李新生, 闫文中, 李同录, 孙国梁. 2001: 西安地裂缝活动趋势分析. 工程地质学报, 9(1): 39-43.
    引用本文: 李新生, 闫文中, 李同录, 孙国梁. 2001: 西安地裂缝活动趋势分析. 工程地质学报, 9(1): 39-43.
    LI Xinsheng, YAN Wenzhong, LI Tonglu, SUN Guoliang. 2001: ANALYSIS ON THE MOVEMENT TENDENCY OF XIAN GROUND FISSURES. JOURNAL OF ENGINEERING GEOLOGY, 9(1): 39-43.
    Citation: LI Xinsheng, YAN Wenzhong, LI Tonglu, SUN Guoliang. 2001: ANALYSIS ON THE MOVEMENT TENDENCY OF XIAN GROUND FISSURES. JOURNAL OF ENGINEERING GEOLOGY, 9(1): 39-43.

    西安地裂缝活动趋势分析

    ANALYSIS ON THE MOVEMENT TENDENCY OF XIAN GROUND FISSURES

    • 摘要: 西安地裂缝的形成及活动主要受构造活动及人类活动因素影响, 而近来地裂缝的超常活动主要与过量抽取地下水引起的地面不均匀沉降有关。根据对抽水及地面荷载引起地层压密固结过程的分析、地下水位变化趋势的分析以及应用 Ver-hulst模型计算、预测结果, 西安地裂缝的强烈活动将有减缓或逐渐稳定的趋势。有关地裂缝活动的最新实际监测数据已显示出一些相应的征兆。

       

      Abstract: The formation and movement of Xian ground fissures are mainly caused by geotectonic movement and human activities. The extraording movement of the ground fissures mainly resulted from uneven ground subsidence that caused by the over pumping of ground water. According to analyses of compaction consolidation process of sediments layers, ground water variation tendency, and result of Verhulst model prediction, it is concluded that the movement intensity of Xian ground fissures tends to gradually become weaken. The resent observation data on ground fissures movement show some indicatons to reduction in its rate.

       

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