• 대한토목학회논문집
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• 제31권1C호
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• pp.19-27
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• 2011

본 연구에서는 도로 성토현장에서 파 기반의 비파괴시험법과 관입시험의 현장 다짐품질 측정에 대한 적용성을 평가하였다. 현장에서 다짐 노상토의 물리 역학적 특성을 평가하기 위해 흙강성 측정기(SSG), 시간영역 반사측정기(TDR), 소형 전기-기계 시스템(MEMS) 가속도계 등의 비파괴시험을 이용하여 다짐 전후 흙의 응답을 평가하였고, 동적 콘관입시험기(DCP)를 이용하여 다짐 후 전단특성을 평가하였다. 현장시험은 두 가지 흙의 종류에 대해 네 가지의 다짐장비 및 다짐에너지로 조성된 성토지반에서 수행되었다. 시험결과, 조사 매커니즘이 다른 시험법인 SSG, TDR, MEMS 가속도계 및 DCP로 측정된 흙의 파라메터들은 상호 연관성이 있는 것으로 분석되었으며, 다짐지반의 전체적인 품질 및 공학적인 응답을 고려하여 시험 방법들을 현장에 적용할 경우, 기존의 다짐도 평가 방법들을 대체 또는 보완하여 현장에서 신속한 다짐품질 평가를 수행할 수 있는 것으로 나타났다.

• 지질공학
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• 제19권3호
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• pp.409-415
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• 2009

일반적으로 흙의 투수계수를 예측하기 위하여 Kozeny-Carman 공식이 널리 적용되어왔다. 그러나 Kozeny-Carman 공식은 모래질 흙의 투수계수 예측에는 좋은 결과를 나타내나 점성토와 같은 세립토에는 적합하지 않다. 따라서 본 논문에서는 Kozeny-Carman 공식을 고려하여 점성토의 투수계수를 예측할 수 있는 이론식을 제시하였다. 이론식을 위해 해안가의 점성토와 댐의 심벽재로 사용하는 다짐 점성토의 토질특성에 대해 조사 분석하였다. 연구 결과, 토질특성과 투수계수 사이의 주요 관계 요소로, 해안가 점성토는 점토함유율, 다짐 점성토는 #200통과율과 관계가 있는 것으로 나타났다.

• 한국농공학회지
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• 제17권3호
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• pp.3815-3832
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• 1975

This study was made to investigate various engineering properties of earth materials resulting from their changes in density and moisture content. The results obtained in this study are summarized as follows: 1. The finner the grain size is, the bigger the Optimum Moisture Content(OMC) is, showing a linear relationship between percent passing of NO. 200 Sieve (n) and OMC(Wo) which can be represented by the equation Wo=0.186n+8.3 2. There is a linear relationship of inverse proportion between OMC and Maximum Dry Density (MDD) which can be represented by the equation ${\gamma}$d=2.167-0.026Wo 3. There is an exponential curve relationship between void ratio (es) and MDD whose equation can be expressed ${\gamma}$d=2.67e-0.4550.9), indicating that as MDD increases, void ratio decreases. 4. The coefficent of permeability increases in proportion to decrease of the MDD and this increase trend is more obvious in coarse material than in fine material, and more obvious in cohesionless soil than in cohesive soil. 5. Even in the same density, the coefficient of permeability is smaller in wet than in dry from the Optimum Moisture Content. 6. Showing that unconfined compressive strength increases in proportion to dry density increase, in unsaturated state the compacted in dry has bigger strength value than the compacted in wet. On the other hand, in saturated state, the compacted in dry has a trend to be smaller than the compacted in wet. 7. Even in the same density, unconfined compressive strength increases in proportion to cohesion, however, when in small density and in saturated state, this relationship are rejected. 8. In unsaturated state, cohesion force is bigger in dry than in wet from OMC. In saturated state, on the other hand, it is directly praportional to density. 9. Cohesion force decreases in proportion to compaction rate decrease. And this trend is more evident in coarse matorial than in fine material. 10. Internal friction angle of soil is not influenced evidently on the changes of moisture content and compaction rate in unsaturated state, On the other hand in saturated state it is influenced density. 11. Cohesion force is directly proportional to unconfined compressive strength(qu), indicating that it has approximately 35 percent of qu in unsaturated state and approximately 70 percent of qu in saturated state.

