ISSN 1000-3665 CN 11-2202/P
    梁健, 张虎元, 张永雷, 张磊. 北京市平原区典型地质灾害危险性评估[J]. 水文地质工程地质, 2008, 35(5): 113-115.
    引用本文: 梁健, 张虎元, 张永雷, 张磊. 北京市平原区典型地质灾害危险性评估[J]. 水文地质工程地质, 2008, 35(5): 113-115.
    LIANGJian~, . Risk evaluate for typical geological hazards in Beijing plain[J]. Hydrogeology & Engineering Geology, 2008, 35(5): 113-115.
    Citation: LIANGJian~, . Risk evaluate for typical geological hazards in Beijing plain[J]. Hydrogeology & Engineering Geology, 2008, 35(5): 113-115.

    北京市平原区典型地质灾害危险性评估

    Risk evaluate for typical geological hazards in Beijing plain

    • 摘要: 北京市平原区地质灾害主要表现为活动断裂、地震砂土液化和地面沉降。文章结合具体实例对三种地质灾害危险性及其评估方法进行了探讨。活动断裂的危险性主要根据断裂的活动时期、断裂不同部位的活动性以及评估区距离断裂活动部位的远近程度进行评估。地震砂土液化判别采用现场标准贯入试验进行评估。地面沉降预测评估依据地下水累计开采量与累计地面沉降量的相关关系分析和固结理论进行。

       

      Abstract: Typical geological hazards in Beijing plain included active fault,seismic liquefaction of sand and land subsidence.A practical research area was selected to evaluate the risk of typical geological hazards in Beijing plain.It was suggested that the risk of active faults can be reasonably explained by the history of the faults and their occurrence period,while the risk of groundsill seismic liquefaction was examined in the field with penetration test.With applying consolidation theory,the risk of land subsidence was indirectly calculated according correlation between accumulative withdrawal of groundwater and accumulative land subsidence.

       

    /

    返回文章
    返回