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太原盆地岩溶地热系统的形成演化及其地热资源潜力

汪新伟, 王婷灏, 李海泉, 张瑄, 罗璐, 刘慧盈, 王嗣敏, 向才富. 2022. 太原盆地岩溶地热系统的形成演化及其地热资源潜力[J]. 中国地质, 49(3): 716-731. doi: 10.12029/gc20220304
引用本文: 汪新伟, 王婷灏, 李海泉, 张瑄, 罗璐, 刘慧盈, 王嗣敏, 向才富. 2022. 太原盆地岩溶地热系统的形成演化及其地热资源潜力[J]. 中国地质, 49(3): 716-731. doi: 10.12029/gc20220304
WANG Xinwei, WANG Tinghao, LI Haiquan, ZHANG Xuan, LUO Lu, LIU Huiying, WANG Simin, XIANG Caifu. 2022. Evolution of karst geothermal system and its geothermal resource potential in Taiyuan Basin[J]. Geology in China, 49(3): 716-731. doi: 10.12029/gc20220304
Citation: WANG Xinwei, WANG Tinghao, LI Haiquan, ZHANG Xuan, LUO Lu, LIU Huiying, WANG Simin, XIANG Caifu. 2022. Evolution of karst geothermal system and its geothermal resource potential in Taiyuan Basin[J]. Geology in China, 49(3): 716-731. doi: 10.12029/gc20220304

太原盆地岩溶地热系统的形成演化及其地热资源潜力

  • 基金项目:
    中国石油化工股份有限公司科技项目(JP15002、JKL18033)资助
详细信息
    作者简介: 汪新伟, 男, 1968年生, 博士, 研究员, 现主要从事地热资源勘查研究; E-mail: wangxinwei.xxsy@sinopec.com
  • 中图分类号: P314

Evolution of karst geothermal system and its geothermal resource potential in Taiyuan Basin

  • Fund Project: Supported by sinopec science and technology project"Geothermal resources potential and target evaluation of Ordovician limestone in Taiyuan Area"(No.JP15002, No.JKL18033)
More Information
    Author Bio: WANG Xinwei, male, born in 1968, doctor, researcher, mainly engaged in basin structure and geothermal resources exploration; E-mail: wangxinwei.xxsy@sinopec.com .
  • 研究目的

    太原盆地作为优质岩溶热储分布与城市供暖需求匹配良好的地区之一,其岩溶地热系统的形成演化与成因要素的研究对本区地热资源的整体开发以及断陷盆地型地热资源展布规律的认识均具有重要的指导意义。

    研究方法

    本文在综合前人研究成果与最新54口地热井资料的基础上,分析了太原盆地岩溶地热系统的热源、热储展布和水热动力学特征,并分8个单元评价了地热资源量。

    研究结果

    结果表明,岩溶热储发育的层位主要为华北板块广泛分布的下古生界奥陶系,经历了早古生代末的表生岩溶、晚古生代的直接盖层沉积、中生代岩溶地热系统初始形成、新近纪的改造与第四纪最终定型等5个阶段。该地热系统的热源来自于新生代裂谷盆地产生的高大地热流(最高达79.12 mW/m2),热传递方式可分为强烈对流型(盆地边缘)和热传导型(盆地内部)截然不同的两类。热储储集性能具纵向分层、平面分带特征。在纵向上识别出15~20层有效储集段,累计厚度160~180 m,可划分为3~4层主力含水段;在平面上有利储集带主要受NE向隐伏构造的控制,且主力含水层在运移过程中易发生“越流”现象。盆地中段的奥陶系热储因埋藏适中(约400~1900 m)、且储层温度较高(30~75℃),是最有利的勘探开发区。依据热储体积法评价出太原盆地岩溶地热系统可利用的静态地热资源量为83.03×108 GJ,折合标煤2.83×108 t。

    结论

    年开采地热资源量可满足1502万m2的供暖面积。鉴于目前已开发资源仅占可开发的23.3%,开发潜力巨大。

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  • 图 1  太原盆地构造区划与岩溶水系统分区图

    Figure 1. 

    图 2  太原盆地及邻区构造—地层格架图

    Figure 2. 

    图 3  太原盆地岩溶地热系统演化示意图

    Figure 3. 

    图 4  太原盆地典型钻井深度—温度关系图

    Figure 4. 

    图 5  GX-2井测井曲线与产能测试对比

    Figure 5. 

    图 6  太原盆地西温庄地热田单井产水量等值线分布图

    Figure 6. 

    图 7  太原盆地奥陶系岩溶热储顶面埋深(a)与温度(b)分布图

    Figure 7. 

    图 8  太原盆地岩溶地热系统地热水运移模式图(剖面位置见图 1B—B’)

    Figure 8. 

    表 1  太原盆地GX-2井测井解释对应表

    Table 1.  Corresponding tables for log interpretation of GX-2 well in Taiyuan Basin

    下载: 导出CSV

    表 2  西温庄地热田地热井产液剖面测试结果统计

    Table 2.  Statistical table of liquid-producing profile test results of geothermal wells in Xiwenzhuang geothermal field

    下载: 导出CSV

    表 3  太原盆地奥陶系岩溶热储地热资源评价参数取值与计算结果

    Table 3.  Summary of evaluation parameters and calculation results of geothermal resources for Ordovician in Taiyuan Basin

    下载: 导出CSV
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出版历程
收稿日期:  2019-12-24
修回日期:  2020-02-28
刊出日期:  2022-06-25

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