基于土壤氡气测量和可控源音频大地电磁的陕西眉县汤峪地热预测

doi:10.11720/wtyht.2023.0010

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摘要

陕西眉县汤峪地热田储量丰富,但经过长期开采,现有地热井水温度和出水量逐年下降,因此亟需寻找新的潜在地热资源。区内已知地热井受断裂控制明显,故研究此处深部断裂展布对于潜在地热资源的探究具有重要现实意义。受方法本身限制和地形影响,研究区难以进行传统地质路线调查或大规模工程以探究控热断裂,因此本文优选基于穿透性的土壤氡气测量与可控源音频大地电磁的新技术方法组合探测隐伏断裂,进而圈定研究区潜在地热资源。基于实测的地表土壤氡浓度异常数据和CSAMT反演提供的地下电性结构模型,在验证已知断裂的基础上,新推断隐伏断裂6条,预测潜在地热区2处,并建立了汤峪地热田概念模型。结果表明,隐伏断裂处的土壤氡浓度远高于区域背景值,CSAMT反演视电阻率结果显示其位于低阻破碎带,圈定的潜在地热区分别位于剖面450~750 m和850~1150 m范围内,深度约250~300 m。本次研究认为,地热田整体位于低阻且土壤氡异常值大于区域背景值3倍的区域,研究结果可为该地区后续潜在地热资源的可持续开发利用提供借鉴。

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	薛东旭
	刘诚
	郭发
	王俊
	徐多勋
	杨生飞
	张沛

关键词 ：土壤氡气测量, CSAMT, 隐伏断裂, 地热资源, 汤峪

Abstract：

Despite abundant geothermal reserves of the Tangyu geothermal field in Meixian County, Shaanxi Province, long-term exploitation has decreased the water temperatures and yields of its existing geothermal wells year by year. Hence, there is an urgent need to explore new potential geothermal resources in the geothermal field. Since the known geothermal wells in the geothermal field are significantly controlled by faults, investigating the deep fault propagation holds critical significance for exploring the geothermal field’s potential geothermal resources. Due to the method limitations and the topographic influence, identifying thermal control faults through conventional geological route investigation or large-scale engineering is not applicable to the geothermal field. Therefore, a new technical method combining the penetrating soil radon measurement and the controlled source audio magnetotelluric (CSAMT) method was employed in this study to find concealed faults and delineate potential geothermal areas. Based on the measured surface soil radon concentration anomaly data and the subsurface electrical structure model derived from the CSAMT data inversion, this study inferred six new concealed faults on the basis of corroborating the known faults, predicted two potential geothermal areas, and built a conceptual model for the Tangyu geothermal field. As revealed by the results, the soil radon concentrations at concealed faults are much higher than the regional background value, and the concealed faults are located in the low-resistivity fracture zones as indicated by the apparent resistivity results based on CSAMT data inversion. Besides, the two potential geothermal areas spread from 450~750 m and 850~1 150 m on the profile, respectively, at depths of approximately 250~300 m. This study concludes that the geothermal field resides in a low-resistivity region with soil radon anomalies three times the regional background value. The results of this study provide a reference for the subsequent sustainable production and utilization of potential geothermal resources in the region.

Key words： soil radon measurement CSAMT concealed fault geothermal resource Tangyu

收稿日期: 2023-01-03 修回日期: 2023-04-11 出版日期: 2023-10-20

ZTFLH:

P631

基金资助:中国地质调查局国土空间生态地质调查及修复项目“西安城市群周边健康地质调查试点”(DD20211574)

通讯作者: 刘诚

作者简介: 薛东旭(1996-),男,工程师,硕士,2021年毕业于中国地质大学(北京)地球探测与信息技术专业,主要从事地球物理方法研究及应用工作。Email:18645810303@163.com

引用本文:

薛东旭, 刘诚, 郭发, 王俊, 徐多勋, 杨生飞, 张沛. 基于土壤氡气测量和可控源音频大地电磁的陕西眉县汤峪地热预测[J]. 物探与化探, 2023, 47(5): 1169-1178.
XUE Dong-Xu, LIU Cheng, GUO Fa, WANG Jun, XU Duo-Xun, YANG Sheng-Fei, ZHANG Pei. Predicting the geothermal resources of the Tangyu geothermal field in Meixian County, Shaanxi Province, based on soil radon measurement and the controlled source audio magnetotelluric method. Geophysical and Geochemical Exploration, 2023, 47(5): 1169-1178.

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https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2023.0010 或 https://www.wutanyuhuatan.com/CN/Y2023/V47/I5/1169

Fig.1 研究区大地构造位置(a)和地质(b)(据文献[3,20]修改)
1—第四系全新统;2—第四系上更新统;3—斜长角闪片麻岩;4—混合岩化片麻岩;5—糜棱岩化花岗岩;6—片麻状花岗岩;7—地层界线;8—断裂构造;9—地热井;10—河流水系;11—公路;12—研究区范围

Table 1 眉县汤峪地热温泉放射性指标检测结果

Table 2 研究区地层物性特征统计^[32]

Fig.2 标量CSAMT测量装置平面示意

Fig.3 研究区土壤氡浓度平面

Fig.4 联合剖面Ⅰ综合解释推断

Fig.5 典型测点视电阻率和阻抗相位曲线

Fig.6 眉县汤峪地热田概念模型

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