Carbon Sequestration Potential of Yanchang Formation Sandstone of JX Well, Ordos Basin

MING XiaoRan; LIU Li; LIU NaNa; SONG TuShun; WANG FuGang; YU YanLong

doi:10.14027/j.cnki.cjxb.2015.01.021

Volume 33 Issue 1

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MING XiaoRan, LIU Li, LIU NaNa, SONG TuShun, WANG FuGang, YU YanLong. Carbon Sequestration Potential of Yanchang Formation Sandstone of JX Well, Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 202-210. doi: 10.14027/j.cnki.cjxb.2015.01.021

Citation:

MING XiaoRan, LIU Li, LIU NaNa, SONG TuShun, WANG FuGang, YU YanLong. Carbon Sequestration Potential of Yanchang Formation Sandstone of JX Well, Ordos Basin[J]. Acta Sedimentologica Sinica, 2015, 33(1): 202-210. doi: 10.14027/j.cnki.cjxb.2015.01.021

Carbon Sequestration Potential of Yanchang Formation Sandstone of JX Well, Ordos Basin

doi: 10.14027/j.cnki.cjxb.2015.01.021

1.
College of Earth Sciences of Jilin University, Changchun 130061;
2.
College of Environment and Resources of Jilin University, Changchun 130021

Received Date: 2013-12-25
Rev Recd Date: 2014-03-17
Publish Date: 2015-02-10

Abstract

There are still some controversies surrounding the security of mudstone upon injection layer of CO₂ injection project that implemented by Shenhua Group in the potential target area of CO₂ underground embedded, Ordos Basin. Forecast the ability of adjourned carbon sequestration after CO₂ penetrate cap rock by research of JX well Yanchang Formation(upon injection layer) that adjacent to injection well of Shenhua Group that the drilling stratigraphic system and rock assemblage are same. The samples of researching layer are mainly feldspar sandstone and lithic feldspar sandstone, followed by lithic sandstone and lithic quartz sandstone, and the rock types of provenance are mainly felsic volcanic rocks, followed by intermediate volcanic rocks and a small amount of quartz sedimentary rock, with componential characteristics of neutral anorthosite at the same time. The parent rocks of sandstone of the upper section(466~534 m) and lower section(666~958 m) suffered weak-medium chemical alteration, maybe they experienced recycling process, but the parent rocks of sandstone in the middle section(534~666 m) did not suffer from chemical alteration and they are likely the first cycle sediment. As the place of adjourned carbon sequestration, Yanchang Formation has the material conditions of achieving CO₂ mineral traps and potential of forming dawsonite, calcite, ankerite and siderite which called sequestration mineral.
- Erdos Basin,
- Yanchang Formation,
- petrology,
- geochemistry,
- carbon sequestration potential

