介绍了腾冲台水温、水位观测井的地理位置、地质构造条件和水温、水位仪器布设、运行情况.对腾冲台水温、水位以及尼泊尔8.1级地震的同震响应特征分析,结果显示:尼泊尔8.1级地震引起的腾冲台水温、水位同震响应表现形态为水位下降-水温上升型,同震效应表现非常显著.水温同震响应滞后于水位同震响应.当水位产生同震响应时,水震波引起井孔内不同温度层位的井水多次对流和掺混,致使水温产生同震响应变化.水位同震响应持续时间比水温持续时间短,但水位的响应程度相比水温要剧烈.%The Nepal M 8.1 earthquake occurred at 2:11 p.m. April 25th 2015. The paper briefly introduced the geological location, geological structure condition, setting and operating conditions of water temperature and water level instruments of the observation well of Tengchong seismic station. Based on the analysis of the coseismic response characteristics of the water temperature and water level in Tengchong seismic station to the in Nepal M 8.1 earthquake, it is believed that the coseismic effect is very significant and its type is water level falling-water temperature rising. Water temperature rising was caused by water level falling, so the former happened behind the latter. The duration of water level falling is shorter than that of water temperature rising, while the response of the former is stronger than the latter.
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