• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.703-710
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• 2003

In the sub-surface environments, detection of the movement of contaminant substances and recharge of groundwater by rainfall are very important factors which contain porosity and effective porosity of porous media. In this paper, the applicability of permittivity methods and proposed dielectric mixing models (DDMs) are discussed. This study showed that the ratio of effective porosity to porosity of Toyoura and River sands were 0.856 and 0.843. From the relationships between the relative porosity and effective porosity, all measured values can be confirmed to outside the range to about 0.800 for Toyoura and River sands under all experiments by FDR and FDR-V systems. In the study, this permittivity equipment can be considered to be good enough to measure determining the physical parameters of saturated soils. Consequently, this permittivity method can be contributed to estimate a porosity and effective porosity of saturated porous media because it is easy and instantaneous than previous in-situ methods.

• 지질공학
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• 제14권2호
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• pp.169-177
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• 2004

포화 및 불포화 상태로 이루어진 지반 내에서 지하수의 함량 및 오염물질의 침투 이동은 지반을 구성하고 있는 다공질 매질의 공극률과 유효공극률에 매우 큰 영향을 받는다. 본 연구는 불포화 매질에 대한 유효공극률을 측정하기 위해서 Frequency domain reflectometry(FDR) system 및 측정센서를 개발하여 실내실험을 수행하였다. 또한 측정된 유전율상수의 관계로부터 유효공극률을 산정할 수 있는 유전을 믹싱모델(dielectric mixing model)을 제안하였다. 실험결과에서 불포화 흙 시료인 표준사(standard sand)와 강모래(river sand)의 유효공극률의 범위는 공극률과 비교해 약 65∼85% 내외에서 측정되었다. 특히, 측정된 유효공극률과 공극률의 관계에서 공극률이 증가할수록 유효공극률은 다소 감소하는 경향을 보이는 것으로 측정되었다. 이는 흙 입자사이의 공극 내에 존재하는 미량의 공기에 의한 것으로써 불포화 상태의 흙 칼럼이 충분히 포화 상태에 도달하지 못하였기 때문이다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.354-361
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• 2005

Physical parameters such as porosity and effective porosity are important physical parameters that determine the transfer and movement of water and solutes in porous media. Various methods of determining these parameters have been developed, with varying degrees of accuracy and applicability. Most of the existing methods produce static results. They do not produce instantaneous and real time of porosity and effective porosity in a porous media. In this study, a new permittivity method called Frequency Domain Reflectometry with Vector analyzer (FDR-V) is proposed to determine the porosity and effective porosity of some sand samples in the laboratory. The advantage of the FDR-V method is that it instantaneously determines the temporal variation of dielectric constants of porous media. Then, the porosity and the effective porosity of porous media are computed using well established empirical equations. Results obtained from the FDR-V method compared favorably with results from other permittivity methods such as gravimetric, injection and replacement tests. The ratio of effective porosity to porosity was $85{\sim}92%$, when FDR-V was used. This value compared favourably with 90%, which has been usually quoted in previous studies. Considering the convenience and its applicability, the measurement system of FDR-V permittivity holds a great potential in porous media and contaminant transport studies.

• 지질공학
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• 제13권4호
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• pp.419-428
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• 2003

지반을 대상으로 지하수의 이동 및 오염물질 침투에 대한 평가를 위해, 지반을 구성하고 있는 매질의 공극률과 유효공극률을 파악하는 것은 매우 중요하다. 이들은 물질 이동을 결정하는 중요한 물리적 파라메터이다. 본 연구에서는 새로운 유전율 시스템인 FOR-V (Frequency domain reflectometry with vector network analyzer)를 적용하여 표준사 (Standard sand)와 강모래 (River sand)에 대한 공극률 및 유효공극률을 측정하기 위한 실험적 연구를 실시하였다. 또한, 이들을 측정하기 위해, 다공질 매질에 대한 유전율상수의 특성을 고려한 유전율 믹싱모델 (dielectric FDR-V 시스템을 적용한 주입실험 (Injection test)과 주입물질의 농도를 측정하는 치환실험 (Replacement test)을 수행하였다. 두 종류의 실험 결과치를 비교한 결과, 측정된 유효공극률을 공극률과 비교해 보면, 약 85 - 92 %의 범위 내에 존재하는 것으로 측정되었다. 일반적인 흙의 유효공극률은 공극률에 대해 약 90 % 범위 내에 분포하고 있는 것으로 알려져 있으나, 본 연구에서는 다소 낮은 결과치를 보이고 있다. 이러한 현상은 시스템의 측정 프로브의 측정 범위가 직경 0.36 cm의 동축측정프로브 끝부분에서 이루어져 비교적 작기 때문에 제작된 흙 시료전 체적에 대한 유효공극률의 결과치이기 보다는 프로브가 위치한 지점에 대한 측정치로 판단된다. 이러한 측정 프로브의 특성을 고려해 볼 때, FDR-V 시스템은 연구자가 의도한 연구에 따라 특정 지점에 대한 지반의 정밀한 물리적 특성을 파악할 수 있을 것으로 사료된다.

