会
- 会议地点：中国福建福州
- 主办单位：中国地质学会青年工作委员会
- 学会名称：中国地质学会地质学报编辑部
- 页数：3
- 文件大小：199k
- 原文格式：O
- 会议级别：全国
摘要
<正>天然气水合物(Natural Gas Hydrate)主要分布于多年冻土区、大陆架边缘的海洋沉积物和深湖泊沉积物中。在标准状况下,1 m~3水合物分解最多可产生164 m~3的甲烷和0.8 m~3的水。据估计,全球天然气水合物中的碳储量为2×10~(16)m~3,相当于全球已探明常规化石燃料总碳量的2倍以上(Kvenvolden,1999)。作为一种洁净能源(Lee et al.,2001),天然气水合物同时具有分布广泛、资源量大、埋藏浅、能源密度高等特点,目前已被视为未来石油、天然气的一种新型潜在替代能源。1国外冻土区水合物研究现状国外冻土区发现天然气水合物的地区主要包
引文
韩路,武淑娇,李建华,吕杰,祝有海.2011.祁连山冻土区天然气水合物DK-2钻孔微生物群落.地质通报,30(12):1874-1882.
黄霞,祝有海,王平康,郭星旺.2011.祁连山冻土区天然气水合物烃类气体组分的特征和成因.地质通报,30(12):1851-1856.
卢振权,祝有海,张永勤,文怀军,李永红,贾志耀,王平康,李清海.2010b.青海祁连山冻土区天然气水合物的气体成因研究.现代地质,24(3):581-588.
庞守吉,苏新,杨旭,王平康,李永红,郭星旺,李清海.2011.祁连山冻土区天然气水合物科学钻探试验井中侏罗统的沉积学特征.地质通报,30(12):1829-1838.
王平康,祝有海,卢振权,郭星旺,黄霞.2011.祁连山冻土区天然气水合物岩性和分布特征.地质通报,30(12):1839-1850.
赵省民,邓坚,李锦平,陆程,宋健.2011.漠河多年冻土区天然气水合物的形成条件及成藏潜力研究.地质学报,85(9):1536-1550.
祝有海,张永勤,文怀军,卢振权,王平康.2010.祁连山冻土区天然气水合物及其基本特征.地球学报,31(1):7-16.
祝有海.2006.加拿大马更些冻土区天然气水合物试生产进展与展望地球科学进展.地球科学进展,21(5):513-520.
Bock M,Schmitt J,Moller L.2010.Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-oeschger events.Science,328:1686-1691.
BrookE,Archer D,Dlugokencky E.2008.US Climate Change Science Program-Synthesis and Assessment Report 3.4:Abrupt Climate Change.US Geological Survey,2008.
CoUett T S,Dallimore S R.2000.Permafrost-related natural gas hydrate.In Max M D ed.Natural Gas Hydrate in Oceanic and Permafrost Environments.The Netherlands:Kluwer Academic Publishers,43-60.
CoUett T S.1993.Permafrost-associated gas hydrate accumulations.In Sloan E D,Happer J,Hnatow M ed.International Conference on Natural Gas Hydrates.Annals of the New York Academy of Science,715:247-269.
CoUett T S.2002.Energy resource potential of natural gas hydrates.AAPG,86(11):1971-1992.
Connell-Madore S and Katsube T J.2007.Grain-size distribution and gas permeability of sediment samples from the JPEX/JNOC/GSC et al.Mallik 5L-38 gas hydrate production research well,Northwest Territories.Geological Survey of Canada,Current Research,6:13.
Dallimore S R,Collett T S.1999.Regional gas hydrate occurrences,permafrost conditions,and Cenozoic geology,Mackenzie Delta area.In Dallimore S R,Uchida T,CoUett T S ed.Scientific Result s f rom JAPEX/JNOC/GSC Mallik 2L-38 Gas Hydrate Research Well,Mackenzie Delta,Northwest Territories,Canada.Geological Survey of Canada,Bulletin,544:31-43.
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Lee S Y,Gerald D H.2001.Methane hydrates potential as a future energy source.Fuel Processing Technology,71:181-186.
Milkov A V.2005.Molecular and stable isotope compositions of natural gas hydrates;a revised global dataset and basic interpretations in the context of geological settings.Organic Geochemistry,36(5):681-702.
NSF.2010.Methane releases from arctic shelf May Be Much Larger and Faster Than Anticipated,http//www.eurek alert org/pub_releases/2010-03/nsf-mrf030410.php,2010.
Schiermeier Q.2008.Fears surface over methane leaks.Nature,4SS:572-573.
