CAJ | 학술논문

以赣州井2007年6月-2011年9月水位观测数据为研究对象，辅以水文和气象资料作对比分析，运用数理方法分析水位动态变化特征。通过分析发现，赣州井水位动态变化的主要干扰因素是降水渗入和贡水水位。另外，在无降水和地震的情况下，水位也表现出有明显的潮汐和气压效应。
이공주정2007년6월-2011년9월수위관측수거위연구대상，보이수문화기상자료작대비분석，운용수리방법분석수위동태변화특정。통과분석발현，공주정수위동태변화적주요간우인소시강수삼입화공수수위。령외，재무강수화지진적정황하，수위야표현출유명현적조석화기압효응。
This paper assessed the well water level observation data of ganzhou well from June 2007 to September 2011, based on the analyses of hydrological and meteorological data. The dynamic changing characters are analyzed by the mathematical method. Through the analysis, the main interference factors of dynamic change of water level in ganzhou well are the infiltration of the rainfall and gongshui water level. In addition, in the absence of rainfall and earthquake conditions, water level also shows obvious effect of tidal and barometric pressure.