• 한국지반공학회논문집
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• 제18권3호
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• pp.105-112
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• 2002

성토하부 연약지반에서 상재하중의 변화가 없는 상태에서 과잉간극수압의 증가가 Berthierville와 Olga 지역에서 보고되었다. 이와같은 비정상적인 현상들을 고전적인 압밀이론으로 설명하기는 어렵다. 본 논문은 비선형 점소성모델윽 사용하여 자연점토지반에서 유발되는 간극수압 증가를 설명하였다. 제안된 모델은 Darcy 법칙에 의한 간극수압 소산과 점소성 변형에 의한 간극수압 생성에 대한 복합적인 거동을 모사할 뿐만 아니라 시간 의존적인 점소성 거동과 변형을 속도 의존적인 선행압밀하중 특성을 표현할 수 있다. 수치해석기법을 적용하여 Berthierville각 Olga 지역의 성토과정을 해석하였으며, 수치해석 결과와 계측된 값을 비교한 결과 제안된 비선형 점소성모델볶 사용하여 성토가 끝난 직후 간극수압의 증가현상을 설명할 수 있다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.890-897
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• 2005

Stability of embankment is influenced on landfill condition, permeability, shear strength and soil engineering propensity and so on, and need examination in reply because is different according to change of soil property of foundation ground and permeability condition. Analyzed seepage behaviour by finite element method for embankment, and change permeability of base to analyze effect that permeability of ground water table formation before embankment and analyze seepage behaviour to typical embankment in this research. In the case of permeability of foundation ground is 10 more than landfill permeability, rise of groundwater table was changed slightly. Pore water pressure was decreased slowly in landfill after rainfall. The effect of permeability of foundation ground was effected in change of pore water pressure. For permeability of foundation ground is 10 more than landfill, stability of road landfill was small changed during rainfall. But in the case of permeability of base soil similar to landfill permeability, road landfill stability was large decreased during rainfall.

• 한국해양공학회지
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• 제30권6호
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• pp.505-519
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• 2016

If the seabed is exposed to high waves for a long period, the pore water pressure may be excessive, making the seabed subject to liquefaction. As the water pressure change due to wave action is transmitted to the pore water pressure of the seabed, a phase difference will occur because of the fluid resistance from water permeability. Thus, the effective stress of the seabed will be decreased. If a composite breakwater or other structure with large wave reflection is installed over the seabed, a partial standing wave field is formed, and thus larger wave loading is directly transmitted to the seabed, which considerably influences its stability. To analyze the 3-D dynamic response characteristics of the seabed around a composite breakwater, this study performed a numerical simulation by applying LES-WASS-3D to directly analyze the wave-structure-soil interaction. First, the waveform around the composite breakwater and the pore water pressure in the seabed and rubble mound were compared and verified using the results of existing experiments. In addition, the characteristics of the wave field were analyzed around the composite breakwater, where there was an opening under different incident wave conditions. To analyze the effect of the changed wave field on the 3-D dynamic response of the seabed, the correlation between the wave height distribution and pore water pressure distribution of the seabed was investigated. Finally, the numerical results for the perpendicular phase difference of the pore water pressure were aggregated to understand the characteristics of the 3-D dynamic response of the seabed around the composite breakwater in relation to the water-structure-soil interaction.

• Geomechanics and Engineering
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• 제37권4호
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• pp.383-393
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• 2024

Monopile foundations of offshore wind turbines embedded in soft clay are subjected to the long-term cyclic lateral loads induced by winds, currents, and waves, the vibration of monopile leads to the accumulation of pore pressure and cyclic strains in the soil in its vicinity, which poses a threat to the safety operation of monopile. The researchers mainly focused on the hysteretic stress-strain relationship of soft clay and kinds of stiffness degradation models have been adopted, which may consume considerable computing resources and is not applicable for the long-term bearing performance analysis of monopile. In this study, a modified cyclic stiffness degradation model considering the effect of plastic strain and pore pressure change has been proposed and validated by comparing with the triaxial test results. Subsequently, the effects of cyclic load ratio, pile aspect ratio, number of load cycles, and length to embedded depth ratio on the accumulated rotation angle and pore pressure are presented. The results indicate the number of load cycles can significantly affect the accumulated rotation angle of monopile, whereas the accumulated pore pressure distribution along the pile merely changes with pile diameter, embedded length, and the number of load cycles, the stiffness of monopile can be significantly weakened by decreasing the embedded depth ratio L/H of monopile. The stiffness degradation of soil is more significant in the passive earth pressure zone, in which soil liquefaction is likely to occur. Furthermore, the suitability of the "accumulated rotation angle" and "accumulated pore pressure" design criteria for determining the required cyclic load ratio are discussed.

• 한국농공학회지
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• 제45권4호
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• pp.126-136
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• 2003

The B value on the saturated soil is commonly known as the amount of 1. Usually this concept is consistent with the condition that effective stress is equal to zero, but it was reported in some literatures that the B value was less than 1 in spite of saturated condition in the test of very stiff material such as rock and quasi-stiff material on which the stiffness can be mobilized because of effective stress not equal to zero. In this study the B value was measured on various effective stress conditions on normally consolidated clay. The test results in the B value less than 1 in spite of perfect saturation. The measured excessive pore water pressure was not only smaller than the change of the total stress, but also the function of time on clay.

