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基于兰州断陷盆地地热地质条件的石佛沟地热资源潜力评估

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陈秀清, 王涛, 黄晓辉, 王宝玉. 基于兰州断陷盆地地热地质条件的石佛沟地热资源潜力评估[J]. 水文地质工程地质, 2023, 50(6): 213-224. doi: 10.16030/j.cnki.issn.1000-3665.202306028
引用本文: 陈秀清, 王涛, 黄晓辉, 王宝玉. 基于兰州断陷盆地地热地质条件的石佛沟地热资源潜力评估[J]. 水文地质工程地质, 2023, 50(6): 213-224. doi: 10.16030/j.cnki.issn.1000-3665.202306028
shu
CHEN Xiuqing, WANG Tao, HUANG Xiaohui, WANG Baoyu. Evaluation of geothermal resource potential in Shifogou based on geothermal geological conditions of the Lanzhou faulted basin[J]. Hydrogeology & Engineering Geology, 2023, 50(6): 213-224. doi: 10.16030/j.cnki.issn.1000-3665.202306028
Citation: CHEN Xiuqing, WANG Tao, HUANG Xiaohui, WANG Baoyu. Evaluation of geothermal resource potential in Shifogou based on geothermal geological conditions of the Lanzhou faulted basin[J]. Hydrogeology & Engineering Geology, 2023, 50(6): 213-224. doi: 10.16030/j.cnki.issn.1000-3665.202306028
shu

基于兰州断陷盆地地热地质条件的石佛沟地热资源潜力评估

  • 1.

    兰州资源环境职业技术大学，甘肃 兰州　730000

  • 2.

    甘肃省有色工程勘察设计研究院，甘肃 兰州　730000

  • 3.

    甘肃智广地质工程勘察设计有限公司，甘肃 兰州　730000

  • 基金项目: 甘肃省教育厅产业支持计划项目（2021CYZC-01）
详细信息
    作者简介: 陈秀清（1969-），女，本科，正高级工程师，主要从事环境地质工程教学与科研工作。E-mail：494425273@qq.com

  • 中图分类号: P314

Evaluation of geothermal resource potential in Shifogou based on geothermal geological conditions of the Lanzhou faulted basin

  • 1.

    Lanzhou Resources & Environment Voc-Tech University, Lanzhou, Gansu　730000, China

  • 2.

    Gansu Nonferrous Engineering Survey, Design and Research Institute, Lanzhou, Gansu　730000, China

  • 3.

    Gansu Zhiguang Geological Engineering Survey & Design Co. Ltd., Lanzhou, Gansu　730000, China

    摘要

  • 针对兰州石佛沟景区地热地质条件勘探研究程度较低，严重制约当地地热资源开发利用这一问题，在充分搜集整理已有资料的基础上，总结了兰州断陷盆地地热地质条件和热储特征，结合可控源音频大地电磁测深法（CSAMT）探测结果，推断了盆地东部南段石佛沟的地热资源开发潜力。结果表明：（1）分别以深沟桥（F5）、雷坮河（F8）隐伏断裂为界，兰州断陷盆地地热地质条件具有明显差异性，可分为西部西固城区、中部七里河区、东部城关—石佛沟区；（2）平面上由西向东不同深度的热储温度呈增加趋势，垂向上2000～2500 m深度的地热增温率升高，可推断为兰州断陷盆地地热开采的基本深度；（3）东部南段的石佛沟景区潜存层状传导型地热和断裂带状地热资源，层状地下热水赋存于兰州断陷盆地南部边缘地段，断裂带状地下热水赋存于F2断裂破碎带或F2与F8断裂的交汇地段，据此推断在石佛沟景区可能存在层状和带状“复合型”地热水的富集地段。研究建议断裂带状热储层的地热水勘探开采井深度可按800～1100 m考虑，“复合型”层状热储层的勘探开采井深度可按1500～2000 m考虑；预测该地段地下热水井口出水温度可达50～60 °C，单井涌水量可达500～1000 m3/d，热水水质可达到医疗洗浴质量标准。结果可为当地地热资源勘探和开发利用提供依据。

