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지하수류가 밀폐형 천공 지중열교환기 성능에 미치는 영향(1)
한정상,한찬,윤운상,김영식,Hahn, Jeong Sang,Hahn, Chan,Yoon, Yun Sang,Kiem, Young Seek 한국지하수토양환경학회 2016 지하수토양환경 Vol.21 No.3
To analyze the influence of various groundwater flow rates (specific discharge) on BHE system with balanced and unbalanced energy loads under assuming same initial temperature (15℃) of ground and groundwater, numerical modeling using FEFLOW was used for this study. When groundwater flow is increased from 1 × 10<sup>−7</sup> to 4 × 10<sup>−7</sup>m/s under balanced energy load, the performance of BHE system is improved about 26.7% in summer and 22.7% at winter time in a single BHE case as well as about 12.0~18.6% in summer and 7.6~8.7% in winter time depending on the number of boreholes in the grid, their array type, and bore hole separation in multiple BHE system case. In other words, the performance of BHE system is improved due to lower avT in summer and higher avT in winter time when groundwater flow becomes larger. On the contrary it is decreased owing to higher avT in summer and lower avT in winter time when the numbers of BHEs in an array are increased, Geothermal plume created at down-gradient area by groundwater flow is relatively small in balanced load condition while quite large in unbalanced load condition. Groundwater flow enhances in general the thermal efficiency by transferring heat away from the BHEs. Therefore it is highly required to obtain and to use adequate informations on hydrogeologic characterristics (K, S, hydraulic gradient, seasonal variation of groundwater temperature and water level) along with integrating groundwater flow and also hydrogeothermal properties (thermal conductivity, seasonal variation of ground temperatures etc.) of the relevant area for achieving the optimal design of BHE system.
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몽골의 천부 지열에너지(냉난방 에너지)개발 가능성에 관한 연구
한정상(Jeongsang Hahn),윤운상(Yun Sang Yoon),윤건신(Kern Sin Yoon),이태열(Tae Yul Lee),김형수(Hyong Soo, Kim) 한국지열·수열에너지학회 2012 한국지열에너지학회논문집 Vol.8 No.2
Time-series variation of groundwater temperature in Mongolia shows that maximum temperature is occured from end of October to the first of February(inter time) and minimum temperature is observed from end of April to the first of May(summer time). Therefore ground temperature is s a good source for space heating in winter and cooling in summer. Groundwater temperatures monitored from 3 alluvial wells in Ulaabaatar at depth between 20 and 24 m are (4.43±0.8)℃ with average of 4.21℃ but mean annual ground temperature(MAGT) at the depth of 100 m in Ulaanbaatar was about 3.5~6.0℃. Bore hole length required to extract 1 RT’s heat energy from ground in heating time and to reject 1 RT’s heat energy to ground in summer time are estimated about 130 m and 98 m respectively. But in case that thermally enhanced backfill and U tube pipe placement along the wall are used, the length can be reduced about 25%. Due to low MAGT of Ulaabaatar such as 6℃, the required length of GHX in summer cooling time is less than the one of winter heating time. Mongolia has enough available property, therefore the most cost effective option for supplying a heating energy in winter will be horizontal GHX which absorbs solar energy during summer time. It can supply 1 RT’s ground heat energy by 570 m long horizontally installed GHX.
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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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