• 한국지반공학회지:지반
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• 제2권1호
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• pp.15-26
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• 1986

포화된 정규압밀 점토가 비배수 전단을 받을 때 흙 속에 발생하는 과열간극수압과 변형의 관계를 밝히기 위하여 두개의 재성형 점토와 한개의 비휴선 시료를 사용하여 압밀-비배수 삼축위축 시험을 시행하였다. 시험은 등방일정규압밀된 시료이 열색 표준 삼축타축 시험으르 변형 제어와 응력 제어 방식에 의하여 수행되었으며, 시험 결과로 부터 전단중의 과잉간변수압과 변형의 관계를 표현 할 수 있는 쌍유선 함수를 찾아내었다. 이 쌍곡선함수는 응력일변형 거동에 대한 Kondner의 쌍곡선 모형과 같은 형태의 함수이며 이 함점니 사용되는 두 개의 계수는 삼축압축 시험(CU)으로부터 구해진다.

• Geomechanics and Engineering
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• 제9권5호
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• pp.669-685
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• 2015

A three-dimensional elastoplastic constitutive model, also known as a UH model (Yao et al. 2009), was developed to describe the stress-strain relationship for normally consolidated and over-consolidated soils. In this paper, an acoustic tensor and discriminator of bifurcation for the UH model are derived for the strain localization of saturated clays under undrained and fully and partially drained conditions. Analytical analysis is performed to illustrate the points of bifurcation for the UH model with different three-dimensional stress paths. Numerical analyses of cubic specimens for the bifurcation of saturated clays under undrained and fully and partially drained conditions are conducted using ABAQUS with the UH model. Analytical and numerical analyses show the similar bifurcation behaviour of overconsolidated clays in three-dimensional stress states and various drainage conditions. The results of analytical and numerical analyses show that (1) the occurrence of bifurcation is dependent on the stress path and drainage condition; and (2) bifurcation can appear in either a strain-hardening or strain-softening regime.

• 한국지반공학회지:지반
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• 제9권4호
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• pp.27-36
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• 1993

본 연구에서는 실트흙의 거동에 대하여 자동화된 삼축시험기를 사용하여 정하중(monotonic loading)과 반복 동하중(cyclic loading)하에서 파괴전과 파괴상태시 응력 변형률 상태를 제시하였다. 시료성형을 위하여 순수 실트인 실리카 분말을 사용했으며 시료는 조밀한 경우(D,=80%, eo=0.68)와 느슨한 경우(D,=35pl, eo=0.9)의 2종류로 만들어 등방 압밀후 배수. 비배수 상태하 에서 삼축압축과 인장시험을,비배수 상태하에서 반복 동하중 시험을 하였다. 해석 결과 전반적인 실트의 거동은 사질토와 비슷하지만 점토질흙에 비해서는 체적팽창(dilatancy)으로 인하여 정하중과 반복동하중하에서 상당히 다른 거동을 보임을 알 수 있었다.

• 한국농공학회지
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• 제36권3호
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• pp.74-83
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• 1994

A series of isotropic consolidation tests, undrained and drained triaxial compression tests was carried out to investigate the physical characteristics and behaviours of marine silty sands collected from the western coast of Korea. This study also included a theoretical development of the constitutive equation to evaluate stress-strain relationship and volume change of silty sands. The results and main conclusions of the study are summarized as follows; 1. Isotropic compression and swelling index are linearly decreased with an increase in relative density. 2. Both undrained shear strengh and elastic modulus are increased with an increase in relative density and confining pressure. 3. Internal friction angles obtained from drained and undrained compression tests of the soils are proportional to relative density. 4. The phenomenon of dilatancy of each sample is less profound when confining stress is increased but more profound when relative density is increased. 5. The slope of critical state lines is 1.78 for Saemangum, 1.70 for Siewha and 1.26 for Sukmoon sands. 6. In this study, Drucker-Praper type criterion is used and hardening function of Cap model is modified by hyperbolic fuction. This will improve a lack of physical meaning of hardening parameters in conventional Cap model. 7. A newly developed constitutive equation to the forementioned silty sands and checked its applicability. This is in good agreement with the measured data.

