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松辽盆地南部大情字井区青山口组地热水化学特征及成因模式

杜先利 王泓博 赵容生 季辉 朱焕来 代登亮 王颖 李迎九 肖红平

杜先利, 王泓博, 赵容生, 季辉, 朱焕来, 代登亮, 王颖, 李迎九, 肖红平. 松辽盆地南部大情字井区青山口组地热水化学特征及成因模式[J]. 地质科技通报, 2024, 43(3): 22-35. doi: 10.19509/j.cnki.dzkq.tb20230605
引用本文: 杜先利, 王泓博, 赵容生, 季辉, 朱焕来, 代登亮, 王颖, 李迎九, 肖红平. 松辽盆地南部大情字井区青山口组地热水化学特征及成因模式[J]. 地质科技通报, 2024, 43(3): 22-35. doi: 10.19509/j.cnki.dzkq.tb20230605
DU Xianli, WANG Hongbo, ZHAO Rongsheng, JI Hui, ZHU Huanlai, DAI Dengliang, WANG Ying, LI Yingjiu, XIAO Hongping. Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 22-35. doi: 10.19509/j.cnki.dzkq.tb20230605
Citation: DU Xianli, WANG Hongbo, ZHAO Rongsheng, JI Hui, ZHU Huanlai, DAI Dengliang, WANG Ying, LI Yingjiu, XIAO Hongping. Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 22-35. doi: 10.19509/j.cnki.dzkq.tb20230605

松辽盆地南部大情字井区青山口组地热水化学特征及成因模式

doi: 10.19509/j.cnki.dzkq.tb20230605
基金项目: 

中国石油天然气股份有限公司科技项目"松辽盆地低孔低渗地热利用目标优选及关键技术研究" kt2021-20-01

详细信息
    作者简介:

    杜先利, E-mail: duxl@nepu.edu.cn

    通讯作者:

    赵容生, E-mail: zhaors@jlu.edu.cn

  • 中图分类号: P314.2;TK521

Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin

More Information
  • 摘要:

    位于长岭凹陷鞍部的大情字井地区水热型地热资源丰富, 其中储层温度较高、岩性好、含水量高的青山口组是最佳热储层, 因此, 阐明地热水的成因模式对于该区地热资源的可持续开发利用具有重要意义。通过青山口组7口井地热水样的水化学测试, 结合收集的8组氢氧同位素数据, 研究了目标区地热水的来源及混合过程, 并分析了成因模式。结果表明, 青山口组地热水主要为部分平衡的Cl-Na型流体, 补给来源为长白山地区的大气降水和原生沉积水, 补给高程为2 347~2 370 m; 通过2 210~3 470 m的循环吸热过程形成现今温度为81.25~112.80 ℃的地热流体存储于半开放体系的青山口组碎屑岩储层中。另外, 研究区NE、NW向2组断裂系统是地热流体循环的主要导水通道, 地热流体在深循环过程中与围岩矿物发生水岩反应, 碳酸盐岩及硅酸盐矿物的溶解, 形成了以Na+、Cl-和HCO3-离子为主的地热水资源。

     

  • 图 1  松辽盆地位置图(a)和大情字井地区构造图(b) (据文献[36]修改)

    Figure 1.  Location of the Songliao Basin (a) and tectonic map of the Daqingzijing area (b)

    图 2  松辽盆地构造演化图(据文献[37]修改)

    Q.第四系; E+N.古近系+新近系; K2.上白垩统; K1.下白垩统; J3.侏罗系; T.三叠系

    Figure 2.  Tectonic evolution map of the Songliao Basin

    图 3  大情字井地区断裂构造纲要图(据文献[41]修改)

    a.T1反射层(相当于嫩江组底界);b.T2反射层(相当于青山口组底界)

    Figure 3.  Outline of the fault structure in the Daqingzijing area

    图 4  研究区地热水Piper三线图

    Figure 4.  Three-line diagram of geothermal water Piper in the study area

    图 5  研究区地热水Gibbs图

    Figure 5.  Gibbs diagram of geothermal water in the study area

    图 6  研究区地热水主要元素摩尔浓度关系

    Figure 6.  Relationship between the main elements of geothermal water in the study area

    图 7  大情字井地热水样δD-δ18O关系

    Figure 7.  δD-δ18O relationship of geothermal water sampling in Daqingzijing area

    图 8  地热水中温度与SiO2质量浓度的关系

    Figure 8.  Relationship between temperature and SiO2 concentration in geothermal water

    图 9  地热水Na-K-Mg平衡三角图

    Figure 9.  Na-K-Mg equilibrium triangle diagram of geothermal water

    图 10  冷水混合比例与地热水温度关系图

    Figure 10.  Relationship between cold water mixing ratio and geothermal water temperature

    图 11  长岭凹陷地热水资源成因模式图(据文献[60]修改)