    Aiming at the problem of low degree of exploration and research of geothermal geological conditions in the Shifugou area, which seriously restricts the development and utilization of geothermal resources, on the basis of available data, the geothermal geological conditions and the characteristics of the thermal reservoir in the Lanzhou faulted basin are summarized. Combined with the exploration results of the controlled source audio frequency magnetotelluric (CSAMT) method, the potential of geothermal resources development in the Shifogou area in the southern part of the basin is inferred. The results show that (1) the geothermal geological conditions in the Lanzhou faulted basin are obviously different. Taking the buried faults of Shengouqiao (F5) and Leitai River (F8) as the boundary, respectively, the faulted basin can be divided into the western Xigu district, central Qilihe district and eastern Chengguan-Shifogou district. (2) The geothermal temperature increases from west to east, and increases vertically from the depth of 2000 to 2500 m, inferring that this is the basic depth of geothermal exploitation in the Lanzhou faulted basin. (3) In the southern section of the eastern part may exist layered-conductive geothermal resources and fault-zone geothermal resources, it is inferred that there may exist “combined type” of layered and banded geothermal water in the Shifogou district, which is located in the F2 fracture zone or the intersection of F2 fracture zone and F8 fault zone. It is suggested that the exploration and production well depth of geothermal water in the faulted-zone thermal reservoir should be considered as 800−1100 m, and that the exploration and production well depth of the “combined” layered thermal reservoir should be considered as 1500−2000 m. The wellhead geothermal water temperature in this area is expected to reach 50−60 °C, the single well yield can reach 500−1000 m3/d, and the quality of the geothermal water can reach the standard for medical bathing. The results can provide a basis for geothermal resources exploration in Lanzhou.

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  • 图 1  兰州断陷盆地地热地质图（修编自文献[25 − 26]）

    Figure 1. 

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    图 2  兰州断陷盆地地热地质剖面图（修编自文献[25 − 26]）

    Figure 2. 

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    图 3  兰州断陷盆地地热盖层和热储厚度图（修编自文献[25 − 26]）

    Figure 3. 

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    图 4  兰州断陷盆地地热水文地质平面图（修编自文献[25 − 26]）

    Figure 4. 

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    图 5  兰州断陷盆地不同深度地温场图（修编自文献 [25 − 26]）

    Figure 5. 

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    图 6  二维反演视电阻率等值色阶及推断解释断面图

    Figure 6. 

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    图 7  CSAMT代表点82、160的测深曲线

    Figure 7. 

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    图 8  石佛沟地段CSAMT物探推断地热综合成果图

    Figure 8. 

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    表 1  盆地地热井揭示的地层结构

    Table 1.  Basin stratigraphic structure revealed by drilled holes

    分区 编号 孔深/m 地层厚度（层底深度）/m
    Q N E K AnЄGl.
    西部 DR1 2500.3 10.0 270.0（280） 1335.0（2090） >410.3（>2500）
    SGDR 2508.3 235.0 510.0（745） 1763.3（2508）
    RSDR 2330.0 278.0 511.0（789） 1532.0（2321） >9.0（>2330）
    中部 K1 2502.0 386.0 486.0（872） 1504.0（2376） >126.0（>2502）
    DR2 3000.5 812.5 610.5（1423） 1006.0（2429） >571.5（3000）
    YTDR 2003.0 237.0 600.0（837） 890.0（1727） >276.0（>2 003）
    东部 DR3 2000.2 22.5 65.0（87.5） 964.5（1052） >948.2（2000）
    LKDR 2006.0 34.2 125.3（160） 714.3（874） 391.4（1266） 257.6+483.2（γ）（1523）
    下载: 导出CSV

    表 2  地热资源和水质主要指标

    Table 2.  Main indicators of geothermal water resources and water quality

    分区 编号 地热资源主要指标 水质主要指标/（mg·L−1）
    H/m Q/（m3·d−1） S/m q/（L·s−1·m−1） M/m T/°C 氟 溴 锶 锂 偏硼酸 偏硅酸
    西部 DR1 19.7 1238.6 268.2 0.05 456.0 50 — — — — — —
    SGDR 23.5 1530.2 137.5 0.13 640.3 75 1.08 6.00 16.17 0.541 3.15 58.18
    RSDR 18.1 2101.7 165.1 0.15 432.0 74 0.94 13.80 35.71 0.976 16.96 53.56
    中部 K1 22.6 2148.3 75.2 0.33 600.0 73 1.10 1.95 31.23 0.940 3.33 48.75
    DR2 59.14 2186.6 100.0 0.25 600.0 68 — — — — — —
    YTDR 6.0 185.6 130.0 0.02 450.0 60 2.40 0.04 2.22 0.390 15.14 35.76
    东部 DR3 43.0 737.0 290.0 0.03 157.0 35 — — — — — —
    LKDR 5.0 163.0 235.0 0.01 376.0 42 1.13 — 21.74 0.390 4.48 —
    　　注：H为水位埋深；Q为涌水量；S为降深；q为单位涌水量；M为热储层厚度；T为孔口水温度。依据《天然矿泉水地质勘探规范》（GB/T 13727—1992），K1和LKDR为锶水，SGDR和RSDR为锶水、硅水，YTDR为氟水，SGDR和RSDR中的溴达到了矿水标准，SGDR和YTDR中的偏硼酸达到了矿水标准；“—”表示未测。
    下载: 导出CSV
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收稿日期:  2023-06-17
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