http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
복합지열시스템에 대한 부지특성화: 대수층의 수리지질학적 특성
목종구,박유철,박영윤,김승겸,오정석,선우은미,Mok, Jong-Koo,Park, Yu-Chul,Park, Youngyun,Kim, Seung-Kyum,Oh, Jeong-Seok,Seonwoo, Eun-Mi 대한지질공학회 2017 지질공학 Vol.27 No.3
This study was performed in order to hydrogeological analysis of aquifer, which is a necessary part for evaluating the efficiency of the combined well and open-closed loops geothermal (CWG) systems. CWG systems have been proposed for the effective utilization of geothermal energy by combining open loop geothermal systems and closed loop geothermal systems. Small aperture CWG systems and large aperture CWG systems were installed at a green house land with water curtain facilities in Chungju City. Aquifer tests include pumping tests and step-drawdown tests were conducted to analyse hydrogeological characteristics of aquifer in the study area. The transmissivity was estimated in the range of $13.49{\sim}58.99cm^2/sec$, and the storativity was estimated in the range of $1.13{\times}10^{-5}{\sim}5.20{\times}10^{-3}$. The geochemical analysis showed $Ca^{2+}$ ion and ${HCO_3}^-$ ion were dominant in groundwater. The Langelier Saturation Index and the Ryznar Stability Index showed low scaling potential of groundwater. In the analysis of vertical water temperature change, the geothermal gradient was estimated as $2.1^{\circ}C/100m$, which indicated the aquifer was enough for geothermal systems. In conclusion, groundwater is rich, can stably use geothermal heat, and it is less likely to cause deterioration of thermal energy efficiency by precipitation of carbonate minerals in study area. Therefore, the study area is suitable for installation of the combined geothermal system. 본 연구는 복합지열시스템의 효율성 평가를 위하여 필요한 부분인 대수층의 수리지질학적 분석을 위하여 수행되었다. 복합지열시스템은 개방형 지열시스템과 밀폐형 지열시스템을 결합하여 지열의 효과적 이용을 목적으로 제안되었으며, 연구지역인 충주시 금가면의 수막재배 지역에 소구경 복합지열시스템과 대구경 복합지열시스템이 설치되었다. 연구 지역 대수층의 수리지질학적 특성 분석을 위하여 양수시험과 단계양수시험을 포함하는 현장수리시험 결과, 대수층의 투수량계수는 $13.49{\sim}58.99cm^2/sec$의 범위를 가지며, 저유계수는 $1.13{\times}10^{-5}{\sim}5.20{\times}10^{-3}$의 범위로 분석되었다. 또한, 지구화학적 분석에서 지하수 성분 중 $Ca^{2+}$이온과 ${HCO_3}^-$ 이온이 우세한 것으로 나타났고, 랑겔리어 지수 및 리즈나 지수 분석에서 지하수 내의 탄산염 광물의 침전 가능성이 낮게 평가되었다. 수직적 수온 변화 분석에서는 평균 증온률이 $2.1^{\circ}C/100m$로 평가되어 지열 특성이 충분한 것으로 나타났다. 따라서, 연구지역에서는 지하수의 양이 풍부하고 지중열을 안정하게 사용할 수 있으며 탄산염 광물의 침전에 의한 열에너지 효율 저하가 발생할 가능성이 낮으므로 복합지열시스템 설치가 적합한 것으로 판단된다.
밀폐형과 개방형이 결합된 복합지열시스템의 지중열교환기 성능 분석
박영윤,송재용,이근춘,김기준,목종구,박유철,Park, Youngyun,Song, Jae-Yong,Lee, Geun-Chun,Kim, Ki-Joon,Mok, Jong-Koo,Park, Yu-Chul 한국지하수토양환경학회 2017 지하수토양환경 Vol.22 No.5
This study was conducted to evaluate performance of geothermal heat exchanger (GHE) in the combined well and open-closed loops geothermal (CWG) systems. The CWG systems were designed to combine open loop geothermal heat pumps and closed loop geothermal heat pumps for high energy efficiency. GHE of the CWG systems could be installed at pumping wells for agricultural usage. To get optimal heat exchange capacity of GHE of the CWG systems, 4 GHEs with various materials and apertures were tested at laboratory scale. Polyethylene (PE) and stainless steel (STS) were selected as GHE materials. The maximum heat exchange capacity of GHEs were estimated to be in the range of 33.0~104 kcal/min. The heat exchange capacity of STS GHEs was 2.4~3.2 times higher than that of PE GHE. The optimal cross section area of GHE and flow rate of circulating water of GHE were estimated to be $2,500mm^2$ and 113 L/min, respectively. For more complicated GHE of the CWG systems, it is necessary to evaluate GHEs at various scales.
분자생물학적 방법을 이용한 지열시스템 관정 및 주변지역 미생물종 모니터링
안창민,한지선,김창균,박유철,목종구,장범주,Ahn, Chang-Min,Han, Ji-Sun,Kim, Chang-Gyun,Park, Yu-Chul,Mok, Jong-Koo,Jang, Bum-Ju 한국지하수토양환경학회 2012 지하수토양환경 Vol.17 No.6
This study was conducted to monitor microbial species dynamics within the aquifer due to long term operation of geothermal heat pump system. The species were identified by molecular biological methods of 16S rDNA. Groundwater sample was collected from both open (S region) and closed geothermal recovery system (J region) along with the control. J measured and control as well as S measured found Ralstonia pickettii as dominant species at year 2010. In contrast, Rhodoferax ferrireducens was dominantly observed for the control of S. In 2011, Sediminibacterium sp. was universely identified as the dominant species regardless of the monitoring places and type of sample, i.e., measured or control. The difference in the dynamics between the measured and the control was not critically observed, but annual variation was more strikingly found. It reveals that possible environmental changes (e.g. ORP and DO) due to the operation of geothermal heat recovery system in aquifer could be more exceedingly preceded to differentiate annual variation of microbial species rather than positional differences.