• 한국신재생에너지학회:학술대회논문집
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• 2010.11a
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• pp.123.2-123.2
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• 2010

본 논문에서는 2008년 4월 이후 지열원 열펌프가 설치되어지는 현장에 시험공의 지중열전도도를 현장열응답법을 이용하여 측정하였으며, 그간에 측정된 지중열전도도를 이용하여 전국의 지중온도 및 지중열전도도의 산포도를 정리하였다. 지중열교환기의 심도가 150m일 때 지중온도 분포는 약 $12.0{\sim}19^{\circ}C$의 넓은 분포를 보였으나 대부분의 지중온도가 $15.0{\sim}17.0^{\circ}C$의 범위에 분포하였으며, 지중열전도도의 경우도 마찬가지로 1.50 ~ 9.00 W/mk 값으로 아주 넓은 분포를 보였으나 2.30 ~ 2.90W/mk 값이 가장 많이 나타냈다.

• Proceedings of the KIEE Conference
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• 2009.07a
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• pp.391_392
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• 2009

DTS 시스템에서 측정하는 분포온도 데이터는 지중케이블의 상태 감시에 유용하게 사용될 수 있다. 본 연구에서는 분포온도센서로부터 획득되는 온도 데이터를 기반으로 지중케이블의 상태 감시 및 실시간 허용용량을 산정할 수 있는 모니터링 시스템을 개발하였다. 본 시스템은 사례 기반의 모니터링 GUI를 구축하는 것을 지양하고, 임의의 지중케이블 시스템에 적용이 가능한 GUI 설정 기능을 갖추었으며, 케이블의 동적허용용량 산정 모듈, 분포온도 해석 모듈, 경보 모듈, 설정 모듈, 이력조회 모듈 등으로 구성된다.

• Korea Journal of Geothermal Energy
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• v.3 no.2
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• pp.3-10
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• 2007

• Journal of the Korean earth science society
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• v.26 no.1
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• pp.93-105
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• 2005

Climatological characteristics in the variation of soil temperatures in Korea were investigated using Korea Meterological Administration's observation data. And the impacts of soil moisture on the variation of soil temperature were examined using observed precipitation data. The climatological averages of soil temperatures are ranged from 14.4 to $15.0^{\circ}C$ regardless of depths. And they showed an latitudinal gradient with a warm temperature at the southern region and 'U' shape as in the air temperature with a high value along the coastal region. The relatively higher heat capacity and low conductivity of soil compared to those of the air resulted in the significant delay of the maximum and minimum date with depth. As a results, soil acts as a heat source during winter while a heat sink during summer. Global warming and urban heat island have increased the soil temperatures with an average rate $0.3\~0.5^{\circ}C/10-year$ as in the air temperature during last 30 years $(1973\~2002)$. However, the warming rate is maximized during spring contrary to the winter in the air temperature. The temporal variation of soil temperatures is strongly affected by that of soil moisture through an modification of the heat capacity and heat convection. In general, the increased soil moisture clearly decreased the temporal variations and increased the deep layer soil temperatures during cold season.

• 월간 기계설비
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• s.93
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• pp.60-75
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• 1998

지표면으로부터 일정한 깊이 이하의 토양이 보유하고 있는 지열에너지는 에너지자원을 절약하기 위해서는 매우 유용한 에너지원이 될 수도 있다. 따라서 지중에너지를 활용하기 위한 지중온도분포에 대한 해석과 그 활용면에서 도로 융설시스템 및 건물의 냉난방의 에너지원으로 이용할 수 있는 에너지절약 방안에 대한 연구개발이 추진되고 있다.

