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    松辽盆地南部保康体系上白垩统CO2埋存条件与潜力

    金超 曾荣树 田兴有

    金超, 曾荣树, 田兴有, 2013. 松辽盆地南部保康体系上白垩统CO2埋存条件与潜力. 地球科学, 38(6): 1229-1239. doi: 10.3799/dqkx.2013.120
    引用本文: 金超, 曾荣树, 田兴有, 2013. 松辽盆地南部保康体系上白垩统CO2埋存条件与潜力. 地球科学, 38(6): 1229-1239. doi: 10.3799/dqkx.2013.120
    JIN Chao, ZENG Rong-shu, TIAN Xing-you, 2013. CO2 Storage Conditions and Capacity of Upper Cretaceous Series in Baokang Sedimentary System in the Southwest of Songliao Basin. Earth Science, 38(6): 1229-1239. doi: 10.3799/dqkx.2013.120
    Citation: JIN Chao, ZENG Rong-shu, TIAN Xing-you, 2013. CO2 Storage Conditions and Capacity of Upper Cretaceous Series in Baokang Sedimentary System in the Southwest of Songliao Basin. Earth Science, 38(6): 1229-1239. doi: 10.3799/dqkx.2013.120

    松辽盆地南部保康体系上白垩统CO2埋存条件与潜力

    doi: 10.3799/dqkx.2013.120
    基金项目: 

    国家重点基础研究发展计划"973"项目 2011CB707303

    详细信息
      作者简介:

      金超(1983-), 女, 博士研究生, 从事沉积地质学与CO2地下埋存方面的研究.E-mail: baobei181920@126.com

    • 中图分类号: P535

    CO2 Storage Conditions and Capacity of Upper Cretaceous Series in Baokang Sedimentary System in the Southwest of Songliao Basin

    • 摘要: CO2地下埋存是一项缓解全球气候变暖的措施.采用沉积地质学的研究方法, 首次对松辽盆地南部长岭凹陷的保康沉积体系沿水流方向进行连井剖面分析, 结合室内显微镜薄片鉴定和岩心观察等手段, 对保康体系的沉积相类型及其时空分布规律、储盖层沉积特征、水文地质及构造特征等进行了研究.结果表明, 研究区青山口组-嫩江组是CO2地下埋存的良好储盖组合, 同时计算研究区CO2埋存量为7.43×109 t, 大约相当于2002年中国CO2排放量的2倍、2009年中国的全年排放量.

       

    • 图  1  研究区构造位置(据王永春修改,2007)

      Fig.  1.  The tectonic location of the study area

      图  2  连井剖面线位置及研究区部分井位

      Fig.  2.  The location of partial wells and the section lines in the study area

      图  3  以青一段最大湖泛面为基准沿保康体系水流方向的连井剖面图

      Fig.  3.  The connected-well's profile along the flow direction of Baokang system from Qingshankou to Nenjiang Formation

      图  4  研究区储层砂岩类型(据路风香和桑隆康,2000)

      Q.石英;F.长石;R.岩屑;1.石英砂岩;2.长石石英砂岩;3.岩屑石英砂岩;4. 长石砂岩;5.岩屑长石砂岩;6.长石岩屑砂岩;7.岩屑砂岩

      Fig.  4.  The reservoirs' sandstone types in the study area

      图  5  青山口组储层有效孔隙度与渗透率关系

      a.青一段储层孔渗关系;b.青二、三段储层孔渗关系

      Fig.  5.  The relationship of porosity to permeability in sandstone reservoir of Qingshankou Formation

      图  6  研究区内部分井位储层地下水矿化度分布

      Fig.  6.  The groundwater salinity distribution of partial wells in the study area

      图  7  松辽盆地南部568测线地质剖面(据王永春修改,2007)

      Fig.  7.  The geologic section of 568 survey line in South Songliao basin

      表  1  研究区盖层各岩性厚度及所占比例

      Table  1.   The thickness and ratio of each kind of lithology of the cap rock in the study area

      最小厚度(m) 最大厚度(m) 平均厚度(m) 最小比例(%) 最大比例(%) 平均比例(%)
      块状泥岩 214.5 442.5 318.21 46.910 96.970 89.580
      粉砂质泥岩 4.0 138.0 28.50 1.154 34.620 7.382
      油页岩 0 15.0 7.28 0 4.975 2.036
      泥页岩 0 132.5 40.90 0 27.749 1.000
      下载: 导出CSV

      表  2  研究区各阶段构造运动、断裂及应力场性质

      Table  2.   Tectonic movement, fracture property and the variation of stress field in every stage in the study area

      盆地变化 构造运动 断裂性质 应力场变化
      收缩阶段 燕山运动Ⅳ幕、Ⅴ幕影响,其后受喜山运动控制 两次总体抬升,形成大量褶皱,断裂由正转逆 拉张性转为挤压性
      坳陷阶段 盆地整体下降统一沉积 基底断裂活动减弱,断层不再向上延伸 热沉降
      断陷阶段 燕山运动Ⅱ幕、Ⅲ幕 大规模正断裂活动伴随火山喷发 拉张性
      隆起阶段 华力西运动 北东向或北北东向正断裂为主 拉张性
      下载: 导出CSV

      表  3  研究区青山口组计算参数及埋存量

      Table  3.   Capacity calculating parameters of target reservoirs in the study area

      青一段 青二段 青三段 姚一段
      保康砂体面积(km2) 10 000 20 000 15 000 10 000
      砂体平均厚度(km) 0.043 0.049 0.100 0.008
      平均体积(km3) 430 980 1 500 80
      平均有效孔隙度(%) 14.12 18.66 18.66 9.20
      有效埋存量(t) 0.85×109 2.56×109 3.92×109 0.10×109
      总埋存量(t) 7.43×109
      下载: 导出CSV
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