• 한국지반공학회논문집
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• 제18권5호
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• pp.27-35
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• 2002

원 지반을 성토하여 인공적으로 형성된 다짐지반에 터파기를 하여 관을 매립하거나, 암거를 설치하는 작업을 수행 하는 경우가 자주 있다. 이 때 조성되는 임시굴착사면의 기울기를 적용함에 있어서 실험이나 사면안정해석 등의 적절한 과정을 수행하지 않음으로 인해 사면붕괴가 발생하여 인명 피해는 물론이고 공기의 지연 및 공사비의 증액 등 크고 작은 손실을 초래하고 있다. 본 논문에서는 이러한 임시사면의 안정성 검토를 위해 대표적인 경우들에 대한 사면안정해석을 수행하였으며, 특히 사면안정에 대한 다짐지반의 비등방성에 따른 전단강도의 영향을 검토하였다. 해석에서 적용한 다짐지반의 비등방성 전단강도는 전단면과 다짐층 간의 경사를 변화시키면서 수행한 일련의 직접전단시험으로부터 추정하였다. 해석 결과, 비등방성을 고려하는 지의 여부에 따라서 임시사면의 적절한 안정기울기가 소폭으로 변화할 가능성이 있음을 알았다. 그러나, 이에 따른 안전율의 변화나 파괴면의 양상은 그리 크게 변하지 않는 것으로 나타났다.

• 한국농공학회지
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• 제45권2호
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• pp.86-95
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• 2003

During this study, constant stress ratio tests with previous compression anisotropic stress history are performed on compacted decomposed granite soil sampled at Iksan, Jeonbuk. Yielding points are determined from stress-strain curves. The shape and characteristics of compression anisotropic yield curves is examined. In addition, the measured value of yielding curve and stress-strain behavior is predicted by Yasufuku's anisotropic constitutive model based on non-associated flow rule. The main results are summarized as follows : 1) Shape of yielding curves shows almost ellipse but asymmetry with respect to stress path during previous consolidation stress. 2) Yasufuku's anisotropic constitutive model is suitable in evaluation of yielding curves on anisotropic consolidated decomposed granite soil. 3) The predicted stress-strain curve shows reasonable agreement to measured behaviours.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2006년도 춘계 학술발표회 논문집
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• pp.1224-1227
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• 2006

It has been recognized unsaturated soil behaviour playing an important role in geomechanics. Up to now, only a few experimental data are available for the technical difficulties related to both volume changes and suction measurements. In this study, the volume changes of unsaturated compacted silty soil were monitored with proximeter (i.e. non-contactable transducer) during various triaxial compression tests, which gave a realistic estimation in the volume changes of unsaturated soil sample. The measurement of volume changes were performed with 0.5% of the maximum error under the axial strain ratio of less than 10%. The experimental results have revealed that the mechanical behaviour of unsaturated soil can be significantly affected by the matric suction. During the shearing processes, the level of maximum deviator stress under the initial suction pressure of 50kPa was higher than that under the initial suction pressure of 10kPa. On the other hand, the volume changes became smaller under the increase in the initial suction pressure.

