张子广, 盛艳蕊, 马利军, 王曰风, 朱振兴, 丁志华. 赤城井水温趋势转折上升原因分析[J]. 华北地震科学, 2014, 32(2): 50-54. DOI: 10.3969/j.issn.1003-1375.2014.02.010
引用本文: 张子广, 盛艳蕊, 马利军, 王曰风, 朱振兴, 丁志华. 赤城井水温趋势转折上升原因分析[J]. 华北地震科学, 2014, 32(2): 50-54. DOI: 10.3969/j.issn.1003-1375.2014.02.010
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ZHANG Zi-guang, SHENG Yan-rui, MA Li-jun, WANG Yue-feng, ZHU Zhen-xing, DING Zhi-hua. CAUSE ANALYSIS OF CHICHENG WELL WATER TEMPERATURE TREND TURNING UP[J]. North China Earthquake Sciences, 2014, 32(2): 50-54. DOI: 10.3969/j.issn.1003-1375.2014.02.010
Citation: ZHANG Zi-guang, SHENG Yan-rui, MA Li-jun, WANG Yue-feng, ZHU Zhen-xing, DING Zhi-hua. CAUSE ANALYSIS OF CHICHENG WELL WATER TEMPERATURE TREND TURNING UP[J]. North China Earthquake Sciences, 2014, 32(2): 50-54. DOI: 10.3969/j.issn.1003-1375.2014.02.010
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赤城井水温趋势转折上升原因分析

CAUSE ANALYSIS OF CHICHENG WELL WATER TEMPERATURE TREND TURNING UP

    摘要
  • 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。

     

    Abstract: 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.

     

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