• Geomechanics and Engineering
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• 제7권3호
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• pp.263-277
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• 2014

In the conventional design of retaining structures in a seismic zone, seismic inertia forces are commonly assumed to act upwards and towards the wall facing to cause a maximum active thrust or act upwards and towards the backfill to cause a minimum passive resistance. However, under certain circumstances this design approach might underestimate the dynamic active thrust or overestimate the dynamic passive resistance acting on a rigid retaining structure. In this study, a new analytical method for dynamic active and passive forces in c-${\phi}$ soils with an infinite slope was proposed based on the Rankine earth pressure theory and the Mohr-Coulomb yield criterion, to investigate the influence of seismic inertia force directions on the total active and passive forces. Four combinations of seismic acceleration with both vertical (upwards or downwards) and horizontal (towards the wall or backfill) directions, were considered. A series of dimensionless dynamic active and passive force charts were developed to evaluate the key influence factors, such as backfill inclination ${\beta}$, dimensionless cohesion $c/{\gamma}H$, friction angle ${\phi}$, horizontal and vertical seismic coefficients, $k _h$ and $k_v$. A comparative study shows that a combination of downward and towards-the-wall seismic inertia forces causes a maximum active thrust while a combination of upward and towards-the-wall seismic inertia forces causes a minimum passive resistance. This finding is recommended for use in the design of retaining structures in a seismic zone.

• Journal of Ship and Ocean Technology
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• 제1권1호
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• pp.35-47
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• 1997

The consequences associated with ships running aground depend very much on the soil characteristics of the sea bed and the geometrical shape of the ship bow. The penetration into the sea bed depends on these factors and the penetration is an important factor for the ship motion because it influences the ship heave and pitch motions as well as the friction between the ship and the soil. In this paper a rational calculation model is presented for the sea bed soil reaction forces on the ship bottom. The model is based on the assumption that the penetration of the ship bow generates a flow of pore water through the grain skeleton of the soil. The flow is governed by Darcy\`s law and it is driven by the pressure of the pore water at the bow. In addition to this pore water pressure, the bow is subjected to the effective stresses in the grain skeleton at the bow surface. These stresses are determined by the theory of frictional soils in rupture. Frictional stresses on the bow surface are assumed to be related to the normal pressure by a simple Coulomb relation. The total soil reaction as a function of velocity and penetration is found by integration of normal pressure and frictional stresses over the surface of the bow. The analysis procedure is implemented in a computer program for time domain rigid body analysis of ships running aground and it is verified in the paper through a comparison of calculated stopping lengths, effective coefficients of friction, and sea bed penetrations with corresponding experimental results obtained by model tests as well as large, scale tests.

• 한국진공학회지
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• 제5권1호
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• pp.14-24
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• 1996

We have investigated atomic and electronic structures of a clean Pd(111) surface using low energy electron diffraction (LEED) and angle-resolved photoemission spectroscopy (ARPES). A typical clean LEED pattern with a 3-fold symmetry has been observed, corresponding to that for an fcc (111) surface. ARPES measurements have been performed along the $\Gamma-M,\Gamma-K,\Gamma-M$TEX> symmetry lines, from which the experimental band structure of Pd(111) has been determined. The experimental band structure and work function of Pd(111) surface are found to agree well with the calculated band structure of bulk Pd and the calculated work function of Pd(111), respectively. However, the peak positions in the experimental band structure are located closer to the Fermi level than in the theoretical band structure by 0.1~0.8 eV, depending on the $\kappa$-points in the Brillouin zone. In additin, the experimental band widths are narrower than the theoretical band widths by about 0.5eV. The effects of the localized surface Pd 4d states and the Coulomb interaction between Pd 4d bulk electrons have been discussed as possible origins of such discrepancies between experiment and theory.