References

[1]	Bachu S, Adams J J.Sequestration of CO₂ in geological media in response to climate change: Capacity of deep saline aquifers to sequester CO₂ in solution[J]. Energy Conversion and Management, 2003, 44(20): 3151-3175.
[2]	李小春,刘延峰,白冰,等. 中国深部咸水含水层CO₂储存优先区域选择[J]. 岩石力学与工程学报,2006,25(5):963-968.[Li Xiaochun, Liu Yanfeng, Bai Bing, et al. Ranking and screening of CO₂ saline aquifer storage zones in China[J]. Chinese Journal of Rock Mechanics and Engineering, 2006, 25(5): 963-968.]
[3]	郭建强,张森琦,刁玉杰,等. 深部咸水层CO₂地质储存工程场地选址技术方法[J]. 吉林大学学报:地球科学版,2011,41(4):1084-1091.[Guo Jianqiang, Zhang Senqi, Diao Yujie, et al. Site selection method of CO₂ geological storage in deep saline aquifers[J]. Journal of Jilin University: Earth Science Edition, 2011, 41(4): 1084-1091.]
[4]	Winter E M, Bergman P D.Availability of depleted oil and gas reservoirs for disposal of carbon dioxide in the United States[J]. Energy Conversion and Management, 1993, 34(9//10/11): 1177-1187.
[5]	Bachu S, Shaw J.Evaluation of the CO₂ sequestration capacity in Alberta's oil and gas reservoirs at depletion and the effect of underlying aquifers[J]. Journal of Canadian Petroleum Technology, 2003, 42(9): 51-61.
[6]	Credoz A, Bildstein O, Jullien M,et al. Experimental and modeling study of geochemical reactivity between clayey cap rocks and CO₂ in geological storage conditions[J]. Energy Procedia, 2009, 1(1): 3445-3452.
[7]	李小春,小出仁,大隅多加志. 二氧化碳地中隔离技术及其岩石力学问题[J]. 岩石力学与工程学报,2003,22(6):989-994.[Li Xiaochun, Hitoshi K, Takashi O. CO₂ aquifer storage and the related rock mechanics issues[J]. Chinese Journal of Rock Mechanics and Engineering, 2003, 22(6): 989-994.]
[8]	宋新民,杨思玉. 国内外CCS技术现状与中国主动应对策略[J]. 油气藏评价与开发,2011,1(1/2):25-30.[Song Xinmin, Yang Siyu. Current situation of CCS technology at home and abroad and the positive strategy that China should adopt toward it[J]. Reservoir Evaluation and Development, 2011, 1(1/2): 25-30.]
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[10]	Torpa T A, Gale J.Demonstrating storage of CO₂ in geological reservoirs: the Sleipner and SACS projects[J]. Energy, 2004, 29(9/10): 1361-1369.
[11]	Moritis G.CO₂ sequestration adds new dimension to oil, gas production[J]. Oil and Gas Journal, 2003, 101(9): 71-83.
[12]	曲建升,曾静静. 二氧化碳捕获与封存:技术、实践与法律——国际推广二氧化碳捕获与封存工作的法律问题分析[J]. 世界科技研究与发展,2007,29(6):78-83.[Qu Jiansheng, Zeng Jingjing. Carbon dioxide capture and storage: technology, demonstration, and legal aspects——an analysis on the legal related issues of international CCS efforts[J]. World Sci-tech R & D, 2007, 29(6): 78-83.]
[13]	郑晓鹏. 海上天然气田伴生CO₂的海上捕集及回注技术[J]. 中国造船,2007,48(增刊):297-302.[Zheng Xiaopeng. Study on offshore associated CO₂ capture and injection technology[J]. Shipbuilding of China, 2007, 48(Suppl.): 297-302.]
[14]	张鸿翔,李小春,魏宁. 二氧化碳捕获与封存的主要技术环节与问题分析[J]. 地球科学进展,2010,25(3):335-340.[Zhang Hongxiang, Li Xiaochun, Wei Ning. The major technology track and analysis about carbon dioxide capture and storage[J]. Advances in Earth Science, 2010, 25(3): 335-340.]
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[16]	Roser B P, Korsch R J. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data[J]. Chemical Geology, 1988, 67(1/2): 119-139.
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[18]	Pettijohn F J. Sedimentary Rocks[M]. New York: Harper & Row, 1957: 224-242.
[19]	Bock B, McLennan S M, Hanson G N.Geochemistry and provenance of the Middle Ordovician Austin Glen Member (Normanskill Formation) and the Taconian Orogeny in New England[J]. Sedimentology, 1998, 45(4): 635-655.
[20]	Haskin L A, Haskin M A, Frey F A, et al. Relative and absolute terrestrial abundances of the rare earths[M]// Ahrens L H. Origin and Distribution of the Elements. Oxford: Pergamon, 1968: 889-911.
[21]	王清晨,从柏林. 大别山超高压变质岩的地球动力学意义[J]. 中国科学(D辑):地球科学,1996,26(3):271-276.[Wang Qingchen, Cong Bolin. Geodynamic significance of ultrahigh pressure metamorphic rocks of Dabie Mountain[J]. Science China (Seri. D):Earth Sciences, 1996, 26(3): 271-276.]
[22]	赵振华. 微量元素地球化学原理[M]. 北京:科学出版社,1997: 199-204.[Zhao Zhenhua. Principle of Trace Element Geochemistry[M]. Beijing: Science Press, 1997: 199-204.]
[23]	张英利,王宗起,闫臻,等. 库鲁克塔格地区新元古代贝义西组的构造环境:来自碎屑岩地球化学的证据[J]. 岩石学报,2011,27(6):1785-1796.[Zhang Yingli, Wang Zongqi, Yan Zhen, et al. Tectonic setting of Neoproterozoic Beiyixi Formation in Quruqtagh area, Xinjiang: Evidence from geochemistry of clastic rocks[J]. Acta Petrologica Sinica, 2011, 27(6): 1785-1796.]
[24]	毛光周,刘池洋. 地球化学在物源及沉积背景分析中的应用[J]. 地球科学与环境学报,2011,33(4):337-348.[Mao Guangzhou, Liu Chiyang. Application of geochemistry in provenance and depositional setting analysis[J]. Journal of Earth Sciences and Environment, 2011, 33(4): 337-348.]
[25]	童胜琪,刘志飞, Phon Le K,等. 红河盆地的化学风化作用:主要和微量元素地球化学记录[J]. 矿物岩石地球化学通报,2006,25(3):219-225.[Tong Shengqi, Liu Zhifei, Phon Le K, et al. Chemical weathering in the Red River Basin: records of major and trace elemental geochemistry[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2006, 25(3): 219-225.]
[26]	张鑫,张金亮. 东营凹陷南坡沙河街组四段砂岩地球化学特征[J]. 地质科学,2007,42(2):303-318.[Zhang Xin, Zhang Jinliang. Sedimento-geochemical features of sandstones from the fourth member, Shahejie Formation in the southern slope of Dongying sag [J]. Chinese Journal of Geology, 2007, 42(2): 303-318.]
[27]	Bachu S. Sequestration of CO₂ in geological media: criteria and approach for site selection in response to climate change[J]. Energy Conversion and Management, 2000, 41(9): 953-970.
[28]	高玉巧,刘立,曲希玉. CO₂与砂岩相互作用机理与形成的自生矿物组合[J]. 新疆石油地质,2007,28(5):579-584.[Gao Yuqiao, Liu Li, Qu Xiyu. Mechanism of CO₂-sandstone interaction and authigenic mineral assemblage[J]. Xinjiang Petroleum Geology, 2007, 28(5): 579-584.]
[29]	Berg A, Banwart S A.Carbon dioxide mediated dissolution of Ca-feldspar: implications for silicate weathering[J]. Chemical Geology, 2000, 163(1/2/3/4): 25-42.
[30]	Xu Tianfu, Apps J A, Pruess K. Mineral sequestration of carbon dioxide in a sandstone–shale system[J]. Chemical Geology, 2005, 217(3/4): 295-318.
[31]	Gunter W D, Perkins E H, McCann T J.Aquifer disposal of CO₂-rich gases: Reaction design for added capacity[J]. Energy Conversion and Management, 1993, 34(9/10/11): 941-948.
[32]	黄可可,黄思静,佟宏鹏,等. 长石溶解过程的热力学计算及其在碎屑岩储层研究中的意义[J]. 地质通报,2009,28(4):474-482.[Huang Keke, Huang Sijing, Tong Hongpeng, et al. The thermodynamic calculations of feldspar dissolution and significance of the study of clastic reservoirs[J]. Geological Bulletin of China, 2009, 28(4): 474-482.]
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Carbon Sequestration Potential of Yanchang Formation Sandstone of JX Well, Ordos Basin

