• 한국지반공학회논문집
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• 제20권6호
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• pp.119-126
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• 2004

본 논문에서는 현장계측을 통해 관측된 소일네일링 벽체의 거동을 분석하였다. 연구의 주요내용으로는 인발시험을 통해 산정한 네일과 지반의 경계면에서 전단강도의 발생, 지반의 수평변위, 네일에 발생하는 인장력의 분포 및 경계면에서의 전단강도의 발현 등이다. 특히, 경계면에서의 전단응력 발생 과정 및 전단강도 발현에 대한 심도있는 분석을 실시하였다. 본 연구에서 분석된 자료는 국내 소일네일링의 예비설계 단계시 참고 자료로 활용될 수 있을 것으로 기대된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1997년도 가을 학술발표회 논문집
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• pp.19-36
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• 1997

This paper discusses the reduction and subsequent recovery and increase of shear strength of clay in the vicinity of soil-cement column. Laboratory and field tests were conducted to investigate the effects on surrounding clay during and after soil-cement column installation in soft Ariake clay. Discussions were made on the mechanism of strength changes of clay by considering the thixotropic recovery, reconsolidation effect, penetration of cement slurry and diffusion of exchangeable cations. On the basis of field and laboratory observations, 10 days after column installation, the decreased shear strength of surrounding clay during mixing was recovered and 30 days later, shear strength of surrounding clay increased 30% by average. Therefore, it is recommended that the increase of shear strength of clay can be taken into consideration in the bearing capacity and stability analysis of the composite ground.

• 한국환경복원기술학회지
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• 제4권3호
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• pp.49-54
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• 2001

It is common that the soil layer is a few meters below the earth's surface and the rock mass is below the soil layer in the view of geological characteristics in Korea. And the boundary between rock and soil is clearly divided. When dealing with the stability of rock masses, as in the case of rock slopes or dam foundations, the majority of the collapses is not within the soil layer, but within the soil-rock boundary. Therefore it is important to identify the shear strength characteristics between soil-rock boundary. And then in the method of reinforcement on landslide this chose a cut slope near Daemo elementary school in Seoul, surveyed shear strength between soil-rock contacts and considered a large scale collapse using a limit equilibrium method.

• 한국산림과학회지
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• 제66권1호
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• pp.16-36
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• 1984

화강암질풍화토(花崗岩質風化土)의 미교란(未攪亂) 시료(試料)를 사용하여 일면(一面) 직접(直接) 전단시험(剪斷試驗)으로 측정(測定)한 전단강도(剪斷强度)와 함수비(含水比), 간극비(間隙比), 건조밀도(乾燥密度), 비중(比重)과의 관계(關係)를 통계(統計) 분석(分析)하였고, 화강암질풍화토(花崗岩質風化土)의 사방시공지(砂防施工地)에 식재(植栽)된 리기다소나무림(林)과 리기테-다소나무림(林)에서 토양단면(土壤斷面)을 만들어 산중식토양경도계(山中式土壤硬度計)로 토양(土壤)의 견밀도(堅密度)를 측정(測定)하고 수근분포(樹根分布)를 조사(調査)하여 통계(統計) 분석(分析)한 결과(結果) 다음과 같다. 1) 함수비(含水比), 간극비(間隙比)와 전단강도(剪斷强度) 간(間)에는 유의적(有意的)인 부(負)의 상관(相關)이며 직접적(直接的)인 관계(關係)에 있었다. 2) 건조밀도(乾燥密度)와 전단강도(剪斷强度) 사이에는 정(正)의 상관(相關)이며 직접적(直接的)인 관계(關係)에 있었다. 3) 비중(比重)과 전단강도(剪斷强度) 간(間)에는 유의적(有意的)인 상관관계(相關關係)를 인정(認定)할 수 없었다. 4) 전단강도(剪斷强度)에 영향(影響)을 미치는 영향요소(影響要素)의 직접효과(直接效果)의 크기는 함수비(含水比)>간극비(間隙比)>건조밀도(乾燥密度)의 순위(順位)이다. 5) 다중선형(多重線型) 회귀방정식(回歸方程式)의 분산분석결과(分散分析結果) 함수비(含水比)만이 회귀성(回歸性)이 인정(認定)되므로 함수비(含水比)를 독립변수(獨立變數)로 하여 전단강도(剪斷强度)를 추정(推定)하기 위한 회귀방정식(回歸方程式)은 제한(制限)된 건조밀도(乾燥密度)의 범위내(範圍內)에서 적합도(適合度)가 매우 높게 평가(評價)되었다. 6) 토양(土壤)의 견밀도(堅密度)는 토심(土深)이 깊어짐에 따라 높아진다. 7) 토양(土壤)의 지표경도(指標硬度)와 수근수(樹根數) 간(間)에는 유의적(有意的)인 부(負)의 상관(相關)이며 직접적(直接的)인 관계(關係)에 있었다. 8) 리기다소나무와 리기테-다소나무의 수근(樹根)은 토심(土深) 20cm까지에 대부분 분포(分布)하고 있었다. 9) 리기다소나무림(林)과 리기테-다소나무림(林)에서 측정(測定)한 토양(土壤)의 지표경도(指標硬度)를 독립변수(獨立變數)로한 회귀방정식(回歸方程式)으로 수근수(樹根數)를 추정(推定)할 수 있었으나 낮은 적합도(適合度)를 나타내었다.

