• 산업기술연구
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• 제22권B호
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• pp.211-218
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• 2002

The paper is to show the behavior of composit ground which is installed with sheet pile in soft soil improved by sand compaction pile. The results of load-settlement relationship, earth pressure, stress concentration characteristics, and final water content were obtained by centrifuge model test. Two cases of tests, installation of sheet pile on the corner and both side of the loading plate for the improved SCP ground which was designed twice of the footing width, were performed for the tests under the vertical and horizontal loading and both side of corner. Finite element program(CRISP) for sand compaction pile using elasto-plastic model and numerical analysis for soft soil using modified cam-clay constitutive equation were compared and analized with the results of model tests. The result of analysis show the increased bearing capacity of soil after, SCP and sheet pile was installed.

• 한국수자원학회논문집
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• 제40권3호
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• pp.215-221
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• 2007

본 연구에서는 침투정 설치 시 침투정 토양표면의 막힘 현상에 따른 침투능 저하를 감소시키기 위한 빙안을 강구 하고자 하였다. 또한 각기 다른 토양특성에 따른 침투능의 변화를 알아보기 위하여 여러 다른 실험조건에서 침투능의 변화를 관찰하였다. 실험결과에 의하면 침투정 설치 시 침투정의 하부토양은 자갈이나 가급적 입경이 큰 토양을 설치함으로써 침투정으로부터 우수를 빠른 시간 내에 배수시킬 수 있을 것으로 사료된다. 하지만 장기적으로 시간이 경과함에 따라서 침투능이 감소하는 경향을 보이는 것을 고려할 때 토양 내부에 부유토사의 침투에 따른 막힘 현상이 발생되고 있는 것으로 사료된다. 하부 자연 토양의 다짐을 방지하기 위하여 자연토양 상부에 가급적 얕은 깊이로 모래를 설치하고 가급적 굵은 자갈을 상부에 설치하여 저류능과 수두를 높여 침투능을 향상시키는 것이 바람직하다. 또한 정기적으로 침투정에 발생하는 crust(경화 토피층)를 제거하고 침투정내 모래를 수시로 교체하여 원래의 침투능을 유지하도록 하는 것이 필요하다.

• 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.

• 한국지반공학회논문집
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• 제15권5호
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• pp.205-215
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• 1999

파쇄성 사질토 지반은 세계각지의 해안을 중심으로 넓게 분포되어 있고, 칼슘성분을 다량 함유한 석회질 모래지반은 입자파쇄의 영향으로 높은 압축성을 나타내는 특징이 있다. 본 연구에서는 모래의 강도-변형특성에 관여하는 입자파쇄의 특성을 명백히 하기 위하여, 세가지 종류의 카보네이트계 모래와 실리카계의 모래를 이용하여 광범위한 응력영역에 대한 등방압축시험을 실시하였다. 다양한 상대밀도에 대한 등방압축 조건에서 압축 항복응력과 입자 파쇄응력과의 관계로부터 파쇄성지표 K를 제안하였다. 제안된 파쇄성지표 K는 흙입자 강도와도 밀접한 관계를 가지며, 흙의 파쇄성을 평가하기 위한 중요한 인자로 사료된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2006년도 춘계 학술발표회 논문집
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• pp.301-310
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• 2006

A series of laboratory tests was carried out for analyzing compaction characteristics of hydraulic fill soils(or hydraulically filled soils). Hydraulic fill soils were settled down by the weight of soil particle itself in water and consolidated by the extraction of water from the soil structures. Water content and dry unit weight were observed as the depth of sedimentation and consolidation soil. It was found from the result that the optimum water content $(W_{cpt})$ of the maximum unit weight$(\gamma_{dmax})$ is higher than that of laboratory compaction test(KS F 2312 A method). It was due to difference in compaction energy and compaction effect between two methods. And the maximum dry unit of hydraulic fill soil is smaller than that of laboratory compaction test. Especially in terms of compaction effect, the maximum relative compaction degrees$(R_{cmax})$ of Seamangum dredged sand, river sand and mixed sand, half and half of dredged and river sands, were 85%, 91% and 86%, respectively. It means that the compaction effect can be $85\sim91%$ of the maximum unit weight in laboratory compaction test.

