CAJ | 학술논문

本文简单介绍了延寿台水温井的观测条件与环境，分析了该井观测到的多次同震水位变化以及伴随的深层水温变化，并且水温多是上升，震后一至数小时后又恢复。由于井水振荡使水受到扰动，导致不同深度不同温度水的混合，从而造成同震水温变化的弥散模型，而后由于水的热传导作用又恢复正常。
본문간단개소료연수태수온정적관측조건여배경，분석료해정관측도적다차동진수위변화이급반수적심층수온변화，병차수온다시상승，진후일지수소시후우회복。유우정수진탕사수수도우동，도치불동심도불동온도수적혼합，종이조성동진수온변화적미산모형，이후유우수적열전도작용우회복정상。
This paper briefly introduced the condition and environment of observation on the water temperature of Yanshou well. The coseismic water level oscillation and correlated deep water temperature changes have been observed in this well. And the water temperature usually rises and recovers after one to several hours. It suggested that the temperature drop is produced by dispersive transfer of heat as the water oscillates, and follow-up thermal conduction makes temperature recovery.