低孔低渗咸水层CO2封存选址评价体系—以鄂尔多斯盆地为例

Evaluation system of CO2 geological storage site in low porosity and low permeability saline aquifers—A case study of Ordos Basin

  • 摘要: 【目的】 深部咸水层作为地下空间资源来实施CO2注入与地质封存项目,是实现温室气体减排和碳中和目标的一项重要手段。CO2咸水层地质封存选址及潜力评价多为较宏观的盆地级、区域级,选址评价体系尚未考虑低孔低渗地层的适宜性。【方法】 基于鄂尔多斯盆地榆神地区192口测井资料,开展非油气层段地层划分与对比、岩性和物性解释并识别咸水层,在标定的优势咸水层地层特征、盖层封闭性、封存潜力、地表环境等研究基础上,提出并分级量化了考虑低孔低渗储层发育特征的CO2咸水层地质封存选址评价指标。【结果和结论】 所提出的一级评价指标为地质封存条件、封存能力条件和社会环境条件,分别表征咸水层可注入性、可封存性、地表可行性的,其中地质封存条件包括储层岩性、储层厚度、孔隙度、渗透率等二级评价指标,封存能力条件包括盖层封闭性、埋深、封存潜力、断裂等二级评价指标,社会环境条件包括地下资源开发现状、土地利用现状、塌陷及灾害区、源汇匹配、公众接受度等二级评价指标。建立的基于鄂尔多斯盆地低孔低渗砂岩储层现状的靶区级、场地级CCS项目选址评价体系,将为进一步确定CO2咸水层地质封存工业化项目的落地和实施提供依据和指导。

     

    Abstract: 【Objective】 As an underground space resource, the deep saline formation is an important site to implement CO2 injection and geological storage, which is a necessary means to achieve the goal of greenhouse gas emission reduction and carbon neutrality. The site selection and potential evaluation of CO2 aquifer reservoir geological storage are mostly at the macro basin level and regional level, and the site selection evaluation system has not considered the suitability of low porosity and low permeability strata. 【Method】 Based on the well logging data of 192 Wells in Yusheng area, Ordos Basin, this paper carries out the formation division and correlation, lithology and physical property interpretation of non-oil and gas reservoirs and identifies the aquifer reservoirs. Then, based on the study of the formation characteristics, seal property, sealing potential and surface environment, an evaluation index for the location of geological storage of deep saline CO2 reservoirs considering the development characteristics of low porosity and low permeability reservoirs is proposed and quantified.【 Result and Conslusion】 The proposed first-level evaluation indexes are geological storage conditions, storage capacity conditions and social environmental conditions, which represent the injectivity, storage ability and surface feasibility respectively. The geological storage conditions include the second-level evaluation indexes such as reservoir lithology, reservoir thickness, porosity and permeability. The conditions of storage capacity include second-level evaluation indicators such as closure of cap layer, buried depth, storage potential, fracture, etc., while the social environment conditions include second-level evaluation indicators such as the status of underground resource development, land use status, collapse and disaster area, source-sink matching, and public acceptance. The established site selection evaluation system for target and site level CCS projects based on the current situation of low porosity and low permeability sandstone reservoirs in Ordos Basin will provide guidance for constructing the industrial CO2 aquifer geological storage projects.

     

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