用地下流体震前瞬间流动机制解释大地震短临前兆的特征
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MOMENTARY FLOW MECHANISM OF SHORT TERM EARTHQUAKE PRECURSOR
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    摘要:

    海城、唐山、松潘等七级大地震前,其短临异常表现出群体性、多样性、突发性,同时性、几起几落及异常群体向震中迁移等特征,简称一大二跳。而油、水井喷涌型异常,又是上述短临异常群体中的一种。对这种异常的机理研究表明,它要经过快速负荷加载、瞬间流动、卸载及渗流滞后三个过程。本文研究了伴随这三个过程可能会发生的地面垂直和水平的形变变化、应力变化、电磁变化等前兆现象。这些异常变化都因受控于震前快速负荷加载效应及瞬间流动效应,因而就能显示出大震前短临异常的上述特征。文章最后还对震前高孔隙压力产生的机理、地下流体瞬间流动的可能模式等问题进行了讨论。

    Abstract:

    Immediately before an earthquake the pressure water layer may produce momentary flow under the action of pulse-shaped earthquake force. In the light of the unsteady flow theory the authors proposed a mechanism to calculate the theoretical curves of the water level drop and the flowing rate of the underground water in the abnormal boreholes according to the radial symmetrical flow model so as to imitate the typical observational curve of the uprising of well water. The developing process of this mechanism requires the formation and vanishing of a funnelshaped distribution of ground water level. Therefore, it is necessary to make further calculations on the theoretical abnormal curves of vertical deformation on the ground surface, gravity, geoelectricity and geomagnetism. These phenomena are all related to the growth and decay of the funnel. Before a strong earthquake, lots of abnormal points of uprising of well water type are generated. At the same time, due to variations of the ground stress and deformation field, the balance state of ground water distribution is disturbed and subsurface fluid flows along faults and crevasses. Thus, geophysical effects more complex than radial symmetrical flow will be produced. This is a shallow layer mechanism of short-term precursors.

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王六桥,李善因.用地下流体震前瞬间流动机制解释大地震短临前兆的特征[J].地震工程学报,1984,6(3):35-43. Wang Liuqiao, Li Shanyin. MOMENTARY FLOW MECHANISM OF SHORT TERM EARTHQUAKE PRECURSOR[J]. China Earthquake Engineering Journal,1984,6(3):35-43.

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  • 收稿日期:1983-01-27
  • 最后修改日期:1983-11-01
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  • 在线发布日期: 2017-06-24