• 대한토목학회논문집
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• 제3권3호
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• pp.71-86
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• 1983

현재(現在) WSD로 설계(設計)되고 있는 우리 나라 철근(鐵筋)콘크리트 옹벽구조물(擁壁構造物)에 있어서 가장 보편적으로 사용되고 있는 캔틸레버 옹벽(擁壁)의 안정해석(安定解析) 및 각부설계(各部設計)를 보다 합리적(合理的)이며 확률적(確率的)인 신뢰성(信賴性) 이론(理論)을 도입하여 신뢰성(信賴性) 모델에 따른 안정해석(安定解析) 및 각부설계(各部設計)에 대한 신뢰성(信賴性) 설계규준(設計規準)을 LRFD에 의거하여 제안(提案)하고, 또 안정해석(安定解析)의 공칭안전율(公稱安全率)에 대한 이론적(理論的)인 근거를 제시(提示)하는 것이 본(本) 연구(硏究)의 주요내용(主要內容)이다. 신뢰성(信賴性) 이론(理論)에 의해 안정해석(安定解析) 및 각부설계(各部設計)에 대한 한계상태방정식(限界狀態方程式)을 유도하고, Coulomb의 주동토압계수(主動土壓係數), Hansen의 지지력공식(支持力公式)을 사용하여 Cornell의 MFOSM에 의해 불확실량(不確實量) 산정(算定)의 알고리즘을 유도하였으며 그에 따른 불확실량수준(不確實量水準)은 우리 나라의 현실(現實)을 고려한 적절한 값으로 제안(提案)하였다. 현행(現行) R.C. 옹벽설계규준(擁壁設計規準)에 따라 Calibration 하므로서 목표신뢰성지수(目標信賴性指數)${\beta}_0$를 다음과 같이 선택하고(전도(轉倒): ${\beta}_0$=4.0, 골동(滑動): ${\beta}_0$=3.5, 지지력(支持力): ${\beta}_0$=3.0, 휨: ${\beta}_0$=3.0, 전단(剪斷): ${\beta}_0$=3.2), 이 ${\beta}_0$에 대응하는 하중(荷重) 및 저항계수(抵抗係數)를 산정(算定)하였으며, 안정해석(安定解析)에 대한 현행(現行) 철근(鐵筋)콘크리트 표준시방서(標準示方書)의 안전율(安全率)을 검토한 결과 다음과 같은 값이 적절하다는 것을 알았다(전도(轉倒): 1.8, 골동(滑動): 1.9, 지지력(支持力): 3.6). 또한 현행(現行) WSD R.C. 옹벽(擁壁)의 설계규준(設計規準)을 위해 신뢰성(信賴性)에 의한 공칭안전율(公稱安全率)과 허용응력(許容應力)을 제안(提案)하였다. 그리고 본(本) 연구(硏究)에서 제안(提案)하는 R.C. 옹벽(擁壁)의 LRFD 신뢰성(信賴性) 설계규준(設計規準)을 현행(現行) R.C. 표준시방서(標準示方書)의 설계규준(設計規準)에 대응(對應)하는 설계규준(設計規準)으로 도입함이 바람직하다는 사실을 확인할 수 있었다.

• 자원환경지질
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• 제10권1호
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• pp.37-48
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• 1977

The earth's crust is unceasingly undergoing deformations because of the forces acting upon it. The relationship between the tectonic forces and the resulting deformations are found from the states of stresses in the earth's crust induced by these forces. The study has been attempted to analyze the deformations of the overlying sedimentary layers, which are deformed by the magma intrusion along its lower boundary. The elastic model is constructed to analyze the geologic structures, by means of the theory of elasticity, and then the appropriate boundary conditions are given. The solution of the Airy stress function which satisfies the given boundary conditions is derived from the analytic method. The internal stress distributions of the deformed elastic model layer are portrayed by principal stress trajetories, and then the corresponding potential faults and joints systems are predicted from the Coulomb-Mohr failure criterion. The internal displacement distributions are shown by the calculated displacement components vectors, namely horizontal, vertical and net components. Results of the numerical calculations show the developments of some geologic structures as follows; (1) one set of shear joints and or two sets of shear joints which are oppisite directions, and one set of extension joints parallel to the ${\sigma}_1$ direction, (2) one set of high angle thrusts and normal faults, (3) symmetric fold; both limbs are dipping in opposite direction with low angle. The field work at the Wall-A San area, located near Jinju City, in southern Korea, had accomplished to compare the field structures with the predicted ones. The results of the comparison exhibits the developments of joint and fault systems satisfactorily consistent with each others. But the area does not show any type of folding, in spite of the intrusion of a granodiorite massif, this fact is one of the important features of the whole Kyungsang sedimentary basins of Mesozoic age distributed at the south-eastern parts of Korea. For this reason, it is thought that the magma intrusion had occurred with extremly low pressure. The geologic structures have been modified by the erosion and weathering throughout the geologic time, and the conditions of the sedimentary layers (width, thickness and radius of magma) are not the same as before, being intruded by the magma. To enlighten this, it is preferable to study these geologic structures with analyses of various types of rheological models.