    Figure 11.  Genetic model of geothermal water resources in the Changling Sag

    表  1  研究区水样测试数据

    Table  1.   Analysis results of geothermal water sampling in the study area

    水样编号 深度/ m TDS K+ Na+ Ca+ Mg2+ Cl- SO42- HCO3- I- Br- B3+ SiO2
    ρB/(mg·L-1)
    S1 1 484.1 14 178.9 42.4 5 303.5 41.7 19.0 7 801.1 43.7 927.5 3.2 9 3.7 30.0
    S2 1 847.6 14 129.2 46.8 5 344.8 20.0 12.2 6 579.2 132.1 1 994.1 4.7 9 6.4 57.6
    S3 2 030.5 9 763.4 98.9 3 348.0 31.3 43.0 3 658.4 144.1 1 439.7 2.9 1 2 53.5
    S4 2 302.4 16 395.1 58.8 6 027.6 91.8 17.0 8 644.1 312.2 1 243.6 3.8 9 5.8 58.9
    S5 2 240.4 19 697.8 59.6 7 081.6 110.2 13.4 8 804.7 118.1 1 510.2 4.2 7 10.7 59.5
    S6 2 409.5 9 426.5 49.2 3 363.9 36.3 6.9 4 200.8 754.6 1 014.8 6.5 3 12.2 63.0
    S7 2 489.8 13 846.0 82.1 4 970.0 52.7 16.3 6 490.5 905.4 1 329.0 3.2 7 13.4 63.2
    水样编号 深度/m T/℃ pH值 变质系数(γNa+/γCl-) 盐化系数Cl-/(HCO3-+CO32-) 氯镁系数(γCl-/γMg2+) 脱硫系数(100×γSO42-/γCl-)
    S1 1 484.1 64.0 7.5 1.04 8.41 140.77 0.41
    S2 1 847.6 81.4 9.0 1.25 3.29 184.89 1.46
    S3 2 030.5 87.4 9.0 1.43 2.54 29.17 22.81
    S4 2 302.4 93.0 7.0 1.07 6.95 174.33 2.63
    S5 2 240.4 94.0 7.0 1.23 5.83 225.28 17.54
    S6 2 409.5 97.8 7.0 1.24 4.14 208.74 13.09
    S7 2 489.8 100.0 7.0 1.28 4.88 236.52 10.17
    注:储层岩性为粉砂岩
    下载: 导出CSV

    表  2  水样的同位素测试结果

    Table  2.   Isotopic results of water samples

    编号 水样类型 δD/‰ δ18O/‰ 资料来源
    D1 大气降水 -75.13 -10.34 文献[53]
    D2 水库水 -59.00 -7.20 文献[54]
    D3 江水 -63.30 -8.20 文献[54]
    D5 浅层地下水 -71.70 -9.90 文献[55]
    D6 浅层地下水 -78.50 -10.40 文献[55]
    D7 地热水 -98.10 -11.30 文献[56]
    D8 地热水 -97.40 -12.20 文献[56]
    下载: 导出CSV

    表  3  研究区地热水补给高程

    Table  3.   Geothermal water supply elevation in the study area

    水样编号 采样高程/m 样品δD/‰ 大气降水δD/‰ K/(‰ (100 m)-1) 补给高程/m
    D7 1 667 -98.10 -63.30 -4.95 2 370
    D8 1 657 -97.40 -63.30 -4.95 2 347
    下载: 导出CSV

    表  4  地热水热储温度

    Table  4.   Thermal storage temperature of geothermal water

    水样编号 ρ(SiO2)/ (mg·L-1) 热储温度/℃
    石英(无蒸汽损失)地温计 石英(有蒸汽损失)地温计 SiO2计算/℃ K-Mg温标/℃
    S1 30.00 79.40 83.10 81.25 94.80
    S2 57.57 108.60 108.40 108.50 103.56
    S3 53.50 105.00 105.40 105.20 106.90
    S4 58.93 109.70 109.40 109.55 105.31
    S5 59.53 110.20 109.80 110.00 109.09
    S6 63.00 112.90 112.20 112.55 113.18
    S7 63.23 113.20 112.40 112.80 115.61
    下载: 导出CSV

    表  5  地热水循环深度调查

    Table  5.   Investigated geothermal water circulation depth

    水样编号 地热增温级/ (m·℃-1) SiO2热储温度/℃ 年平均气温/℃ 恒温带深度[38]/m 循环深度/m
    S1 29.41 81.25 4.5 25 2 282
    S2 21.14 108.50 4.5 25 2 222
    S3 25.71 105.20 4.5 25 2 612
    S4 23.81 111.50 4.5 25 2 572
    S5 24.10 110.00 4.5 25 2 572
    S6 31.95 112.55 4.5 25 3 482
    S7 27.47 112.80 4.5 25 3 002
    下载: 导出CSV
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  • 收稿日期:  2023-10-30
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