• 한국농공학회지
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• 제36권3호
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• pp.90-99
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• 1994

To investigate the undrained shear strength characteristics of marine soils with high water content, high compressibility and weak bearing capacity, a series of undrained triaxial tests with pore pressure measurements on undisturbed and disturbed Banwol marine clay in normally consolidated and overconsolidated states is carried out. The results and main conclusions of this study are summarized as follows : 1 . When the consolidation pressure is increased, the maximum deviator stress of disturbed and undistubed clay in normally consolidated state is increased. Pore pressure parameters and internal friction angle of undisturbed clay are greater than those of disturbed clay. 2. The relationship between pore pressure and axial strain of undisturbed clay in normally consolidated state can be expressed as a hyperbolic function like stress-strain relation proposed by Kondner. 3. In the pore pressure-axial strain relation of disturbed clay in normally consolidated state, failure ratio R'f is greatly deviated in the range of 0.7~0.9 proposed by Christian and Desai. 4. For overconsolided clay, when overconsolidation ratio (OCR) is increased, normalized maximum deviator stress is increased and maximum pore pressure is decreased gradually. 5. Cohesion of overconsolidated clay is greater than that of nomally consolidated clay and internal friction angle slightly is decreased. 6. Pore pressure parameter at failure (Af) of overconsolidated clay is varied with OCR, Af becomes negative values with increment in OCR

• Geomechanics and Engineering
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• 제9권6호
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• pp.729-742
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• 2015

The aim of the present work was the study of instability in a loose sand from Les Dunes beach in Ain Beninan, Algeria, where the Boumerdes earthquake occurred in 2003. This earthquake caused significant structural damages and claimed the lives of many people. Damages caused to infrastructures were strongly related to phenomena of liquefaction. The study was based on the results of two drained and six undrained triaxial tests over a local sand collected in a region where liquefaction occurred. All the tests hereby analyzed followed compression stress-paths in monotonic conditions and the specimens were isotropically consolidated, since the objective was to study the instability due to static loading as part of a more general project, which also included cyclic studies. The instability was modeled with the second-order work increment criterion. The definition of the instability line for Les Dunes sand and its relation with yield surfaces allowed the identification of the region of potential instability and helped in the evaluation of the susceptibility of soils to liquefy under undrained conditions and its modeling. The dilatancy rate was studied in the points where instability began. Some mixed tests were also simulated, starting with drained conditions and then changing to undrained conditions at different time steps.

• Geomechanics and Engineering
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• 제30권3호
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• pp.219-231
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• 2022

Geotechnical materials such as silt, fine sand, or coarse granular soils may be unstable under undrained shearing or during rainfall infiltration starting an unsaturated state. Some researches are available describing the instability of coarse granular soils in drained or undrained conditions. However, there is a need to investigate the instability mechanism of unsaturated silty soil considering the effect of degree of compaction and net confining stress under partially and fully drained conditions. The specimens in the current study are compacted at 65%, 75%, & 85% degree of compaction, confined at pressures of 60, 80 & 120 kPa, and tested in partially and fully drained conditions. The tests have been performed in two steps. In Step-I, the specimens were sheared in constant water content conditions (a type of partially drained test) to the maximum shear stress. In Step-II, shearing was carried in constant suction conditions (a type of fully undrained test) by keeping shear stress constant. At the start of Step-II, PWP was increased in steps to decrease matric suction (which was then kept constant) and start water infiltration. The test results showed that soil instability is affected much by variation in the degree of compaction and confining stresses. It is also observed that loose and medium dense soils are vulnerable to pre-failure instability i.e., instability occurs before reaching the failure state, whereas, instability in dense soils instigates together with the failure i.e., failure line (FL) and instability line (IL) are found to be unique.