• 한국지반환경공학회 논문집
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• 제13권4호
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• pp.71-76
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• 2012

흙의 전단강도는 흙 속의 임의의 면을 따라 발생하는 파괴와 활동에 저항하는 힘으로 흙의 공학적 특성 중에 가장 중요한 요소 중의 하나이다. 전단강도는 앝은 기초나 말뚝의 지지력 해석방법과 같은 기초공학의 문제나 댐 및 절 성토 후의 사면안정, 그리고 토류 구조물의 횡토압과 같은 흙의 안정 문제 해석 등에 이용된다. 본 연구는 화강풍화토에서 점성토 성분을 제거하고 건조시킨 후, 2 00mm(10번체)와 0 85mm(20번체), 0 475mm(40번체)로 분류한 시료로 직접전단시험기를 이용하여 전단강도 변화를 파악하고자 하였으며, 또한 산호모래를 선정하여 비교 시험을 실시하였다. 따라서 본 연구는 입자의 크기에 따른 전단강도 특성을 비교한 연구에 도움이 될 것으로 판단된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2009년도 춘계 학술발표회
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• pp.844-851
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• 2009

A soil mixture with low permeability and bentonite as an additive has been highly utilized as a cutoff material in landfills, banks, and dams. Even though it is anticipated that the water can seep through shear failures in the filter layer due to external loads and embankment loads during construction, usually only the coefficient of permeability of the soil mixture is considered rather than the changes of strength from the different amounts of additives. Therefore, the amount of bentonite was changed between 0%~4% in the soil mixture of the bed material to conduct a series of unconfined compressive strength, tensile strength, and shear strength tests on a specimen in order to study the characteristics of the strength. In the result, the unconfined compressive and tensile strength were increased along with the increased amount of bentonite in the low water content; however, the tensile strength in the consolidated-drained shear test generally showed similar values without significant changes.

• 한국해양공학회지
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• 제23권3호
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• pp.20-29
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• 2009

This study investigated the shear strength characteristics of waste tire powder-added lightweight soil (WTLS), which were developed to recycle dredged soil, bottom ash, and waste tires. The WTLS used in this experiment consisted of dredged soil, bottom ash, waste tire powder, and cement. Test specimens were prepared with various contents of waste tire powder ranging from 0% to 100% at 25% intervals and bottom ash contents of 0% or 100% by the weight of the dry dredged soil. In this study several series of direct shear tests were carried out, which indicated that the shear properties of WTLS were strongly influenced by the mixing conditions, such as the waste tire powder content and bottom ash content. The unit weight, as well as the shear strength of the WTLS, decreased with an increase in waste tire powder content. The shear strength of WTLS with bottom ash was 1.34 times greater than that of WTLS without bottom ash. An average increase in cohesion of 30 kPa was obtained in WTLS with the inclusion of bottom ash due to the bond strength induced from the pozzolanic reaction of the bottom ash. In this test, the maximum value of the internal friction angle was obtained with a 25% content of waste tire powder.

• 한국환경복원기술학회지
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• 제5권3호
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• pp.9-14
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• 2002

It is common that the soil layer is few meters below the earth surface and there are rock masses below the soil layer in the view of geological characteristics in Korea. The boundary between rock and soil is clearly divided. When dealing with the stability of rock masses, as in the case of rock slopes or dam foundations, the majority of the collapses is not within the soil layer, but within the soil-rock boundary. Therefore, it is important to identify the shear strength characteristics between soil-rock contacts. It has been common practice to assume that the strength of the soil or shale represents the minimum strength present. However, it has been suggested by Patton(1968) that such an assumption may not be valid and that lower shear strengths might be obtained along the soil-rock interface than for either material alone. Then, in this thesis, introduce rock and residual soil shear strength tests and the specimen preparation and testing procedures are described in detail and also the testing results are presented and discussed.

• Geomechanics and Engineering
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• 제1권1호
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• pp.35-52
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• 2009

A significantly thick zone of steep slopes is commonly encountered above groundwater table and the soils within this zone are unsaturated with negative pore-water pressures (i.e., matric suction). Matric suction contributes significantly to the shear strength of soil and to the factor of safety of unsaturated slopes. However, infiltration during rainfall increases the pore-water pressure in soil resulting in a decrease in the matric suction and the shear strength of the soil. As a result, rainfall infiltration may eventually trigger a slope failure. Therefore, understanding of shear strength characteristics of saturated and unsaturated soils under shearing-infiltration (SI) conditions have direct implications in assessment of slope stability under rainfall conditions. This paper presents results from a series of consolidated drained (CD) and shearing-infiltration (SI) tests. Results show that the failure envelope obtained from the shearing-infiltration tests is independent of the infiltration rate. Failure envelopes obtained from CD and SI tests appear to be similar. For practical purposes the shear strength parameters from the CD tests can be used in stability analyses of slopes under rainfall conditions. The SI tests might be performed to obtain more conservative shear strength parameters and to study the pore-water pressure changes during infiltration.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2010년도 춘계 학술발표회
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• pp.577-583
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• 2010

In this study, the effect of void formation resulting from gas hydrate dissociation or loss of some particles within soil structure on the strength of soil is examined. Beag-ma river sands with uniform gradation were used to simulate a gas hydrate bearing or washable soil structure. Empty capsules for medicine are used to mimic large voids, which are bigger than soil particle. Beag-ma river sand was miced with 8% cement ratio and 14% water content and compacted into a shear box. The number and direction embedded into a specimen. After 4 hours curing, a series of direct shear test is performed on the capsule embedded cemented sands. Shear strength of cemented sands with capsules depends on the volume and direction. The volume and direction formed by voids are most important factors in strength. A shear strength of a specimen with large voids decreases up to 39% of a specimen without void. The results of this study can be used to predict the strength degradation of gas hydrate bearing sediments after dissociation and loss of fine particles within soil structure.