Sweet spot selection in CO2 saline aquifers geological storage, Yulin-Shenmu Area
- Journal of Northwest University (Natural Science Edition) Vol. 53, Issue 6, Pages: 900-912(2023)
- 作者机构：
1.西北大学 地质学系/榆林碳中和学院/二氧化碳捕集与封存国家地方联合工程研究中心/陕西省碳中和技术重点实验室，陕西 西安 710069
2.延安大学 石油工程与环境工程学院，陕西 延安 716000
- 作者简介：
- 基金信息：
DOI：10.16152/j.cnki.xdxbzr.2023-06-003
CLC：
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ZHANG Xiaoli, LI Yajun, FENG Chun, et al. Sweet spot selection in CO2 saline aquifers geological storage, Yulin-Shenmu Area. [J]. Journal of Northwest University (Natural Science Edition) 53(6):900-912(2023)
ZHANG Xiaoli, LI Yajun, FENG Chun, et al. Sweet spot selection in CO2 saline aquifers geological storage, Yulin-Shenmu Area. [J]. Journal of Northwest University (Natural Science Edition) 53(6):900-912(2023) DOI： 10.16152/j.cnki.xdxbzr.2023-06-003.
摘要
融合区域重力、磁法、电法、遥感、地震资料和测井资料，分析地层构造特征及可能存在的断裂；对远离断层的区域，基于钻井、录井、测井资料综合分析，通过精细岩性识别、储层物性、盖层特征分析，厘清钻井中优质储层、盖层组合特征及展布；结合CO,2,可注入性实验模拟结果，形成CO,2,咸水层封存甜点优选技术序列，从而达到优选CO,2,咸水层封存潜力甜点的目的。研究表明，榆林和神木地区的纸坊组3段、神木及其附近的石千峰组千5段、榆林北部和西北部的延长组长10底部的砂体发育，物性较好，优质储层发育，储盖组合优，远离断层，砂体埋藏深度分别为750~1 500 m，1 500~2 100 m，850~1 350 m。研究后认为，纸3段、千5段优质储层发育区为CO,2,咸水层封存甜点分布有利潜力区，榆林北部和西北部的长10底部优质储层发育区为CO,2,咸水层封存甜点潜力接替区；和尚沟组、刘家沟组砂体相对不发育，主要为泥质地层，起到良好区域封盖作用。
Abstract
Comprehensive analysis of the structural characteristics and the possible faults by integrating gravity, magnetic, electrical, and remote sensing data; for areas far away from faults, based on comprehensive analysis of drilling and logging data, fine lithology identification, reservoir physical properties and cap rock characteristics is used to clarify the characteristics of high quality reservoirs-cap rock combinations and spatial distribution; based on the simulation results of CO,2, injectability experiments, a sequence of optimization techniques about the site selection for the CO,2, geological storage of sweet spots is formed.Thus, the goal to optimize the site for CO,2, geological storage of sweet spots in the saline aquifers is achieved. Research shows, the third member of the Zhifang Formation, the 5th member of the Shiqianfeng Formation in the area of Shenmu and the Chang 10 Member of Yangchang Formation in the northern and northwestern regions of Yulin have well-developed sand bodies with good physical properties, excellent caprock and lateral shielding conditions, far away from the faults, with burial depth of 750~1 500 m, 1 500~2 100 m, and 850~1 350 m. Research suggests that the development area of high-quality reservoirs in the third member of the Zhifang Formation and the 5th member of the Shiqianfeng Formation are the favorable potential sweet spot distribution areas for the CO,2, geological storage in the saline aquifers, and the development area of high-quality reservoirs at the bottom of Chang10 in the northern and northwestern regions of Yulin is a potential replacement sweet spot distribution area for the CO,2, geological storage in the saline aquifers; in the study area, the sand bodies of the Heshanggou Formation and Liujiagou Formation are relatively underdeveloped and mainly composed of mud strata, which play a good sealing role.
关键词
咸水层二氧化碳地质封存测井储盖组合甜点选址
Keywords
saline aquifersCO2 geological storagewell logreservoir-caprock assemblagesweet spotsite selection
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