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热示踪法对广州城市化地下温度影响的辨识

连健斌 李绍恒 陈建耀 龚柔艳 梁贝竹 董林垚

中山大学学报(自然科学版)(中英文)2024,Vol.63Issue(4):29-36,8.
中山大学学报(自然科学版)(中英文)2024,Vol.63Issue(4):29-36,8.DOI:10.13471/j.cnki.acta.snus.ZR20230044

热示踪法对广州城市化地下温度影响的辨识

The identification of the influence of heat tracing method on underground temperature in the urbanization process of Guangzhou

连健斌 1李绍恒 1陈建耀 1龚柔艳 2梁贝竹 1董林垚3

作者信息

  • 1. 中山大学地理科学与规划学院/粤北岩溶区森林生态系统碳水耦合野外观测研究站,广东 广州 510006
  • 2. 湖南农业大学水利与土木工程学院,湖南 长沙 410000
  • 3. 长江水利委员会长江科学院,湖北 武汉 430000
  • 折叠

摘要

Abstract

The intrinsic energy exchange exists between the shallow ground temperature and near-sur-face air temperature.As time progresses,surface temperature changes are propagated downwards and superimposed onto the steady-state geothermal field.Therefore,it is possible to reconstruct the history of ground surface temperature changes using the current subsurface temperature profile.To assess the combined effect of global warming and urbanization on the subsurface temperature of Guangzhou,this paper collected temperature data from Guangzhou station during 1958-2022 and conducted regression analysis and anomaly analysis.Meanwhile,the temperature-depth(T-Z)profiles of 16 observation boreholes in Guangzhou were obtained through field measurements.By conducting regression analysis on the lower section of the temperature profile,the geothermal gradient of the area and the depth of de-viation from the constant geothermal gradient were determined.Finally,the onset time and magnitude of warming were obtained by combining temperature data,and the theoretical curves of the surface warming profile in Guangzhou were derived using the analytical solution equation.The results show that the warming rate of air temperature in Guangzhou from 1958 to 2022 is 0.33℃per decade,with the onset time of warming being 1987,and the magnitude of warming being 2.6℃.The observed geo-thermal gradient in Guangzhou is 0.036℃/m,and the depth of deviation from the constant geothermal gradient is 54.8 m,essentially consistent with the analytically calculated depth of 57.6 m.The study finds that the earlier the start time of urbanization-induced surface warming,the greater the depth of deviation of subsurface temperature from the constant geothermal gradient,indicating the depth of de-viation can be used to describe the process of urbanization.

关键词

全球变暖/城市化/气温/地温/广州

Key words

global warming/urbanization/air temperature/ground temperature/Guangzhou

分类

天文与地球科学

引用本文复制引用

连健斌,李绍恒,陈建耀,龚柔艳,梁贝竹,董林垚..热示踪法对广州城市化地下温度影响的辨识[J].中山大学学报(自然科学版)(中英文),2024,63(4):29-36,8.

基金项目

国家重点研发项目(2023YFC3709002) (2023YFC3709002)

国家自然科学基金(41977171) (41977171)

广东省区域联合基金(2021A1515110505) (2021A1515110505)

中山大学学报(自然科学版)(中英文)

OA北大核心CSTPCD

0529-6579

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