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지하수류가 밀폐형 천공 지중 열교환기 성능에 미치는 영향(2)
한정상,김영식,이주현,이병호,한찬,Hahn, Jeongsang,Kiem, Youngseek,Lee, Juhyun,Lee, Byoungho,Hahn, Chan 한국지하수토양환경학회 2016 지하수토양환경 Vol.21 No.6
An increase of groundwater flux in BHE system creates that ground temperature (locT) becomes lower in summer and higher in winter time. In other words, it improves significantly the performance of BHE system. The size of thermal plume made up by advection driven-flow under the balanced energy load is relatively small in contrast to the unbalanced energy load where groundwater flow causes considerable change in the size of thermal plume as well ground temperature. The ground temperatures of the up gradient and down gradient BHEs under conduction only heat transport are same due to no groundwater flow. But a significant difference of the ground temperature is observed between the down gradient and up gradient BHE as a result of groundwater flow-driven thermal interference took placed in BHE field. As many BHEs are designed under the obscure assumption of negligible groundwater flow, failure to account for advection can cause inefficiencies in system design and operation. Therefore including groundwater flow in the design procedure is considered to be essential for thermal and economic sustain ability of the BHE system.
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지하수류가 대수층 열저장 시스템의 성능에 미치는 영향(3)
한정상,이주현,김영식,이광진,홍경식,Hahn, Jeongsang,Lee, Juhyun,Kiem, Youngseek,Lee, Kwangjin,Hong, Kyungsik 한국지하수토양환경학회 2017 지하수토양환경 Vol.22 No.4
When a warm well located downgradient is captured by cold thermal plume originated from an upgradient cold well, the warm thermal plume is pushed further downgradient in the direction of groundwater flow. If groundwater flow direction is parallel to an aquifer thermal energy storage (ATES), the warm well can no longer be utilized as a heat source during the winter season because of the reduced heat capacity of the warm groundwater. It has been found that when the specific discharge is increased by $1{\times}10^{-7}m/s$ in this situation, the performance of ATES is decreased by approximately 2.9% in the warm thermal plume, and approximately 6.5% in the cold thermal plume. An increase of the specific discharge in a permeable hydrogeothermal system with a relatively large hydraulic gradient creates serious thermal interferences between warm and cold thermal plumes. Therefore, an area comprising a permeable aquifer system with large hydraulic gradient should not be used for ATES site. In case of ATES located perpendicular to groundwater flow, when the specific discharge is increased by $1{\times}10^{-7}m/s$ in the warm thermal plume, the performance of ATES is decreased by about 2.5%. This is 13.8% less reduced performance than the parallel case, indicating that an increase of groundwater flow tends to decrease the thermal interference between cold and warm wells. The system performance of ATES that is perpendicular to groundwater flow is much better than that of parallel ATES.
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한정상(Jeongsang Hahn),윤운상(Yun Sang Yoon),김영식(Youngseek Kiem),한찬(Chan Hahn),박유철(Yu-Chul Park),목종구(Jong-Gu Mok) 한국지열·수열에너지학회 2012 한국지열에너지학회논문집 Vol.8 No.3
Mongolia has three(3) geothermal zones and eight(8) hydrogeothermal systems/regions that are, fold-fault platform/uplift zone, concave-largest subsidence zone, and mixed intermediate-transitional zone. Average temperature, heat flow, and geothermal gradient of hot springs in Arhangai located to fold-fault platform/uplift zone are 55.8℃, 60~110 ㎽/m2 and 35~50 ℃/㎞ respectively and those of Khentii situated in same zone are 80.5℃, 40~50 ㎽/m2, and 35~50 ℃/㎞ separately. Temperature of hydrothermal water at depth of 3,000 m is expected to be about 173~213°C based on average geothermal gradient of 35~50 ℃/㎞. Among eight systems, Arhangai and Khentii located in A type hydrothermal system, Khovsgol in B type, Mongol Altai plateau in C type, and Over Arhangai in D type are the most feasible areas to develop geothermal power generation by Enhanced Geothermal System (EGS). Potential electric power generation by EGS is estimated about 2,760 ㎾ at Tsenher, 1,752 ㎾ at Tsagaan Sum, 2,928 ㎾ at Khujir, 2,190 ㎾ at Baga Shargaljuut, and 7,125 ㎾ at Shargaljuut.
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