• 한국구조물진단유지관리공학회 논문집
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• 제6권3호
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• pp.201-209
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• 2002

Crib wall system은 일반적으로 segmental crib type의 옹벽형식으로 stretcher라는 전 후면 가로보와 세로 방향으로 header라는 버팀보를 연속적으로 쌓아 올리는 공법이다. 이때, stretcher와 header로 구성된 골격 내부에는 흙으로 속채움을 하여 다져, 본 구조체가 일체거동이 가능한 강성체(rigid body)를 형성시킴으로써 배면의 토압에 대하여 저항하는 구조물이다. 따라서, 안정성 해석은 일반적으로 기존의 철근콘크리트 옹벽과 같이 전체 옹벽이 하나의 강성체로 작용한다고 가정하여 토압이론에 의하여 평가하고 있다. 그러나, 변형문제에 있어서 본 구조물은 단순히 하나의 구조체로 가정하여 해석하기가 곤란하다. 왜냐하면, stretcher와 header는 일반 보강토옹벽의 전면 벽체 부재와는 달리 뒷채움재 내에 어떠한 인장 보강재도 삽입되지 않기 때문에 독립된 변위거동을 나타낸다. 또한, 각각의 독립부재로 구성된 재료와 내부채움재의 힘과 변형은 3차원적으로 거동하며 수평토압에 의하여 복합적인 상호거동을 일으키기 때문이다. 따라서, 본 연구는 Crib wall system의 변위경향을 보다 엄밀하게 해석하기 위하여 Brandl(1985)의 full scale 시험 결과를 바탕으로 수치해석 모델을 제시하였다.

• 생물환경조절학회지
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• 제30권4호
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• pp.287-294
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• 2021

국가관리 간척지내 원예단지 조성에 필요한 기반기술 중에 하나인, 온실기초 연구가 부족한 실정이며 고사양의 PHC파일을 대체하기 위한 대안을 검토하고자 하였다. 지반개량공법 중 심층혼합처리공법(DCM) 적용시 허용지지력과 침하량 산정을 통하여 온실기초 공법으로써의 적용가능성을 검토하였다. 새만금간척지 농생명용지 1공구 지반조사를 통해 지반 특성을 파악하고, Terzaghi, Meyerhof, Hansen, Schmertmann 이론식을 적용하여 허용지지력과 침하량을 산정하였다. 직경 800mm를 기준으로, 독립 기초 폭과 길이가 3-6m이고, 기초 심도 3-7m 조건에서 허용지지력과 침하량을 검토하였다. 온실기초 심도가 얕고 콘크리트 매트 간격이 넓을수록 시공비가 절감되는 측면을 고려하여 독립 기초 폭과 길이가 4m, 기초 심도가 3m인 경우가 가장 적합한 것으로 판단되었다. 독립 기초 폭과 길이가 4m이고, 기초 심도가 3m인 조건에 대한 해석 결과로 허용지지력은 169kN/m², 침하량은 2.73mm로 지지력은 이론식 대비 5.6%의 오차를, 침하량은 62.3%의 오차범위를 나타냈다. 향후, 위 검증된 설계 값을 기준으로 구조 시험과 침하모니터링을 통해 신뢰성을 검증하고자 한다. 그 외 나무말뚝, 헬리컬기초 등 유리온실, 내재해형온실에 적용 가능한 기초 공법과의 비교 검증을 통해 각각의 장, 단점을 파악하고 PHC 파일의 대체 가능 유무를 검토할 예정이다. 이는 온실 유형별 시공 공법을 선정하는데 필요한 기초 데이터로 제시될 수 있을 것으로 기대된다.