• 한국지하수토양환경학회지:지하수토양환경
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• 제11권4호
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• pp.41-47
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• 2006

온천공에 대한 일일 적정양수량 및 영향평가는 온천법에서 지정된 온천전문기관이 수행하여야 하는 중요한 조사 항목이다. 온천전문조사는 1996년 이전까지 한국지질자원연구원에서 수행하였으나, 2006년 현재에는 8개 온천전문기관이 온천법에 등록되어 있어 일관된 조사가 이루어지지 않고 있는 실정이다. 따라서 이 논문은 온천법 및 온천업무처리지침에서 규정된 사항을 사례적용하는 방법을 통해서 온천전문기관 및 관련 업체에서 온천조사시 동일한 해석을 할 수 있도록 하는 것이 그 목적이다. 적정양수량 산출시 온천공은 양수후 수위회복이 느린 것이 많아 수위회복시간이 고려되었다. 따라서 단계양수시험후 수위회복이 상대적으로 느린 온천공은 적정양수량이 감소하게 된다. 온천공간 영향평가는 2개 이상 온천공사이의 영향관계를 규명하는 것으로서, 신규공에서 양수시험을 실시하고 주위 공들에서의 수위강하를 관측하여 온천공간 영향의 정도를 평가하고 있다.

• 교육녹색환경연구
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• 제6권2호
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• pp.25-52
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• 2007

This paper is focused on the economical efficiency of the geothermal heat pump system in school. As the importance of problems of environment and energy becomes larger, the development and distribution of energy-saving technology in the whole nation has become influential. This paper is intended, targeting on school buildings scattered all over the country, to evaluate the introduction and possibility of a terrestrial heat system which is in the first stage of introduction in the country, through energy consumption and efficiency in case where a terrestrial heat system is introduced. To do that, the author performed a qualitative analysis of the heat pump system using various terrestrial heat energy and the system introduced to existing school buildings and, through the analysis, made tentative evaluation on the most environment-friendly and energy saving type system. Also, the author performed simulation analysis using a currently typical school building standard and, on the basis of this result, conducted efficiency analysis of various heat pump systems. The conclusion according to synthetical analysis & evaluation can be summarized as follows. In case a heat pump system is introduced to a school building, it was deemed the investment in the early stage would increase, but the investment could be collected within 5~6 years through reduction of large operation expenses. Also, it was analyzed in case of terrestrial heat contracted heat mode using midnight electric power among heat pump systems, not only early investment but also operation expenses could be reduced to a great extent. Accordingly in case the system using terrestrial heat energy is applied to the school buildings that are to be newly built or repaired in the future, it will provide an object-lesson to students as well as contributing to energy saving.

• 지구물리와물리탐사
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• 제10권4호
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• pp.345-352
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• 2007

호주 Century 광산 주변에서 2차원 MT 탐사를 수행하였다. 현장으로부터 약 80 km 떨어진 Gregory Downs(RR_GREG)에 원거리 기준점을 설치, 운영하고 이 자료를 이용하여 양질의 탐사자료의 획득이 가능하였다. 이와 동시에 현장으로부터 약 6,400 km 떨어진 일본 Esashi (RR_ESS)에서 측정된 수평 자기장 자료를 이용하여 원거리 기준 자료처리를 수행한 결과 자기장의 coherency가 낮아 원거리 기준점 자료로 사용하기에는 적합하지 않았다. Century 광산의 주변에서 수행된 측선 탐사자료의 2차원 및 3차원 역산 결과 연구지역의 전반적인 심부 지질구조를 잘 나타내었으며, 탐사의 주된 목표인 Termite Range Fault는 측선의 북쪽에 나타나는 저비저항층과 남쪽에 나타나는 고비저항층의 경계면을 이루면서 북동쪽으로 약간 경사진 것으로 해석되었다.

• 한국지열·수열에너지학회논문집
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• 제3권2호
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• pp.1-7
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• 2007

This paper is concerned with the selection of proper working fluids for medium temperature range heat pipe. The heat pipe which is made of SUS 316L has a total length of 700 mm as well as an outside diameter of 27.2 mm and a thickness of 2.1 mm respectively. Working fluids used in this study were Naphthalene, Biphenyl and Dowtherm A. Their charge amounts were about 40% of the inside volume of evaporator section. Experimental results shows that the Dowtherm A is good for $200^{\circ}C{\sim}300^{\circ}C$temperature range, while the Naphthalene is proper for $300^{\circ}C{\sim}430^{\circ}C$. In the case of the Naphthalene heat pipe, the heat transfer rate reaches 1500 W along with a vapor temperature of $430^{\circ}C$.

