• Geomechanics and Engineering
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• 제12권4호
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• pp.707-721
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• 2017

The objective of this paper is to experimentally study the consolidation of saturated silty clay subjected to repeated heating-cooling cycles using a modified temperature-controlled triaxial apparatus. Focus is placed on the influence of the water content, confining pressure, and magnitudes and number of thermal loading cycles. The experimental results show that the thermally induced pore pressure increases with increasing water content and magnitude of thermal loading in undrained conditions. After isothermal consolidation at an elevated temperature, the pore pressure continues to decrease and gradually falls below zero during undrained cooling, and the maximum negative pore pressure increases as the water content decreases or the magnitude of thermal loading increases. During isothermal consolidation at ambient temperature after one heating-cooling cycle, the pore pressure begins to rise due to water absorption and finally stabilizes at approximately zero. As the number of thermal loading cycles increases, the thermally induced pore pressure shows a degrading trend, which seems to be more apparent under a higher confining pressure. Overall, the specimens tested show an obvious volume reduction at the completion of a series of heating-cooling cycles, indicating a notable irreversible thermal consolidation deformation.

• 한국암반공학회:학술대회논문집
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• 한국암반공학회 2000년도 암반공학문제의 수치해석(Numerical Analysis in Rock Engineering Problems)
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• pp.105-115
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• 2000

방사성 폐기물지하처분이나 열수 및 축열 에너지저장, 지열에너지 개발 등과 같은 대규모 지하공간 프로젝트들이 대두됨에 따라 역학, 수리 및 열적 거동을 동시에 고려한 연구가 필요하게 되었다. 열-수리-역학 상호작용 해석은 열로 교란되고 지하수로 포화된 암반내의 거동을 열 수리, 역학 3가지 지배방정식의 결합을 통해 구현하는 상당히 복잡한 수치 해석 기법 중의 하나이다. 본 연구에서는 기존의 Biot의 압밀이론에 기초한 수식화들을 이용하여 연속체 암반의 열-수리-역학적 상호작용을 모사할 수 있는 유한요소 프로그램을 개발하였다. 개발된 프로그램의 검증을 위해 등온과 비등온 조건하의 일차원 압밀모델에 대한 해석을 실시하여 해석해와 비교하였다. 이타원 압밀에 대한 변수해석을 통하여 포아송비나 수리적 이방성과 같은 인자들이 매체 거동에 미치는 영향을 조사하였다. 앞으로 본 프로그램에 개별체 절리 모델을 통합시켜 보다 일반적인 불연속 암반의 상호작용 거동 해석에 이용할 수 있을 것이다.

• 터널과지하공간
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• 제10권3호
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• pp.355-365
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• 2000

방사성 폐기물지하처분이나 열수 및 축열 에너지저장, 지열에너지 개발 둥과 같은 대규모 지하공간 프로젝트들이 대두됨에 따라 역학, 수리 및 열적 거동을 동시에 고려한 연구가 필요하게 되었다. 열-수리-역학 상호작용 해석은 열로 교란되고 지하수로 포화된 암반내의 거동을 열, 수리, 역학 3 가지 지배방정식의 결합을 통해 구현하는 상당히 복잡한 수치 해석 기법 중의 하나이다. 본 연구에서는 기존의 Biot의 압밀이론에 기초한 수식화들을 이용하여 연속체 암반의 열-수리-역학적 상호작용을 모사할 수 있는 유한요소 프로그램을 개발하였다. 개발된 프로그램의 검증을 위해 등온과 비등온 조건하의 일차원 압밀모델에 대한 해석을 실시하여 해석해와 비교하였다. 이차원 압밀에 대한 변수해석을 통하여 포아송비나 수리적 이방성과 같은 인자들이 매체 거동에 미치는 영향을 조사하였다. 앞으로 본 프로그램에 개별체 절리 모델을 통합시켜 보다 일반적인 불연속 암반의 상호작용 거동 해석에 이용할 수 있을 것이다.

• 한국분말재료학회지
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• 제7권4호
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• pp.237-243
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• 2000

The property and performance of the $Al_2O_3/Ni$ nanocomposites have been known to strongly depend on the structural feature of Ni nanodispersoids which affects considerably the structure of matrix. Such nanodispersoids undergo structural evolution in the process of consolidation. Thus, it is very important to understand the microstructural development of Ni nanodispersoids depending on the structure change of the matrix by consolidation. The present investigation has focused on the growth mechanism of Ni nanodispersoids in the initial stage of sintering. $Al_2O_3/Ni$ powder mixtures were prepared by wet ball milling and hydrogen reduction of $Al_2O_3$ and Ni oxide powders. Microstructural development and the growth mechanism of Ni dispersion during isothermal sintering were investigated depending on the porosity and structure of powder compacts. The growth mechanism of Ni was discussed based upon the reported kinetic mechanisms. It is found that the growth mechanism is closely related to the structural change of the compacts that affect material transport for coarsening. The result revealed that with decreasing porosity by consolidation the growth mechanism of Ni nanoparticles is changed from the migration-coalescence process to the interparticle transport mechanism.

• 한국재료학회지
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• 제11권12호
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• pp.1068-1073
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• 2001

An n-type iron$silicide(Fe_{0.98}Co_{0.02}Si_2)$has been produced by mechanical alloying process and consolidated by vacuum hot pressing. Although as-milled powders after 120 hours of milling did not show an alloying progress,${\beta}-FeSi_2$phase transformation was induced by isothermal annealing at$830{\circ}C$for 1 hour, and the fully transformed${\beta}-FeSi_2$phase was obtained after 4 hours of annealing. Near fully dense specimen was obtained after vacuum hot pressing at$ 1100{\circ}C$with a stress of 60MPa. However, as-consolidated iron silicides were consisted of untransformed mixture of ${\Alpha}-Fe_2Si_5$and ${\varepsilon-FeSi$phases. Thus, isothermal annealing has been carried out to induce the transformation to a thermoelectric semiconducting${\beta}-FeSi_2$phase. The condition for${\beta}-FeSi_2$transformation was investigated by utilizing DTA, SEM, and XRD analysis. The phase transformation was shown to be taken place by a vacuum isothermal annealing at$830{\circ}C$and the transformation behaviour was investigated as a function of annealing time. The mechanical properties of${\beta}-FeSi_2$materials before and after isothermal annealing were characterized in this study.

• 한국표면공학회지
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• 제36권2호
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• pp.200-205
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• 2003

Thermoelectric p-type $Fe_{0.98}$ $Mn_{ 0.02}$$Si_2$ bulk specimens have been produced by mechanical alloying and consolidation by vacuum hot pressing. The subsequent isothermal annealing was not able to fully transform the mestastable as -milled powders into the $\beta$ $-FeSi_2$ phase, so that the obtained matrix consisted of not only thermoelectric semiconducting $\beta$-FeSi$_2$ but also some residual, untransformed metallic $\alpha$ $- Fe_2$$Si_{ 5}$ and $\varepsilon$-FeSi mixtures. Interestingly, $\beta$ - $FeSi_2$ was more easily obtained in the low density specimen when compared to the high density specimen. The oxidation at 700 and $800^{\circ}C$ in air led to the phase transformation of the above described iron - silicides and the formation of a thin silica surface layer.