• 한국대기환경학회지
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• 제6권1호
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• pp.11-21
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• 1990

To quantitatively estimate the effect of yellow sand(loess) fromt he Northern China, various soil sources having similar chemical compositions to yellow sands should be separated and identified. After that, mass contribution for yellow sand can be calculated. The study showed that it was impossible to solve this problem by the traditional bulk analyses. However, particle-by-particle analysis by a CCSEM (computer controlled scanning electron microscope) gave enormous potentials to solve it. To perform this study, seven soil source data analyzed by CCSEM were obtained from Texas, U.S.A. Initially, each soil date was classified into two groups, coarse and fine particle groups since the particle number distribution showed a minimum occurring at 5.2$\mu$m of aerodynamic diameter. Particles in each group were then classified into one of the 283 homogeneous particle classes by the universal classification rule which had been built by an expert system in the early study. Further, mass fractions and their uncertainties for each class in each source were calculated by the Jackknife method, and then source profile matrix for the 7 soil sources was created. To use the profile matrix in the study of source contribution, it is necessary to test the degree of collinearity among sources. The profiles were tested by the singular value decomposition method. As a result, each soil source characterized by artificially created variables was totally independent each other and is ready to use in source contribution studies as a receptor model.

• 한국지반공학회논문집
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• 제28권4호
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• pp.55-65
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• 2012

본 연구는 지반조건에 따른 효과적인 마이크로 파일의 설치방법을 제안하기 위해 실트 또는 모래지반에서 모형시험을 수행하였다. 시험결과, 관입 전단파괴가 발생한 실트지반은 압축변위에 저항하도록 마이크로 파일을 엇갈리게 설치(${\theta}$ < $0^{\circ}$)하는 것이 효과적이며, 전면 또는 국부전단파괴가 발생한 모래인 경우 횡 방향 변위에 저항하도록 마이크로 파일을 경사지게 설치(${\theta}$ > $0^{\circ}$ 또는 ${\theta}$ < $0^{\circ}$) 하는 것이 효과적인 것으로 나타났다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 추계 학술발표회
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• pp.738-743
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• 2008

Ultimate lateral loaded pile capacity is influenced by soil conditions. Methods of calculating ultimate lateral loaded pile capacity in homogeneous soil were suggested by a lot of previous researchers.(Broms 1964, Petrasovits & Award 1972, Prasad & Chari 1999, Zhang et al. 2005) There is only few homogeneous soil in actual condition, however, it could be not conviction that the methods from previous researchers are correct in multi-layered soil. In this study, the variation of ultimate lateral loaded pile capacity was analyzed in the various multi-layered conditions, ultimate lateral loaded pile capacity was calculated by the methods from previous researchers. For this study, the Lateral Pile Load Tests (LPLT) were performed in calibration chamber, the soil was composed by 3 layers and each layers had a various relative density. The results of LPLT were compared with calculated results from the previous researchers.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2006년도 춘계 학술발표회 논문집
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• pp.896-905
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• 2006

Several soil parameters such as particle characteristics, geological element, drainage and loading conditions are influenced on the shear strength of soil. The characteristics of soil particles are important factor to the shear strength of soil. However, this component is not well considered in the determination of soil strength in Korea. The particle shape of sand was analyzed by utilizing SEM(Scanning Electron Micrograph) and compared its results in terms of aspect ratio, angularity and roughness. Based on the determined soil parameters, the ultimate bearing capacity of sandy ground was estimated by using Terzaghi bearing capacity equation.

• 아시안잔디학회지
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• 제8권3호
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• pp.149-165
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• 1994

This report was investigated on the soil and mineral nutrient erosions in comparison among the vegetation floors of M isranthus sisensis, Arternisia stelleriana, Rhododendron mucronula turn, Zoysia ja-ponira and Pinus deusitlora communities and the naked soil on Mt. Keum-hak in Cheolwon-Koon, The erosion of clay, silt, fine sand and coarse sand of the surface soils under the Z. japonira grass-land was far less then those of M. sinensis, A. stelleriana, R. murronulatum and P. densiflora com-munities and the naked soil, The loss of mineral nutrients due to the soil erosion was the lowest level in the Z. japonira grassland and the highest level in the P. densiflora forest and the naked soil, respectively.