日本地球惑星科学連合2015年大会

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セッション記号 A (大気水圏科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW25] 都市域の地下水・環境地質

2015年5月27日(水) 18:15 〜 19:30 コンベンションホール (2F)

コンビーナ:*安原 正也(独立行政法人 産業技術総合研究所)、林 武司(秋田大学教育文化学部)、浅田 素之(清水建設株式会社)、滝沢 智(東京大学大学院工学系研究科都市工学専攻)、鈴木 弘明(日本工営株式会社 中央研究所 総合技術開発部)、西田 継(山梨大学大学院医学工学総合研究部)

18:15 〜 19:30

[AHW25-P04] Long-term monitoring for groundwater temperature at closed loop GSHPs installed site

*Youngyun PARK1Jong-koo MOK2Bum-ju JANG2Seung-jin LEE2Yu-chul PARK3Jin-yong LEE1 (1.Department of Geology, Kangwon National University, Republic of Korea、2.Geo3eco Co. Ltd., Chuncheon, Republic of Korea、3.Department of Geophysics, Kangwon National University, Republic of Korea)

キーワード:Open loop, Ground source heat pump, Groundwater temperature, Korea

This study was performed to evaluate the influence of closed loop ground source heat pumps (GSHPs) on groundwater temperature. The closed loop ground source heat pumps was installed in 2009 and their capacity is 6,952 kW. The monitoring well was installed between wells used to closed loop GSHP and was located approximately 3.5 m away from well used to closed loop GSHP. The groundwater temperature were hourly measured from May 2010 to June 2013. The air temperature had ranged from -15.7 to 30.4oC and showed significant seasonal variations. The water temperature at monitoring well ranged from 13.3 to 16.3oC and their fluctuation trend was similar to air temperature. However, background of groundwater temperature showed narrow range (12.8 to 14.7oC) compared with that at monitoring well. In addition, background of groundwater temperature showed relatively weak seasonal variations. The phase difference between air and groundwater temperature at monitoring well was from approximately 4 to 5 months. The slope of regression line for air and background groundwater temperature was -0.006 and -0.01 oC/day, respectively. In contrast, the slope of regression line for groundwater temperature at monitoring well was 0.05 oC/day. These results indicate that thermal energy is cumulated in groundwater owing to operation of closed loop GSHPs in the study area. These trends can keep going. Therefore, the influence of closed loop GSHPs on groundwater temperature has to be evaluated to conserve groundwater from thermal contamination by operation of closed loop GSHPs and to keep energy efficiency. This work is supported by the Korean Ministry of Environment under "The GAIA project (2014000530001)".