• 한국토양비료학회지
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• 제45권1호
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• pp.1-8
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• 2012

The thermal properties including volumetric heat capacity, thermal conductivity, thermal diffusivity, and diurnal and annual damping depths of 10 representative soil series of Korea were calculated using some measurable soil parameters based on the Taxonomical Classification of Korean Soils. The heat capacity of soils demonstrated a linear function of water content and ranged from 0.2 to $0.8cal\;cm^{-3}^{\circ}C^{-1}$ for dry and saturated medium-textured soil, respectively. A small increase in water content of the dry soils caused a sharp increase in thermal conductivity. Upon further increases in water content, the conductivity increased ever more gradually and reached to a maximum value at saturation. The transition from low to high thermal conductivity occurred at low water content in the soils with coarse texture, and at high water content in the other textures. Thermal conductivity ranged between $0.37{\times}10^{-3}cal\;cm^{-1}s^{-1}^{\circ}C^{-1}$ for dry (medium-textured) soil and $4.01{\times}10^{-3}cal\;cm^{-1}s^{-1}^{\circ}C^{-1}$ for saturated (medium/coarse-textured) soil. The thermal diffusivity initially increased rapidly with small increases in water content of the soils, and then decreased upon further increases in the soil-water content. Even in an extreme soil with the highest diffusivity value ($1.1{\times}10^{-2}cm^2s^{-1}$), the daily temperature variation did not penetrate below 70 cm soil depth and the yearly variation not below 13.4 m as four times of damping depths.

• 대한토목학회논문집
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• 제32권2C호
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• pp.69-77
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• 2012

일반적으로 지열 에너지파일 및 수평형 지열교환기는 기존의 연직형 지열히트펌프에 비하여 지표면에서 가까운 깊이에 설치되며, 이 경우 지열교환기의 열 교환 거동은 토사층에서의 열전도도에 많은 영향을 받게 된다. 기존의 연구에 따르면 지하수위 상부에 놓인 흙의 열전도도는 에너지파일의 열 교환 성능에 많은 영향을 미치는 것으로 알려져 있으며, 이는 부분적으로 포화된 흙의 열전도도는 함수비에 큰 영향을 받기 때문이다. 본 연구에서는 국내에 널리 분포하고 있는 화강풍화토의 열전도도 예측에 대한 연구를 수행하였다. 5개 지역에서 채취한 화강풍화토 시료의 간극율과 포화도를 바꾸어가며 탐침법 기반 열전도도 측정시험을 수행하였고, 기존의 열전도도 추정 모델들의 적합성을 평가하였다. 마지막으로 국내 화강풍화토에 적합한 경험적 예측식을 제안하고 이를 토대로 실험자료를 분석해 보았으며 기존 문헌에 실린 실험결과에 적용하여 그 적절성을 살펴보았다.

• 한국지열·수열에너지학회논문집
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• 제8권1호
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• pp.21-31
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• 2012

This paper reviewed and evaluated some of the commonly used prediction models for thermal conductivity of soils with the experimental data. Semi-theoretical models for two-component materials were found inappropriate to estimate the thermal conductivity of dry state soils. It came out that the model developed by Cote and Konrad gave the best overall prediction results for unsaturated soils available in the literature. However, it still needs to be improved to cover a wider range of soil types and degrees of saturation. In the present study, parametric analysis is also conducted to investigate the effect of soil type and moisture content on the horizontal ground heat exchanger design. The analysis shows that horizontal ground heat exchanger pipe length is reduced with the increase of soil thermal conductivity and water content. The calculation results also show that horizontal ground heat exchanger size can be reduced to a certain extent by using backfilling material with a higher thermal conductivity of solid particles.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2010년도 추계 학술발표회
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• pp.813-824
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• 2010

Thermal conductivity of soils is one of the most important parameters to design horizontal ground heat exchangers. It is well known that the thermal conductivity of soil is strongly influenced by its density and water content because of soil's particulate structure. This paper reviewed and evaluated some of the commonly used prediction models for thermal conductivity of soils with the experimental data available in the literature. Semi-theoretical models for two-component materials were found inappropriate to estimate the thermal conductivity of dry state sands. It came out that the model developed by Cote and Konrad gave the best overall prediction for unsaturated sands available in the literature. Also, a parametric analysis is conducted to investigate the effect of thermal conductivity and water content, soil type on the horizontal ground heat exchanger design. The analysis shows that a required pipe length for the horizontal ground heat exchanger is reduced with the increase of soil thermal conductivity and water content. The calculation results also show that the dimension of the horizontal ground heat exchanger can be reduced to a certain extent by using backfilling material with a higher thermal conductivity of solid particles.

