Quantification of exploitable shallow geothermal energy by using Borehole Heat Exchanger coupled Ground Source Heat Pump systems

被引:31
作者
Hein, Philipp [1 ,2 ,3 ]
Zhu, Ke [4 ]
Bucher, Anke [1 ]
Kolditz, Olaf [2 ,3 ]
Pang, Zhonghe [5 ]
Shao, Haibing [2 ,6 ]
机构
[1] Leipzig Univ Appl Sci HTWK, Fac Mech & Energy Engn, Karl Liebknecht Str 134, D-04277 Leipzig, Germany
[2] UFZ Helmholtz Ctr Environm Res, Permoserstr 15, D-04318 Leipzig, Germany
[3] Tech Univ Dresden, Fac Environm Sci, Helmholtzstr 10, D-01069 Dresden, Germany
[4] Shandong Jianzhu Univ, Fengming Rd 1000, Jinan 250101, Peoples R China
[5] Chinese Acad Sci, Inst Geol & Geophys, Geothermal Res Ctr, Beijing, Peoples R China
[6] Freiberg Univ Min & Technol TUBAF, Fac Geosci Geoengn & Min, Gustav Zeuner Str 12, D-09599 Freiberg, Germany
基金
中国国家自然科学基金;
关键词
Shallow geothermal potential; Borehole heat exchanger (BHE); Ground source heat pump (GSHP); OpenGeoSys (OGS); TEMPERATURE; PERFORMANCE; EFFICIENCY;
D O I
10.1016/j.enconman.2016.08.097
中图分类号
O414.1 [热力学];
学科分类号
摘要
In previous studies, the amount of exploitable shallow geothermal energy was estimated by assuming a uniform temperature drop of 2-6 degrees C in the aquifer. In this work, a more comprehensive numerical model has been employed to evaluate the available amount of shallow geothermal energy by using Borehole Heat Exchanger coupled Ground Source Heat Pump systems. Numerical experiments have been performed by simulating the long-term evolution of the subsurface temperature field, which is subject to the operation of borehole heat exchangers and varying parameters like subsurface thermal conductivity and groundwater flow velocity. The concept of equivalent temperature drop is proposed as an auxiliary quantity for the subsurface. With the help of this parameter, a procedure has been established to quantify the amount of shallow geothermal potential. Following this approach, a realistic equivalent temperature reduction is found to be from -1.8 to -4.4 degrees C in the subsurface over a period of 30 years. This can be translated to an annual extractable geothermal energy value in a unit surface area, and it ranges from 3.5 to 8.6 kW h m(-2) a(-1). The exact value is site specific and heavily depends on the soil thermal conductivity, groundwater velocity, and borehole arrangement. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:80 / 89
页数:10
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