Sowers T.2006.Late quaternary atmospheric CH4 isotope record suggests marine clatherates are stable.Science,311:838-840.
Yakushei V.S.,Chufilinr E.M.2000.Natural gas and gas hydrate accumulations within permafrost in Russia.Cold Regions Science and Technology,31:189-197.
黄霞,祝有海,王平康,郭星旺.2011.祁连山冻土区天然气水合物烃类气体组分的特征和成因.地质通报,30(12):1851-1856.
卢振权,祝有海,张永勤,文怀军,李永红,贾志耀,王平康,李清海.2010b.青海祁连山冻土区天然气水合物的气体成因研究.现代地质,24(3):581-588.
庞守吉,苏新,杨旭,王平康,李永红,郭星旺,李清海.2011.祁连山冻土区天然气水合物科学钻探试验井中侏罗统的沉积学特征.地质通报,30(12):1829-1838.
王平康,祝有海,卢振权,郭星旺,黄霞.2011.祁连山冻土区天然气水合物岩性和分布特征.地质通报,30(12):1839-1850.
赵省民,邓坚,李锦平,陆程,宋健.2011.漠河多年冻土区天然气水合物的形成条件及成藏潜力研究.地质学报,85(9):1536-1550.
祝有海,张永勤,文怀军,卢振权,王平康.2010.祁连山冻土区天然气水合物及其基本特征.地球学报,31(1):7-16.
祝有海.2006.加拿大马更些冻土区天然气水合物试生产进展与展望地球科学进展.地球科学进展,21(5):513-520.
Bock M,Schmitt J,Moller L.2010.Hydrogen isotopes preclude marine hydrate CH4 emissions at the onset of Dansgaard-oeschger events.Science,328:1686-1691.
BrookE,Archer D,Dlugokencky E.2008.US Climate Change Science Program-Synthesis and Assessment Report 3.4:Abrupt Climate Change.US Geological Survey,2008.
CoUett T S,Dallimore S R.2000.Permafrost-related natural gas hydrate.In Max M D ed.Natural Gas Hydrate in Oceanic and Permafrost Environments.The Netherlands:Kluwer Academic Publishers,43-60.
CoUett T S.1993.Permafrost-associated gas hydrate accumulations.In Sloan E D,Happer J,Hnatow M ed.International Conference on Natural Gas Hydrates.Annals of the New York Academy of Science,715:247-269.
CoUett T S.2002.Energy resource potential of natural gas hydrates.AAPG,86(11):1971-1992.
Connell-Madore S and Katsube T J.2007.Grain-size distribution and gas permeability of sediment samples from the JPEX/JNOC/GSC et al.Mallik 5L-38 gas hydrate production research well,Northwest Territories.Geological Survey of Canada,Current Research,6:13.
Dallimore S R,Collett T S.1999.Regional gas hydrate occurrences,permafrost conditions,and Cenozoic geology,Mackenzie Delta area.In Dallimore S R,Uchida T,CoUett T S ed.Scientific Result s f rom JAPEX/JNOC/GSC Mallik 2L-38 Gas Hydrate Research Well,Mackenzie Delta,Northwest Territories,Canada.Geological Survey of Canada,Bulletin,544:31-43.
Dallimore S R,CoUett T S.2005.Summary and implication of the MaUik2002 gas hydrate production research well program//Dallimore S R,CoUett T S,eds.Scientific Results from the Mallik 2002 Gas Hydrate Production Research Well Program,Mackenzie Delta,Northwest Territories,Canada.Geological Survey of Canada,Bulletin 585:1-36.
Kvenvolden K A.1999.Potential effects of gas hydrate on human welfare//Prorceeding of National Academy of Science Colloquium.USA,96:3420-3426.
Lee S Y,Gerald D H.2001.Methane hydrates potential as a future energy source.Fuel Processing Technology,71:181-186.
Milkov A V.2005.Molecular and stable isotope compositions of natural gas hydrates;a revised global dataset and basic interpretations in the context of geological settings.Organic Geochemistry,36(5):681-702.
NSF.2010.Methane releases from arctic shelf May Be Much Larger and Faster Than Anticipated,http//www.eurek alert org/pub_releases/2010-03/nsf-mrf030410.php,2010.
Schiermeier Q.2008.Fears surface over methane leaks.Nature,4SS:572-573.
Sowers T.2006.Late quaternary atmospheric CH4 isotope record suggests marine clatherates are stable.Science,311:838-840.
Yakushei V.S.,Chufilinr E.M.2000.Natural gas and gas hydrate accumulations within permafrost in Russia.Cold Regions Science and Technology,31:189-197.