• 한국지반공학회논문집
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• 제39권9호
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• pp.5-11
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• 2023

지반구조물의 해석에 있어서 해석의 고려 대상과 분야가 점점 다변화되고 있으며, 특히 지반동결과 관련된 분야에서 지반재료의 열적거동 특성에 대한 예측의 필요성이 중요해지고 있다. 신뢰성 있는 지반의 동결거동 평가를 위해서는 다양한 조건에서의 시료의 유효 열전도도 변화에 대한 고려가 필요하다. 본 논문에서는 시료의 간극률, 초기 포화도, Read time 설정을 달리하여 탐침 실험을 수행하였고, 이를 통해 동결 사질토의 유효 열전도도에 영향을 미치는 인자들을 평가하였다. 서로 다른 간극률 조건에서 실험을 수행한 결과, 시료의 간극률이 작을수록 동결토의 유효 열전도도는 증가하는 경향이 나타났다. 반면, 시료의 포화도가 증가할수록 동결토의 유효 열전도도는 증가하였다. 유효 열전도도 측정에 대한 계측기 Read time 설정의 민감도가 존재하였는데, Read time을 1분으로 설정하여 측정하였을 때 측정값의 범위가 국내의 선행연구결과와 유사하게 나타났다.

• 한국태양에너지학회 논문집
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• 제32권5호
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• pp.68-74
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• 2012

Investigation of the effective soil thermal conductivity($k$) is the first step in designing the ground loop heat exchanger(borehole) of a geothermal heat pump system. Another important factor is the borehole thermal resistance($R_b$). Thermal response tests offer a good method to determine the ground thermal properties for the total heat transport in the ground. The first step is measured for initial soil temperature. This is done by supplying a only pump power into a borehole heat exchanger. They need to supply into water unload heat power more than 30 minutes. In this study, the initial soil temperature was found to analysis $14.1{\sim}16.0^{\circ}C$,the ratio was 68.7% represented. In this case of $k$, was 2.1~3.0 $W/m{\cdot}k$, $R_b$ was 0.11~0.20 $m{\cdot}K/W$. In this work, it is also shown that the distribution of a soil thermal conductivity and borehole thermal resistance were on the influence of initial soil temperature. And soil thermal conductivity was related with factors of equation by linear least square method, borehole thermal resistance was on the influence of composite factors.

• 한국군사과학기술학회지
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• 제18권2호
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• pp.125-130
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• 2015

Vehicles and UGV(Unmanned Ground Vehicle) need a variety of road informations, such as road profile, soil type and soil water contents, to run a cross country course. Especially, soil water contents are very important factor to judge the vehicle mobility, because it can change soil strength. This paper describes the real-time measuring method of soil water contents by using the soil thermal conductivity.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2000년도 봄 학술발표회 논문집
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• pp.548-555
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• 2000

It was investigated whether the waste polyethylene chips can be recycled as construction materials in geotechnical engineering field. The standard Proctor test, the hydraulic conductivity test, the large box direct shear test, the thermal conductivity test, the frost heaving test and the time domain reflectometry test were performed on weathered granite soil mixed with variable amount of the waste polyethylene chips. The experimental results showed that the hydraulic conductivity and the shear strength of weathered granite soil increase with increasing the amount of the waste polyethylene chips. On the other hand, the thermal conductivity, the amount of frost heaving and the unfrozen water contents of weathered granite soil decrease with increasing the amount of the waste polyethylene chips.

• 한국지반공학회논문집
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• 제29권2호
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• pp.5-14
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• 2013

지중 토양의 열 물리적 성질 중 열전도도(thermal conductivity)는 지열 히트펌프 시스템(ground-coupled heat pump systems)의 지중열교환기 설계 과정에서 매우 중요한 변수다. 토양의 열전도도는 3상 구조로 인해 함수비와 건조밀도의 영향을 많이 받는다. 본 논문에서는 수평형 지중열교환기의 트렌치 뒤채움재로 사용되는 9종류의 토양(모래-물혼합물)을 대상으로 열전도도 측정결과와 기존 상관식에 의한 계산결과를 비교하였다. 건조토인 경우, 2상 구조의 열전도도 예측모델인 준이론 모델에 의한 열전도도 계산 결과는 측정 결과와 큰 차이를 보였다. 불포화토인 경우, 기존 모델 중 Cote와 Konrad가 제시한 모델에 의한 계산 결과가 측정 결과와 가장 잘 일치하였다. 또한 토양의 열전도도와 함수비, 종류 등이 수평형 지중열교환기의 설계 길이에 미치는 영향을 고찰하였다. 뒤채움재로 사용되는 토양의 열전도도가 증가할수록 수평형 지중열 교환기의 설계 길이는 감소하였다.

• 설비공학논문집
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• 제17권2호
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• pp.173-182
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• 2005

The Performance of U-tube ground heat exchanger for geothermal heat Pump systems depends on the thermal properties of the soil, as well as grout or backfill materials in the borehole. In-situ tests provide a means of estimating some of these properties. In this study, in-situ thermal response tests were completed on two vertical boreholes, 130 m deep with 62 mm diameter high density polyethylene U-tubes. The tests were conducted by adding a monitored amount of heat to water over a $17\~18$ hour period for each vertical boreholes. By monitoring the water temperatures entering and exiting the loop and heat load, overall thermal conductivity values of grout/soil formation were determined. Two parameter estimation models for evaluation of thermal response test data were compared when applied on the same temperature response data. One model is based on line-source theory and the other is a numerical one-dimensional finite difference model. The average thermal conductivity deviation between measured data and these models is of the magnitude $1\%$ to $5\%$.