• 설비공학논문집
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• 제11권2호
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• pp.185-192
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• 1999

Effective thermal conductivities and pressure-drop-related properties of aluminum foam metals have been measured. The effects of porosity and cell size in the aluminum foam metal are investigated in detail. The porosity of the foam metal, considered in the present study, varies from 0.89 to 0.96 and the cell size from 0.65㎜ to 2.5㎜. The effective thermal conductivity is evaluated by comparing the temperature gradient of the foam metal with that of the thermal conductivity-known material. The pressure drop in the foam metal is measured by a highly precise electric manometer while air is flowing through the aluminum foam metal in the channel. The results obtained indicate that the effective thermal conductivities are found to be increased with a decrease in the porosity while the effective thermal conductivities ire little affected by the cell size at a fixed porosity. However, the pressure drop is strongly affected by the cell size as well as the porosity. It is seen that the pressure drop is increased as the cell size becomes smaller, as expected. The minimum pressure drop is obtained in the porosity 0.94 at a fixed cell size. A new correlation of the pressure drop is proposed based on the permeability and Ergun's coefficient for the aluminum foam metal.

• Journal of Mechanical Science and Technology
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• 제19권12호
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• pp.2224-2230
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• 2005

In this study, the validity of the Eshelby-type model for predicting the effective Young's modulus and in-plane Poisson's ratio of the 2-dimensional perforated plate has been investigated in terms of the porosity size and its arrangement. The predicted results by the Eshelby-type model are compared with those by finite element analysis. Whenever the ratio of the porosity size to the specimen size becomes smaller than 0.07, the effective elastic constants predicted by finite element analysis are convergent regardless of the arrangement of the porosities. Under these conditions, the effective Young's moduli of the perforated plate can be predicted within the accuracy of $5\%$ by the Eshelby-type model, which overestimates and underestimates the effective Poisson's ratios by $10\%\;and\;6\%$ for the plates with periodically and non-periodically arranged porosities, respectively.

• International Journal of Air-Conditioning and Refrigeration
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• 제10권2호
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• pp.72-78
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• 2002

Woven wire wick is a very effective structure because of its easiness to insert inside of pipe for a miniature heat pipe. The present study was conducted to predict the porosity and the effective thermal conductivity of liquid-saturated woven wire wick. The porosity and the effective thermal conductivity of the evaporator region indicate different values from those of the condenser region due to the existence of non-flow region. The minimum value of the effective thermal conductivity indicates on condition of the $\theta$=$45^{Wcirc}$ and the values of the effective thermal conductivity increases symmetrically centering around the minimum value. The values of the effective thermal conductivity in the evaporator region at the angle of $45^{Wcirc}$ indicate about 60~80% higher than those in the condenser region for various combinations of copper, and stainless with water and ethanol.