• Proceedings of the KIEE Conference
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• 2015.07a
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• pp.422-423
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• 2015

현재 허용전류는 가장 열악한 조건과 여유분을 주어 계산하기 때문에 지중 송전 케이블의 실제 송전용량은 설계보다 상당히 큰 용량을 사용할 수 있다. 송전용량을 증대시키는 방법 중 하나로 DRS(Dynamic Rating System)를 도입하는 방법이 떠오르고 있다. DRS는 이미 상용화 되어있으나 지중관로의 경우 기존에 포설되어 있는 케이블에 DTS를 설치하기가 곤란하여 관로조건에서는 동적 허용전류를 산정하기에 어려움이 있다. 따라서 본 논문에서는 DTS 계측자료를 이용하여 보정계수법을 통한 허용전류 산정 방법론을 제안한다. 또한 지중관로의 맨홀부에서 측정한 케이블의 표면 온도를 이용하여 관로 내 케이블의 분포 표면 온도를 추정하고 보정계수를 통한 허용전류를 산정하는 방법론을 제안한다.

• 한국신재생에너지학회:학술대회논문집
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• 2006.06a
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• pp.431-433
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• 2006

Accurate information on the ground surface temperature is essential for design of a borehole heat exchanger and thus ensuring the performance of a ground source heat pump system along with knowledge on thermal diffusivity and conductivity of ground. In this study we analyzed the shallow subsurface temperature monitoring data of 58 Korea Meteorological Administration synoptic stations. As a result, we compiled mean annual ground surface temperature distribution map using multiple regression analysis of the monitoring data.

• Korean Journal of Soil Science and Fertilizer
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• v.37 no.3
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• pp.131-135
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• 2004

This study was carried out for the analysis of temperature characteristics on soil surface using soil heat flux which is one of the important parameters forming soil temperature. Soil surface temperature was estimated by using the soil temperature measured at 10 cm soil depth and the soil heat flux measured by flux plate at 5 cm soil depth. There was time lag of two hours between soil temperature and soil heat flux. Temperature changes over time showed a positive correlation with soil heat flux. Soil surface temperature was estimated by the equation using variable separation method for soil surface temperature. Arithmetic mean using temperatures measured at soil surface and 10 cm depth, and soil temperature measured at 5 cm depth were compared for accuracy of the value. To validate the regression model through this comparison, F-validation was used. Usefulness of deductive regression model was admitted because intended F-value was smaller than 0.001 and the determination coefficient was 0.968. It can be concluded that the estimated surface soil temperatures obtained by variable separation method were almost equal to the measured surface soil temperature.

• 한국신재생에너지학회:학술대회논문집
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• 2007.11a
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• pp.477-480
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• 2007

Inlet fluid temperature of the BRE in the geothermal heat pump system depends on heat exchange rate between the refrigerant of the heat pump and the leaving fluid from the BRE. Because the outlet fluid temperature of the BHE varies with time, inlet fluid temperature has to vary with time. In this study, the module to calculate inlet fluid temperature is developed, which can consider the time-varying outlet fluid temperature and the heat exchange capacity of the heat pump. It is assumed that heat loss or gain of the leaving fluid from outlet to inlet of the BHE is negligible, except when the fluid contacts with the refrigerant of the heat pump. This module is combined with TOUGHREACT, a widely accepted three-dimensional numerical simulator for heat and water flow and geochemical reactions in geothermal systems and is applied to data analyses of the thermal response test.

• Geophysics and Geophysical Exploration
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• v.21 no.2
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• pp.82-93
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• 2018

Resistivity monitoring data at embankment dams are affected by the seasonal temperature variation. Especially when the seasonal temperature variation is large like Korea, the temperature effects may not be ignored in the longterm resistivity monitoring. Therefore, temperature effects can make it difficult to accurately interpret the resistivity monitoring data. In this study, through analyzing the time series of ground temperature collected at an embankment dam, ground temperature variations are calculated approximately. Then, based on the calculated temperature profile with depth, the inverted resistivity model of the embankment dam is corrected to remove the temperature effects. From these corrections, it was confirmed that the temperature effects are significant in the upper, superficial part of the dam, but can be ignored at depth. However, temperature correction based only on the temperature distribution in the dam body cannot remove the temperature effect thoroughly. To overcome this problem, the effect of temperature variation in the reservoir water seems to be incorporated together with the air temperature variation.