杨增佺, 步克功, 方召盟. 张北6.2级地震前廊坊地区水位中期异常特征分析[J]. 华北地震科学, 2001, 19(3): 63-67.
引用本文: 杨增佺, 步克功, 方召盟. 张北6.2级地震前廊坊地区水位中期异常特征分析[J]. 华北地震科学, 2001, 19(3): 63-67.
YANG Zeng-quan, BU Ke-gong, FANG Zhao-meng. ANALYSIS TO THE CHARACTERISTIC OF THE MEDIUM TERM ANOMALIES IN GROUNDWATER LEVEL IN LONGFANG REGION BEFORE ZHANGBEI M6.2 EARTHQUAKE[J]. North China Earthquake Sciences, 2001, 19(3): 63-67.
Citation: YANG Zeng-quan, BU Ke-gong, FANG Zhao-meng. ANALYSIS TO THE CHARACTERISTIC OF THE MEDIUM TERM ANOMALIES IN GROUNDWATER LEVEL IN LONGFANG REGION BEFORE ZHANGBEI M6.2 EARTHQUAKE[J]. North China Earthquake Sciences, 2001, 19(3): 63-67.

张北6.2级地震前廊坊地区水位中期异常特征分析

ANALYSIS TO THE CHARACTERISTIC OF THE MEDIUM TERM ANOMALIES IN GROUNDWATER LEVEL IN LONGFANG REGION BEFORE ZHANGBEI M6.2 EARTHQUAKE

  • 摘要: 对张北6.2级地震前廊坊市区域内4口浅井的水位变差研究表明,这4口井的水位变差在张北地震前显示出明显的中期和中短期异常变化,存在着"正值上升→下降→负值→地震"的规律。认为浅井水位作为一种附加力源,以流体载荷、孔隙压力、化学腐蚀的形式作用于地壳岩石,对张北地震的发生起到了促进作用。

     

    Abstract: The study on the variation in groundwater level of the 4 shallow wells in Langfang region before Zhangbei M6.2 earthquake indicates that the variation difference in water level of the 4 wells shows clearly medium and short term anomalies.Their common character is increasing with positive value,decreasing,negative value,and then earthquake.We believe,as a additional force source,water level of shallow well acts on the crustal rock in form of fluid loading,pore pressure and chemical erosion,which promotes the Zhangbei earthquake.

     

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