• 한국지하수토양환경학회지:지하수토양환경
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• 제22권3호
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• pp.27-41
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• 2017

This study dealt with the characteristics and the interrelations of hydrogeological parameters such as hydraulic conductivity, dispersivity and effective porosity of unconsolidated sediments for providing the basic data necessary for the planning of the management and preservation of groundwater quality in the Nakdong River Delta of Busan City, Korea. Groundwater quality in this area has been deteriorated due to seawater intrusion, agricultural fertilizer and pesticide, industrial wastewater, and contaminated river water. The physical properties (grain size distribution, sediment type, sorting) and aquifer parameters (hydraulic conductivity, effective porosity, longitudinal dispersivity) were determined from grain size analysis, laboratory permeability test and column tracer test. Among 36 samples, there were 18 Sand (S), 7 Gravelly Sand (gS), 5 Silty Sand (zS), 5 Muddy Sand (mS), and 1 Sandy Silt (sZ). Hydraulic conductivity was determined through a falling head test, and ranged from $9.2{\times}10^{-5}$ to $2.9{\times}10^{-2}cm/sec$ (0.08 to 25.6 m/day). From breakthrough curves, dispersivity was calculated to be 0.35~3.92 cm. Also, effective porosity and average linear velocity were obtained through the column tracer test, and their values were 0.04~0.46 and 1.06E-04~6.49E-02 cm/sec, respectively. Statistical methods were used to understand the interrelations among aquifer parameters of hydraulic conductivity, effective porosity and dispersivity. The relation between dispersivity and hydraulic conductivity or effective porosity considered the sample length, because dispersivity was affected by experimental scale. The relations between dispersivity and hydraulic conductivity or effective porosity were all in inverse proportion for all long and short samples. The reason was because dispersivity was in inverse proportion to the groundwater velocity in case of steady hydrodynamic dispersion coefficient, and groundwater velocity was in proportion to the hydraulic conductivity or effective porosity. This study also elucidated that longitudinal dispersivity was dependent on the scale of column tracer test, and all hydrogeological parameters were low to high values due to the sand quantity of sediments. It is expected that the hydrogeological parameter data of sediments will be very useful for the planning of groundwater management and preservation in the Nakdong River Delta of Busan City, Korea.

• 지구물리와물리탐사
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• 제15권4호
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• pp.163-176
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• 2012

진공 수포화 과정에서 진공시간과 진공압력을 달리하면서 진공시간 및 압력이 유효공극률 산정에 미치는 영향을 살펴보았다. 시멘트와 모래의 무게비가 1대1인 3개의 시멘트 시험편과 100% 시멘트 모르타르 3개 등 총 6개 시험편을 이용하여 진공 압력을 2, 4, 6, 8, 10 torr, 진공시간을 20, 40, 60, 80, 100분으로 달리하며 측정되는 유효공극률을 비교하였다. 평균 약 25%와 40%로 비교적 큰 유효공극률을 갖는 시멘트 시험편에 대하여 진공압력이 10, 6, 2 torr 일 때 진공시간이 100 ~ 20 분으로 변화하는 3개 시험군 끼리의 결과를 비교하면, 절대편차의 평균값이 0.6%에서부터 0.5%, 0.2%로 작게 나타났다. 진공시간이 100, 60, 20분일 때 진공압력을 각각 2 ~ 10 torr로 변화시키면서 수행한 실험군 끼리의 유효공극률을 비교해도 진공시간이 짧아지면 절대편차의 평균값이 커지는 경향이 있었다. 이로부터 진공압력/진공시간에 관한 국제암반역학회(ISRM) 표준(제안)시험법의 "6 torr 이하/1시간 이상"의 단서로 유추할 수 있었다. 동일한 진공압력에서 진공시간이 20분씩 줄어들 때의 효과와 동일한 진공시간일 때 진공압력이 2 torr씩 낮아질 때의 효과를 정성적으로 밖에 확인할 수 없었는데 그 이유로 습식진공으로 포화된 시험편 내 수분이 $105^{\circ}C$ 오븐 내에서의 건조과정 후에도 완전히 건조되지 않아서 시험편의 초기 함수정도를 동일하게 할 수 없기 때문임을 밝혔다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2006년도 총회 및 춘계학술발표회
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• pp.411-414
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• 2006

This study was examined to determine hydraulic conductivity of vadose zone($K_s$) and effective porosity(${\phi}_e$) of undisturbed soil profiles collected at each vadose zone of 6 study areas in South Korea. Effective porosity was approximately 19% of total porosity for each soil profile. Applied to Ahuja's equation, the correlation between $K_s$ and ${\phi}_e$ showed $y=1.3{\times}10^{-7}x^{2.15}(r^2=0.37)$ for total soil profiles. Although the small numbers of soil profile were used for this study, the result of this study might be used for other soil hydraulic studies as reasonable data.