1. College of Earth Sciences of Jilin University, Changchun 130061;

2. College of Environment and Resources of Jilin University, Changchun 130021

Received Date: 2013-12-25

Rev Recd Date: 2014-03-17

Publish Date: 2015-02-10

Key words:

Abstract: There are still some controversies surrounding the security of mudstone upon injection layer of CO₂ injection project that implemented by Shenhua Group in the potential target area of CO₂ underground embedded, Ordos Basin. Forecast the ability of adjourned carbon sequestration after CO₂ penetrate cap rock by research of JX well Yanchang Formation(upon injection layer) that adjacent to injection well of Shenhua Group that the drilling stratigraphic system and rock assemblage are same. The samples of researching layer are mainly feldspar sandstone and lithic feldspar sandstone, followed by lithic sandstone and lithic quartz sandstone, and the rock types of provenance are mainly felsic volcanic rocks, followed by intermediate volcanic rocks and a small amount of quartz sedimentary rock, with componential characteristics of neutral anorthosite at the same time. The parent rocks of sandstone of the upper section(466~534 m) and lower section(666~958 m) suffered weak-medium chemical alteration, maybe they experienced recycling process, but the parent rocks of sandstone in the middle section(534~666 m) did not suffer from chemical alteration and they are likely the first cycle sediment. As the place of adjourned carbon sequestration, Yanchang Formation has the material conditions of achieving CO₂ mineral traps and potential of forming dawsonite, calcite, ankerite and siderite which called sequestration mineral.

