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北京平原区隐伏断裂与氡浓度响应关系

张晓亮, 白凌燕, 倪敬波, 王志辉, 赵勇, 何付兵. 2022. 北京平原区隐伏断裂与氡浓度响应关系. 物探与化探, 46(2): 344-351. doi: 10.11720/wtyht.2022.1066
引用本文: 张晓亮, 白凌燕, 倪敬波, 王志辉, 赵勇, 何付兵. 2022. 北京平原区隐伏断裂与氡浓度响应关系. 物探与化探, 46(2): 344-351. doi: 10.11720/wtyht.2022.1066
ZHANG Xiao-Liang, BAI Ling-Yan, NI Jing-Bo, WANG Zhi-Hui, ZHAO Yong, HE Fu-Bing. 2022. Relationship between concealed faults and radon concentration in plain areas of Beijing. Geophysical and Geochemical Exploration, 46(2): 344-351. doi: 10.11720/wtyht.2022.1066
Citation: ZHANG Xiao-Liang, BAI Ling-Yan, NI Jing-Bo, WANG Zhi-Hui, ZHAO Yong, HE Fu-Bing. 2022. Relationship between concealed faults and radon concentration in plain areas of Beijing. Geophysical and Geochemical Exploration, 46(2): 344-351. doi: 10.11720/wtyht.2022.1066

北京平原区隐伏断裂与氡浓度响应关系

  • 基金项目:

    中国地质调查局项目“北京地区主要活动断裂精细调查及灾害效应调查“(12120113012000)

    北京市地质矿产勘查开发局项目“通州区南部(751 km2)重大地质问题调查与评价“(PXM2019_158203_000005)

    “北京平原区要活动断裂监测与维护“(PXM2021-158203-000008)

详细信息
    作者简介: 张晓亮(1982-),男,硕士,教授级高级工程师。研究方向为地球物理、城市活动断裂研究。Email: zxlddy@163.com
  • 中图分类号: P632

Relationship between concealed faults and radon concentration in plain areas of Beijing

  • 北京地区隐伏断裂发育,NW及NE向断裂相互交汇,成为未来可能发生地震的构造。为了研究活动断裂与土壤氡浓度的响应关系,本次对北京平原区NW和NE向2条剖面进行了氡浓度测量。通过测试分析,基本查明了隐伏构造与土壤氡浓度的对应关系以及影响土壤氡浓度的相关地质因素。研究表明,活动断裂存在的区域氡浓度明显高于周边区域,且在构造复杂与活动性强的断裂区域氡浓度值变化更为明显;新生界厚度对氡的散逸强度存在一定的制约,北京地区新生界厚度与氡浓度水平成正相关;不同成土母质核素比活度不同,对区域氡浓度背景值亦存在影响。本次研究成果确定了隐伏断裂与土壤氡浓度的对应关系,以及新生界厚度和不同成土母质土壤对土壤氡浓度的影响,为今后在平原区开展隐伏断裂调查及氡浓度研究工作有重要借鉴和指导意义。
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出版历程
收稿日期:  2021-02-03
刊出日期:  2022-06-28

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