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1.西北大学 榆林碳中和学院,陕西 西安 710069
2.西北大学 地质学系/二氧化碳捕集与封存技术国家地方联合工程研究中心,陕西 西安 710069
3.陕西省碳中和技术重点实验室,陕西 西安 710069
4.西北大学 城市与环境学院,陕西 西安 710127
5.中国石油集团测井有限公司,陕西 西安 710077
丁钊,男,从事咸水层CO2地质封存选址研究,2437743050@qq.com。
王浩璠,女,工程师,博士,从事CO2地质封存选址及安全性监测,wanghf@nwu.edu.cn。
收稿:2024-06-10,
纸质出版:2025-10-25
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丁钊, 王浩璠, 马劲风, 等. 榆神地区长10-3亚段咸水层CO2地质封存潜力评价及靶区优选[J]. 西北大学学报(自然科学版), 2025,55(5):1049-1064.
DING Zhao, WANG Haofan, MA Jinfeng, et al. Evaluation of CO2 geological sequestration potential and target optimization of the saline aquifer in the Chang 10-3 sub-member of YuShen area[J]. Journal of northwest university (natural science edition), 2025, 55(5): 1049-1064.
丁钊, 王浩璠, 马劲风, 等. 榆神地区长10-3亚段咸水层CO2地质封存潜力评价及靶区优选[J]. 西北大学学报(自然科学版), 2025,55(5):1049-1064. DOI: 10.16152/j.cnki.xdxbzr.2025-05-009.
DING Zhao, WANG Haofan, MA Jinfeng, et al. Evaluation of CO2 geological sequestration potential and target optimization of the saline aquifer in the Chang 10-3 sub-member of YuShen area[J]. Journal of northwest university (natural science edition), 2025, 55(5): 1049-1064. DOI: 10.16152/j.cnki.xdxbzr.2025-05-009.
评估CO
2
地质封存潜力以及选择优势靶区是咸水层CO
2
地质封存的关键,当前CO
2
地质封存潜力评价方法复杂、参数获取难度大且选址方法多样、选址指标尚不统一。利用钻井、测井、录井、完井等资料对榆林神木(以下简称榆神)地区二叠系上统石千峰组至三叠系上统延长组地层开展地层划分与对比、岩性、物性解释等工作,识别出榆神地区最适合CO
2
地质封存的咸水层,即上三叠统延长组长10
-
3亚段咸水层。根据地下咸水层展布特征,利用容积法完成该层封存潜力评价,结合榆神地区地面环境状况,实现地下+地面综合选址并提出影响选址的7个重要评价指标。最后基于靶区优选区块,开展了层次分析法和模糊综合评价法的靶区评价及排序。研究表明:长10
-
3亚段平均孔隙度9.40%、渗透率1.09 mD、咸水层平均厚度37 m,封存潜力约5.14×10
8
t,所圈定的区块A4是最适合CO
2
地质封
存的优质靶区,具备优先开展CCS项目的条件,可为周边高碳排放企业就近实施CCS项目提供选址及潜力评价的指导。
Assessing the potential of CO
2
geological storage and selecting advantageous targets are the key to the geological storage of CO
2
in saline aquifers. At present
the evaluation methods of CO
2
geological storage potential are complex
the parameters are difficult to obtain
the site selection methods are diverse
and the site selection indicators are not uniform. In this paper
the stratigraphic division and correlation
lithology and physical property interpretation of the Upper Permian ShiQianFeng formation to the Upper Triassic YanChang formation in YuLin-ShenMu area (Hereinafter referred to as “YuShen” area) have been carried out by using drilling
logging and well completion data
the Saline aquifer of Chang 10
-
3 sub-member of YanChang formation of Upper Triassic is the most suitable for CO
2
geological storage in YuShen area. According to the distribution characteristics of underground Saline aquifer
the storage potential of it is evaluated by using the volumetric method
combined with the surface environment conditions of YuShen area
the paper realizes the comprehensive site selection of underground + ground and puts forward 7 important evaluation indexes that affect the site selection. Finally
based on the target optimization block
the evaluation and ranking of target area are carried out by AHP + Fuzzy mathematics comprehensive evaluation method. The results show that the average porosity of the Chang 10
-
3 sub-member is 9.40%
the permeability is 1.09mD
the average thickness of the saline aquifer is 37m
and the storage potential is about 5.14×10
8
t. The delineated block A4 is the most suitable high-quality target area for CO
2
geological storage
which has the conditions to give priority to CCS projects
and can provide guidance for site selection and potential evaluation for surrounding
high-carbon emission enterprises to implement CCS projects nearby.
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