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Reference (37)

[1]	Bachu S, Adams J J.Sequestration of CO₂ in geological media in response to climate change: Capacity of deep saline aquifers to sequester CO₂ in solution[J]. Energy Conversion and Management, 2003, 44(20): 3151-3175.
[2]	李小春,刘延峰,白冰,等. 中国深部咸水含水层CO₂储存优先区域选择[J]. 岩石力学与工程学报,2006,25(5):963-968.[Li Xiaochun, Liu Yanfeng, Bai Bing, et al. Ranking and screening of CO₂ saline aquifer storage zones in China[J]. Chinese Journal of Rock Mechanics and Engineering, 2006, 25(5): 963-968.]
[3]	郭建强,张森琦,刁玉杰,等. 深部咸水层CO₂地质储存工程场地选址技术方法[J]. 吉林大学学报:地球科学版,2011,41(4):1084-1091.[Guo Jianqiang, Zhang Senqi, Diao Yujie, et al. Site selection method of CO₂ geological storage in deep saline aquifers[J]. Journal of Jilin University: Earth Science Edition, 2011, 41(4): 1084-1091.]
[4]	Winter E M, Bergman P D.Availability of depleted oil and gas reservoirs for disposal of carbon dioxide in the United States[J]. Energy Conversion and Management, 1993, 34(9//10/11): 1177-1187.
[5]	Bachu S, Shaw J.Evaluation of the CO₂ sequestration capacity in Alberta's oil and gas reservoirs at depletion and the effect of underlying aquifers[J]. Journal of Canadian Petroleum Technology, 2003, 42(9): 51-61.
[6]	Credoz A, Bildstein O, Jullien M,et al. Experimental and modeling study of geochemical reactivity between clayey cap rocks and CO₂ in geological storage conditions[J]. Energy Procedia, 2009, 1(1): 3445-3452.
[7]	李小春,小出仁,大隅多加志. 二氧化碳地中隔离技术及其岩石力学问题[J]. 岩石力学与工程学报,2003,22(6):989-994.[Li Xiaochun, Hitoshi K, Takashi O. CO₂ aquifer storage and the related rock mechanics issues[J]. Chinese Journal of Rock Mechanics and Engineering, 2003, 22(6): 989-994.]
[8]	宋新民,杨思玉. 国内外CCS技术现状与中国主动应对策略[J]. 油气藏评价与开发,2011,1(1/2):25-30.[Song Xinmin, Yang Siyu. Current situation of CCS technology at home and abroad and the positive strategy that China should adopt toward it[J]. Reservoir Evaluation and Development, 2011, 1(1/2): 25-30.]
[9]	IPCC. IPCC Special Report on Carbon Dioxide Capture and Storage[M].Geneva: WMO/UNDP, 2006, 3: 1-112; 5: 1-133.
[10]	Torpa T A, Gale J.Demonstrating storage of CO₂ in geological reservoirs: the Sleipner and SACS projects[J]. Energy, 2004, 29(9/10): 1361-1369.
[11]	Moritis G.CO₂ sequestration adds new dimension to oil, gas production[J]. Oil and Gas Journal, 2003, 101(9): 71-83.
[12]	曲建升,曾静静. 二氧化碳捕获与封存:技术、实践与法律——国际推广二氧化碳捕获与封存工作的法律问题分析[J]. 世界科技研究与发展,2007,29(6):78-83.[Qu Jiansheng, Zeng Jingjing. Carbon dioxide capture and storage: technology, demonstration, and legal aspects——an analysis on the legal related issues of international CCS efforts[J]. World Sci-tech R & D, 2007, 29(6): 78-83.]
[13]	郑晓鹏. 海上天然气田伴生CO₂的海上捕集及回注技术[J]. 中国造船,2007,48(增刊):297-302.[Zheng Xiaopeng. Study on offshore associated CO₂ capture and injection technology[J]. Shipbuilding of China, 2007, 48(Suppl.): 297-302.]
[14]	张鸿翔,李小春,魏宁. 二氧化碳捕获与封存的主要技术环节与问题分析[J]. 地球科学进展,2010,25(3):335-340.[Zhang Hongxiang, Li Xiaochun, Wei Ning. The major technology track and analysis about carbon dioxide capture and storage[J]. Advances in Earth Science, 2010, 25(3): 335-340.]
[15]	张卫东,张栋,田克忠. 碳捕集与封存技术的现状与未来[J]. 中外能源,2009,14(11):7-14.[Zhang Weidong, Zhang Dong, Tian Kezhong. Carbon capture and sequestration technology[J]. Sino-Global Energy, 2009, 14(11): 7-14.]
[16]	Roser B P, Korsch R J. Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data[J]. Chemical Geology, 1988, 67(1/2): 119-139.
[17]	董林森,刘立,曲希玉,等. CO₂矿物捕获能力的研究进展[J]. 地球科学进展,2010,25(9):941-949.[Dong Linsen, Liu Li, Qu Xiyu, et al. Research progress of ability of mineral trapping of CO₂[J]. Advances in Earth Science, 2010, 25(9): 941-949.]