• 한국지반공학회논문집
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• 제25권2호
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• pp.17-24
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• 2009

일반적으로 점토의 비 배수전단강도 산정은 실내실험을 통해 구하지만 초연약점토의 경우 재료의 특성 상 실내실험이 어렵고, 현장실험 또한 여러 제약조건들을 감수해야 한다. 따라서 본 논문에서는 실내에서 수행한 물성실험 및 슬럼프실험과 실내 베인 전단실험의 결과를 회귀분석을 통해 슬럼프 값과 비 배수전단강도 사이의 상관 관계식을 도출하였다. 도출된 상관 관계식의 신뢰성 확보를 위하여 t-분포를 이용한 통계분석을 실시하였고 현장의 데이터와 비교 분석하여 관계식의 적용성 및 신뢰성을 확보하였다.

• 한국지반환경공학회 논문집
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• 제11권7호
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• pp.33-43
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• 2010

한반도 남해안 부산지역의 해성점토에 대하여 물리적 특성을 사전 파악하고, 지반 강도정수의 상관성을 분석하기 위하여 비교적 신뢰성이 크다고 할 수 있는 대형 항만공사 자료를 활용하였다. 분석자료의 정도를 높이기 위하여 해성점토만을 대상으로 하였다. 통일분류법으로 ML, MH, CL, CH, ML-CL에 해당되는 자료는 분석대상에 포함하였으며, SC로 분류되는 자료는 분석대상에서 제외하였다. 지반강도 특성에 대한 분석은 일축압축시험, 삼축압축시험, 현장베인시험 결과에 의한 비배수 전단강도, 예민비, 유효마찰각에 대하여 분석하였으며, 자료분석시 통계분석을 통하여 이상치를 제거하였으며, 또한, 교란도분석을 수행하여 결과에 대한 신뢰성을 높이고자 하였다. 상관관계 분석에서는 선형회귀분석을 수행하여 깊이에 따른 비배수전단강도의 상관관계를 검토하였다. 또한, 동일한 위치에서 수행된 일축 및 삼축압축시험 자료를 분석하여 비배수전단강도의 상관관계식을 도출하였으며, 그 결과 심도와 비배수전단강도는 $S_u=0.015148D+0.04624$의 관계를 보이며, 삼축압축시험에서 구한 비배수 전단강도가 일축압축시험에서 구한 비배수전단강도의 1.26배 정도 크게 평가되었다.

• 한국지반공학회논문집
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• 제30권1호
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• pp.17-25
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• 2014

해상풍력발전기의 기초는 바람, 조류, 그리고 파도 하중을 받기 때문에 해상풍력발전기 기초를 설계하는 데 있어 반복하중을 받는 기초지반의 전단거동 평가가 필요하다. 지반의 비배수 동적 전단거동은 반복하중 횟수, 수직 유효응력, 반복 전단변형률, 상대 밀도, 그리고 평균 및 반복전단응력의 조합에 영향을 받는다. 본 연구에서는 해양 실트질 모래의 비배수 동적 거동에 대한 평균 및 반복전단응력의 영향을 평가하기 위하여 반복단순전단시험(CDSS)을 수행하였으며 상대밀도 85%, 수직 유효응력 200kPa과 300kPa의 시험조건에서 15%의 이중진폭 동적전단변형률(${\gamma}_{cyc}$)과 영구전단변형률(${\gamma}_p$)를 파괴 기준으로 적용하였다. 시험결과는 설계 그래프와 등고선도로 나타내었다. 결과에 따르면 해양 실트질 모래의 비배수 동적 거동은 평균 및 반복전단응력과 두가지 전단응력의 조합에 의해 크게 변하는 경향을 보였다. 평균전단응력이 존재하는 경우에는 반복전단변형보다는 영구변형에 의해 파괴가 결정되는 것으로 나타났다.