• 지질공학
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• 제3권3호
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• pp.267-278
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• 1993

지하수의 온도측정자료는 자연상태 및 인공적인 충진(Recharge)에 의한 지하수의 유동상태 및 대수층의 특성을 파악할 수 있는 중요한 parameter가 된다. 대수층내 지하수의 온도는 지하수를 저류하고 있는 대수층의 구성암석들의 온도를 반영하며, 지하수의 유동성과 저온능력은 지각내부에서 발달된 지열을 대수층내 분산시키는 역할을 한다. 조사지역내(25개 시추공)에서 측정된 지하수온도자료들은 대수층내 온도분포의 근원적인 수리지질학적 의미와 수리역학적 문제점 해결에 유용하게 이용되며, 또한 지표변으로부터 열원이 전달되는 전파율과 심부 증온율 연구에 기여된다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 총회 및 춘계학술발표회
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• pp.455-458
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• 2004

This study uses time series analyses to evaluate fluctuation of water levels in a geothermal water well due to pumping, in relation to rainfall at Dongrae hot-spring site on the southeastern coast of tile Korean peninsula. The volume of water pumped from the public study wells ranges from 542 to 993 m$^3$/month, and the minimum water level ranged from 35 to 144.7 m during the measured period. Autocorrelation analysis was conducted for the withdrawal rate at the public wells, water levels and rainfall. The autocorrelation of the withdrawal rate shows distinct periodicity with 3 months of lag time, the autocorrelation of rainfall shows weak linearity and short memory with 1 months of lag time, and the autocorrelation of water levels shows weak linearity and short memory with 2 months of lag time. The cross-correlation between the pumping volume and the minimum water level shows a maximum value 1 at a delayed time of 34 months. The cross-correlation between rainfall and the minimum water level shows a maximum value of 0.39 at a delayed time of 32 months.

• 한국지열·수열에너지학회논문집
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• 제13권4호
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• pp.21-30
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• 2017

Recently, It has increased the importance of building energy saving. Pipe insulation as well as building envelope insulation is to improve energy efficiency and reduce the energy loss. However, there continues to use the old standard for pipe insulation that is one of the most important elements in energy savings in buildings. The purpose of this study is to propose suitable pipe insulation thickness for reducing building energy use. The study also reviews pipe insulation thickness standard in accordance to Korea standard, ASHRAE 90.1 and BS5422 and analyzed through thermal simulation. As a result, it is necessary to apply the performance design method of the pipe insulation thickness to reduce the energy loss of the piping.

• 한국지열·수열에너지학회논문집
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• 제12권4호
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• pp.15-20
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• 2016

Even though the control device of the heating system works well, insufficient water flow rates can degrade control performance and thermal comfort. The water flow rate should be adjusted appropriately to cope with the heating load of each zone. In order to solve these problems, a new balancing concept 'dynamic balancing' was proposed where a balancing valve opening can be automatically modulated according to the heating condition of the room. This study analyzed the effects of dynamic balancing upon indoor thermal environment and energy consumption in a radiant floor heating system through field measurement. Under part-load conditions, the use of a dynamic balancing is a more effective method to reduce energy consumption and to prevent a cavitation. Dynamic balancing is able to help boost the temperature of a room in the start-up period.

• Journal of Biosystems Engineering
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• 제23권2호
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• pp.135-146
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• 1998

The equation to predict the soil temprature of Pusan and Chinju city as a function of time and soil depth for the geothermal energy utilization system and agriculture was devised. The equation was $T(x,t)\;=\;Tm\;-\;To{\cdot}ExP(-{\xi}){\cdot}cos{{\omega}{\cdot}[t-to-x/(2{\cdot}{\alpha}{\cdot}{\omega})^{0.5}]}$ with the soil thermal diffusivity, ${\alpha},\;of\;0.4\;\textrm{m}^2/day,\;0.0375\;\textrm{m}^2/day$ and phase zero point, to, of 24 days, 22.4 days in Pusan and Chinju city, respectively, during ten years from 1987 to 1996. The predicted and measured soil temperatures agreed well with the coefficient of determination of 0.95 at the soil depth of 0.0, 0.5, 1.0, 3.0, 5.0 m. The maximum and minimum temperature in Pusan 3.7, $30.1^{\circ}C$ at soil surface and 14.3, $18.0^{\circ}C$ at the depth of 5.0 m. The total mean temperature of soil in Pusan and Chinju city was about 16.3, $16.0^{\circ}C$, respectively.

• 한국지열·수열에너지학회논문집
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• 제7권2호
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• pp.51-59
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• 2011

Storage and transfer heat in soils are governed by the soil thermal properties and these properties are therefore needed in many engineering applications, including horizontal ground heat exchanger for ground-coupled heat pumps. This paper presents the measured results of the thermal diffusivity of soils(silica, quartzite, limestone, sandstone, and masonry soils) used for the trench backfilling materials of the horizontal ground heat exchanger. To assess this thermal property, we (i) measure the soil thermal conductivities and volumetric heat capacities using dual-probe method and (ii) compare the estimates from the de Vries method of summing the heat capacities of the soil constituents. The results show that the thermal diffusivity tends to increase as dry soil begins to wet, but it approaches a constant value or even decreases as the soil continues to wet. Measurements made by using the dual-probe method agreed well with independent estimates obtained using the single-probe method.