[18]	Pettijohn F J. Sedimentary Rocks[M]. New York: Harper & Row, 1957: 224-242.
[19]	Bock B, McLennan S M, Hanson G N.Geochemistry and provenance of the Middle Ordovician Austin Glen Member (Normanskill Formation) and the Taconian Orogeny in New England[J]. Sedimentology, 1998, 45(4): 635-655.
[20]	Haskin L A, Haskin M A, Frey F A, et al. Relative and absolute terrestrial abundances of the rare earths[M]// Ahrens L H. Origin and Distribution of the Elements. Oxford: Pergamon, 1968: 889-911.
[21]	王清晨,从柏林. 大别山超高压变质岩的地球动力学意义[J]. 中国科学(D辑):地球科学,1996,26(3):271-276.[Wang Qingchen, Cong Bolin. Geodynamic significance of ultrahigh pressure metamorphic rocks of Dabie Mountain[J]. Science China (Seri. D):Earth Sciences, 1996, 26(3): 271-276.]
[22]	赵振华. 微量元素地球化学原理[M]. 北京:科学出版社,1997: 199-204.[Zhao Zhenhua. Principle of Trace Element Geochemistry[M]. Beijing: Science Press, 1997: 199-204.]
[23]	张英利,王宗起,闫臻,等. 库鲁克塔格地区新元古代贝义西组的构造环境:来自碎屑岩地球化学的证据[J]. 岩石学报,2011,27(6):1785-1796.[Zhang Yingli, Wang Zongqi, Yan Zhen, et al. Tectonic setting of Neoproterozoic Beiyixi Formation in Quruqtagh area, Xinjiang: Evidence from geochemistry of clastic rocks[J]. Acta Petrologica Sinica, 2011, 27(6): 1785-1796.]
[24]	毛光周,刘池洋. 地球化学在物源及沉积背景分析中的应用[J]. 地球科学与环境学报,2011,33(4):337-348.[Mao Guangzhou, Liu Chiyang. Application of geochemistry in provenance and depositional setting analysis[J]. Journal of Earth Sciences and Environment, 2011, 33(4): 337-348.]
[25]	童胜琪,刘志飞, Phon Le K,等. 红河盆地的化学风化作用:主要和微量元素地球化学记录[J]. 矿物岩石地球化学通报,2006,25(3):219-225.[Tong Shengqi, Liu Zhifei, Phon Le K, et al. Chemical weathering in the Red River Basin: records of major and trace elemental geochemistry[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2006, 25(3): 219-225.]
[26]	张鑫,张金亮. 东营凹陷南坡沙河街组四段砂岩地球化学特征[J]. 地质科学,2007,42(2):303-318.[Zhang Xin, Zhang Jinliang. Sedimento-geochemical features of sandstones from the fourth member, Shahejie Formation in the southern slope of Dongying sag [J]. Chinese Journal of Geology, 2007, 42(2): 303-318.]
[27]	Bachu S. Sequestration of CO₂ in geological media: criteria and approach for site selection in response to climate change[J]. Energy Conversion and Management, 2000, 41(9): 953-970.
[28]	高玉巧,刘立,曲希玉. CO₂与砂岩相互作用机理与形成的自生矿物组合[J]. 新疆石油地质,2007,28(5):579-584.[Gao Yuqiao, Liu Li, Qu Xiyu. Mechanism of CO₂-sandstone interaction and authigenic mineral assemblage[J]. Xinjiang Petroleum Geology, 2007, 28(5): 579-584.]
[29]	Berg A, Banwart S A.Carbon dioxide mediated dissolution of Ca-feldspar: implications for silicate weathering[J]. Chemical Geology, 2000, 163(1/2/3/4): 25-42.
[30]	Xu Tianfu, Apps J A, Pruess K. Mineral sequestration of carbon dioxide in a sandstone–shale system[J]. Chemical Geology, 2005, 217(3/4): 295-318.
[31]	Gunter W D, Perkins E H, McCann T J.Aquifer disposal of CO₂-rich gases: Reaction design for added capacity[J]. Energy Conversion and Management, 1993, 34(9/10/11): 941-948.
[32]	黄可可,黄思静,佟宏鹏,等. 长石溶解过程的热力学计算及其在碎屑岩储层研究中的意义[J]. 地质通报,2009,28(4):474-482.[Huang Keke, Huang Sijing, Tong Hongpeng, et al. The thermodynamic calculations of feldspar dissolution and significance of the study of clastic reservoirs[J]. Geological Bulletin of China, 2009, 28(4): 474-482.]
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Carbon Sequestration Potential of Yanchang Formation Sandstone of JX Well, Ordos Basin

doi: 10.14027/j.cnki.cjxb.2015.01.021

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通讯作者: 陈斌, bchen63@163.com

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