北京太平庄井地下水物理动态研究  

THE PHYSICAL DYNAMIC BEHAVIOR OF GROUNDWATER IN THE TAIPINGZHUANG WELL,BEIJING

作　　者：朱清钟[1] 田竹君[1] 谷元珠[1] 

机构地区：[1]国家地震局地质研究所

出　　处：《地震地质》1996年第4期403-408,共6页Seismology and Geology

摘　　要：根据太平庄井地下水水位、流量、水温等物理动态特征，探讨了三项潮汐动态（水位、流量、水温）、洼地积水倒压传递效应、截流效应、水温同震阶降动态、震前流量突变异常动态等微观动态及其与地震的关系。最后讨论了三项潮汐动态机理，认为太平庄井对地震监测预报，特别是首都圈地震监测预报有重要作用。Based on the physical dynamic behavior of groundwater including water-level,flux and water temperature,and their relative tides effect of inverse transmission of the water press caused by accumulated water in the depressions,effect of the damming flow,rapid-fall coseismic behavfor of water temperature and abnormal behavior of sharp flux change before earthquake,their micro-behaviors as well as the relationship between them and earthquake are discussed.Finally the relative mechanisms are also studied.The result shows that the Taipingzhuang well is important for earthquake monitoring prediction,especially in the capital region.

关 键 词：地震前兆 地下水 物理动态 井水水位 

分 类 号：P315.7[天文地球—地震学]