• Smart Structures and Systems
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• 제34권1호
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• pp.33-40
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• 2024

We aimed to assess the evolution of small-strain stiffness and relative density in non-compacted embankment layers. We developed embedded type in-situ soil stiffness measurement devices for monitoring small-strain stiffness occurring after filling at a test site and conducted comprehensive laboratory compaction tests using an oedometer cell with a bender element. However, direct comparison is extremely difficult because the shear wave velocity measured in the field and laboratory depend on depth and effective stress, respectively. Therefore, we propose a method for establishing a relationship between effective stress and depth using a compressibility model. In this study, the shear wave velocity measured in the field was compared to the estimated shear wave velocity-depth profiles for completely dry and saturated conditions with different relative densities. The relative density under saturated soil conditions may vary between 50% and 90% and tends to be closer to 95%. Under dry soil conditions, the relative density of the embankment can vary from 30% to 70% and tends to approach 76%. For model validation, the relative density estimated from shear wave velocity-depth profiles was compared to that estimated from DCPI data. In other words, the results analyzed in the context of an effective stress-depth model enable the prediction of engineering properties such as the small-strain stiffness and relative density of embankment layers. This study demonstrates that physics-based data analyses successfully capture the relative density of non-compacted embankment layers.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1999년도 봄 학술발표회 논문집
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• pp.497-504
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• 1999

This study presents the physical and engineering characteristics of soil-bentonite admixed liner in I landfill. Main focus was the hydraulic conductivity of compacted soil-bentonite admixed and mechanisms governing low permeable properties of the admixed liner. Laboratory and field tests such as compaction, hydraulic conductivity, density, water content for the soil-bentonite admixed liner were carried out. Quality control criteria for the best construction of the soil-bentonite admixed liner was suggested through laboratory and field test results.

• 방사성폐기물학회지
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• 제17권1호
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• pp.29-36
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• 2019

원자력발전소를 운영하게 되면 사용후핵연료와 같은 고준위방사성폐기물이 필연적으로 발생한다. 이러한 고준위방사성폐기물을 처분하기 위해 심층처분방식이 가장 적합한 대안으로 알려져 있으며 고준위방사성폐기물은 공학적방벽과 천연방벽에 둘러 쌓여 지하 500~1,000 m 깊이의 심지층에 처분된다. 이 중 압축 벤토나이트 완충재는 공학적방벽의 가장 중요한 구성요소이다. 완충재는 처분용기와 자연 암반 사이에 위치해 있기에 주변 지하수 흐름으로부터 처분용기를 보호하고 처분 용기로부터 핵종이 유출되는 것을 저지하는 역할을 한다. 주변 지하수 흐름으로 인한 완충재의 불포화 함수특성 규명은 전체 공학적방벽의 성능을 평가하는데 있어 매우 중요하다고 할 수 있다. 따라서 본 연구에서는 실내 시험을 수행하여 국내 압축 벤토나이트 완충재의 건조밀도, 구속조건 여부, 그리고 건조 및 포화 이력에 따른 압축 벤토나이트 완충재의 함수특성곡선을 도출하여 분석하였다. 구속 조건하에서 건조밀도에 따른 함수특성곡선은 큰 차이를 보이지 않았다. 또한 비구속 조건이 구속 조건에 비해 보다 큰 수분흡입력을 나타냈으며, 아울러 포화 과정보다 건조 과정에서 보다 큰 수분흡인력이 측정되었다.

• Geomechanics and Engineering
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• 제18권5호
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• pp.459-469
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• 2019

It is important to estimate the shear strength of shallow compacted soils as a construction material. A series of constant water content triaxial compression (CWCC) tests under low confining state in this study were performed on compacted geomaterials. For establishing a relationship of the shear strengths between saturated and unsaturated states on compacted geomaterials, the suction stresses were derived by two methods: the conventional suction-measured method and the Suction stress-SWRC Method (SSM). Considering the suction stress as an equivalent confining stress component in the (${\sigma}_{net}$, ${\tau}$) plane, it was found that the peak deviator stress states agree well with the failure line of the saturated state from the triaxial compression test when the SSM is applied to obtain the suction stress. On the other hand, the cavitation phenomenon on the measurement of suction affected the results of the conventional suction-measured method. These results mean that the SSM is distinctly favorable for obtaining the suction value in the CWCC test because the SSM is not restricted by the cavitation phenomenon. It is expected that the application of the SSM would reduce the time required, and the projected cost with the additional equipment such as a pore water measuring device in the CWCC test.