• 한국농공학회지
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• 제38권1호
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• pp.79-89
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• 1996

It is expected that the soil hehaviours in the seahed subjected to cyclic wave loads are much different from that on the ground Cyclic shear stresses developed below the ocean bed as a result of a passing wave train may progressively build up pore pressure in certain soils. Such build-up pore pressure may be developed dynamic behaviour such as liquefaction and significant deformation of the seabed. Currently available analytical and testing methods for the seabed subjected to cyclic wave loads are not general. The purpose of the study are to provide a test method in laboratory and to analyse the mechanism of wave-induced stresses and liquefactions potentials of the unsaturated silty marine sand. It is showed that the test set-up made especially for this study delivers exactly oscillatory wave pressures of the form of sine function. Laboratory test results defining the cyclic shear strength of the unsaturated porous medium that is homogenously sedimented. It is understood that the pore water pressure due to induced-waves is not accumulated as the wave number increases but reveals periodical change on the still water surface. The magnitude of the pore water pressure tends to be attenuated radically with a certain time lag under the action of both high and low waves as depth increases.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.1140-1147
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• 2005

The objective of this study was to identify the effect of the degree of saturation on the resilient modulus of cohesive soils as subgrade. Six representative cohesive soils representing A-4, A-6, and A-7-6 soil types collected from road construction sites across Ohio, were tested in the laboratory to determine their basic engineering properties. Resilient modulus tests were conducted on unsaturated cohesive soils at optimum moisture content, and samples compacted to optimum conditions but allowed to fully saturate. The subgrade compacted at optimum moisture content may be fully saturated due to seasonal change. Laboratory tests on fully saturated cohesive soils showed that the resilient modulus of saturated soils decreased to less than half that of soil specimens tested at optimum moisture content. The reduction of resilient modulus would possibly be caused by the buildup of pore water pressure. In resilient modulus testing performed in this study on saturated samples, pore water pressure increases were observed. Pore water pressure and residual pore water pressure gradually increased with an increase in deviator stress.

• 한국지반환경공학회 논문집
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• 제9권1호
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• pp.33-40
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• 2008

본 연구는 강우시 토사사면의 침투거동 특성을 규명하기 위한 기초연구로서 강우재현장치를 활용하여 실내모형실험을 실시하여 유한사면내의 간극수압의 변화를 측정하였으며, 이를 바탕으로 강우지속시간에 따른 강우시 유한사면내의 침투거동 특성을 분석하였다. 분석결과 강우가 지속적으로 발생됨에 따라 사면내의 간극수압은 점차 증가하는 것을 알 수 있으며, 강우초기에는 사면 중앙부 표면에서 간극수압이 크고 강우가 점차 지속됨에 따라 사면내로 강우가 침투하여 사면붕괴 직전에는 사면내부의 간극수압이 크게 증가되는 것을 알 수 있었다. 본 연구에서 실시한 실내실험은 계측기의 민감도가 높고 조작이 용이하지 못하여 많은 실험결과를 얻지 못하였으며, 향후 다양한 사면경사에서의 유한사면에 대한 강우시 침투거동 특성에 대해 실험적 연구가 필요하다고 생각된다.

• 한국지반공학회논문집
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• 제19권4호
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• pp.15-21
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• 2003

본 연구는 풍화 화강토의 일정 간극비에서 초기함수비의 변화에 따른 거동 특성을 통상의 삼축압축시험기를 이용한 비배수시험을 실시하여 비배수전단시 불포화 풍화 화강토의 간극압, 체적변형 및 응력-변형률 거동특성을 밝히고자한다. 연구에 사용된 시료는 조립질의 풍화 화강토이고 직경 50mm 높이 100mm로 복층다짐하여 삼축 시험용 공시체를 제작하였다. 준비된 공시체를 구속압력과 흡인력($u_a-u_w$)을 각각 달리한 비배수 3축압축시험을 실시하였다. 그 결과 초기 함수비의 변화에 따라 내부마찰각($\phi'$)의 변화는 다소 있지만 흡인력의 변화에 따른 내부마찰각의 변화는 거의없고 유효점착력만이 증가하는 경향을 보이고 있다.

• 콘크리트학회논문집
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• 제20권2호
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• pp.131-138
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• 2008

물-결합재비가 낮은 고성능콘크리트의 자기건조에 의한 습도감소와 수축과의 연관성을 파악하기 위하여 물-결합재비 0.3, 0.4의 배합에 대하여 습도와 변형률을 측정하였다. 그 결과 물-결합재비 0.3의 콘크리트 내부 습도 감소는 약 10%, 수축변형률은 약 $320\times10^{-6}$을 나타내었고, 물-결합재비 0.4의 콘크리트의 경우 4%의 습도 감소와 $120\times10^{-6}$ 수축변형률을 나타내었으며 배합에 상관없이 습도와 변형률은 모두 강한 선형성을 보였다. 콘크리트 내부 습도 변화와 수축변형률의 관계를 보다 구체화하기 위하여 콘크리트 내부 공극을 단일 네트워크로 가정하고 확장 메니스커스 생성가정 하에 공극수에서 발생하는 모세관 압력과 수화조직체에서 발생하는 표면에너지 변화를 습도의 함수로 모델링하여 수축의 구동력으로 작용시킨 결과 실험값과 비교적 일치하는 값을 나타내었다. 이를 근거로 물-결합재비가 낮은 고성능 콘크리트에서 자기건조에 의한 습도감소는 20 nm 이하의 소형공극에서 발생함을 파악할 수 있었으며 따라서 자기수축에 대한 제어 방안은 이러한 소형공극에서의 공극수 표면장력과 포화도에 초점을 맞추어야 함을 확인할 수 있었다.