摘要
赤城井水温2010年底至2011年初由下降趋势转折上升,最大上升幅度约0.02℃,本文对此现象进行了实地调查和分析研究。通过环境因素对比分析,认为该井水温转折上升与赤城县城区白河湾公园蓄水有关。同时,根据分析结果,推测赤城井水温后续变化的可能特征是持平或恢复下降趋势。
Chicheng well water temperature turned up from trend descending between the end of 2010 and the beginning of 2011, the maximum rising rage is about 0.02℃. This phenomenon is studied through field investigation and contrastive analysis in this paper. The analysis shows that the turning up of the Chicheng well water temperature is related to water impounding in Baihewan park in the city proper of Chicheng County. At the same time, the water temperature of Chicheng well will hold the line or restore downward trend.
出处
《华北地震科学》
2014年第2期50-54,共5页
North China Earthquake Sciences
基金
河北省地震科技星火计划项目"怀来地区断层流体地球化学空间特征研究"(项目编号:201308)
关键词
水温
地温
蓄水
异常
赤城
water temperature
ground temperature
water impounding
anomaly
Chicheng
