海潮、固体潮的叠加对深井水位动态的影响  

THE EFFECT OF THE OVERLAP OF THE SOLID AND SEA TIDE TO THE DYNAMIC CHANGE IN THE DEEP WATER TABLE

作　　者：庄光国[1] 

机构地区：[1]福建省地震局

出　　处：《华北地震科学》1992年第1期82-88,共7页North China Earthquake Sciences

摘　　要：作者通过调查和资料统计分析,发现我国沿海地区深井水位动态所呈现出的潮汐周期变化,并非受各潮汐因子的独自影响,而是来自于一种复合潮汐作用,即海潮、固体潮的叠加所产生的复合潮共同制约的结果。又由于井孔-含水层系统、距海远近和江河湖海水力联系等条件的差异而表现出多种多样的水位动态。Based on the survey and statistical analysis, the tide period variation of the dynamic deep water table in the coast area are not caused from the independent effect of the various tide factors but from a complex tide effect, which is the interact result occurred by the overlap of sea tide and solid tide. The various dynamic state of the water levels are due to different distance of water well from the coast and different hydraulic relation among the river, the lake and the sea.

关 键 词：海潮 固体潮 井孔 水位 动态 

分 类 号：P641.74[天文地球—地质矿产勘探]