• 한국농공학회지
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• 제44권1호
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• pp.103-115
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• 2002

During this study, various stress path tests in previous isotropic and anisotropic (compression and tension) stress histories are performed on weathered granite soil sampled at Iksan, Jeonbuk. Yielding points are determined from various stress-strain curves(stress ratio-shear strain, volumetric strain, normalized energy and dissipated total energy curves). The shape and characteristics of isotropic and anisotropic yielding curves are examined. The main results are summarized as follows . 1) Yielding curries defined from stress ratio - normarized energy and dissipated total energy curves show almost perfect ellipse. 2) Directions of plastic strain incremental vector are not perpendicular to yielding curve. 3) Normarized energy and dissipated total energy spread with similar tendency with respect to yielding currie in stress space.

• 한국지반공학회지:지반
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• 제9권2호
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• pp.5-14
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• 1993

화강풍화토는 한국에서 대부분을 차지하고 있는 대표적인 토질이다. 본 연구는 화강풍화토의 동역학적 특성치와 침하특성을 실험적으로 연구함으로써 화강풍화토에 기초를 둔 구조물의 동역학적 해석에 기여하고자 한다. 입도가 서로 다른 두종류의 화강풍화토를 상대밀도 80~90% 범위의 공시체를 성형하여 진동 삼축압축시험을 실시하였다. 시험을 통하여 전단탄성계수와 감쇠계수를 시료의 상대밀도와 구속응력을 달리하여 구하고 이를 전단 변형률의 크기에 따라 표시하였다. 대표적인 결과로서, 전단탄성계수는 화강풍화토를 구성하는 입도분포에 따라 구속응력, 시료의 상대밀도 및 전단변형률과 관련하여 큰 변화를 나타내었다. 모래성분이 많은 화강풍화토의 동적특성치는 Seed와 Idriss에 의하여 정리된 모래의 값 보다 다소 큰 값이 측정되었다. 또한 잘다져진 화강풍화토에 대하여 진동하중에 의한 잔류침하는 거의 일어나지 않았다.

• Geomechanics and Engineering
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• 제9권1호
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• pp.101-113
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• 2015

Saturated soil hydraulic conductivity is a very important soil parameter in numerous practical engineering applications, especially rainfall infiltration and slope stability problems. This parameter is difficult to measure since it is very highly sensitive to various soil conditions. There have been many analytical and empirical formulas to predict saturated soil hydraulic conductivity based on experimental data. However, there have been few studies to investigate in-situ hydraulic conductivity of weathered granite soils, which constitute the majority of soil slopes in Korea. This paper introduces an estimation method to derive saturated hydraulic conductivity of Korean weathered granite soils using in-situ experimental data which were obtained from a variety of slope areas of South Korea. A robust regression analysis was performed using different physical soil properties and an empirical solution with an $R^2$ value of 0.9193 was suggested. Besides that this research validated the proposed model by conducting in-situ saturated soil hydraulic conductivity tests in two slope areas.

• Journal of Ginseng Research
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• 제29권4호
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• pp.192-205
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• 2005

This study is for geochemical relationships between ginsengs and soils from three representative soil types from Keumsan, shale, phyllite and granite areas. For this study, ginsengs (2, 3 and 4 years), with the soils and their host rock, are collected and are analysed for the transitional elements. In the weathered soils, the shale area is high in the most of elements, but low in the granite area. High correlation relationships are shown in the shale area. In the field soils, the shale area is mainly high, but low in the granite area. Comparing with ages, most of elements are high in the 2 year soils, but low in the 4 year soils. Regardless of the localities, positive and negative correlations are dominant in the shale area. In the host rocks, high element contents are shown in the phyllite and shale areas. Positive and negative correlations are found in the shale and phyllite areas for large numbers of the element pairs. In the ginsengs, differences of the element contents with ages are not clear, but show high element contents in the 2 year ginsengs of the shale and phyllite areas, and low contents in the 4 year ginsengs of the granite area. Positive correlations are shown in the Cu-Zn pair in the shale and phyllite areas, and Co-Cu pair in the granite area. In the relative ratios(weathered soil/field soil), most of elements from the shale area are high, above I, suggesting high element contents in the weathered soils of the shale area relative to the granite and phyllite areas. In the relative ratios(weathered soil/host rock), most of elements are above 1, suggesting the high element contents in the weathered soils relative to the host rocks. Relative ratios (soil/ginseng) of the element contents are several to ten times. Regardless of the areas, big differences of the relative ratios are found in the Co and small differences are in the Cu and Zn, which suggest that differences between soils and ginsengs are big in the Co contents and small in the Cu and Zn contents. Regardless of the ages, differences among relative ratios are small in granite area relative to the shale area, which suggest more similar contents between ginsengs and soils in the granite areas.

• 한국가스학회지
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• 제3권2호
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• pp.43-52
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• 1999

지하에 매설된 도시가스 배관에서의 누출 가스에 대한 확산 거동을 관찰하기 위하여 지중 확산실험조를 제작하여 실험하였다. 실험조는 도시가스 공급위치와 농도의 측정위치를 변화시킬 수 있도록 acryl로 제작하였으며, MOS 센서를 이용하여 도시가스 농도를 측정하였다. 가스의 지하 확산을 측정하기 위한 토질로서 주문진 표준사와 화강풍화토를 이용하였으며, 가스누출 속도 변화에 따른 도시가스 농도 변화를 시간에 따라 측정하였다. 누출점으로부터 센서의 측정위치가 가까울수록 또는 누출 속도가 증가할수록 가스의 감지시간이 감소하였으며, 누출가스 농도의 빠른 증가로 인하여 정상상태시 높은 농도를 나타내었다. 또한, 주문진 표준사보다 다짐에 의해 밀도가 증가한 화강풍화토에서 초기에 농도가 낮게 측정되었으나, 시간이 지남에 따라 농도가 높게 나타났다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 지반공학 공동 학술발표회
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• pp.360-372
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• 2005

The weathering degree and shear wave velocity, $V_S$, were evaluated for decomposed granite layers in Hongsung, where earthquake damages have occurred. The subsurface geological layers and their $V_S$ profiles were determined, respectively, from boring investigations and seismic tests such as crosshole, downhole and SASW tests. The subsurface layers were composed of 10 to 40 m thickness of weathered residual soil and weathered rock in most sites. In the laboratory, the weathering indexes with depth were estimated based on the results of X-ray fluorescence analysis using samples obtained from field, together with the dynamic soil properties determined from resonant column tests using reconstituted specimens. According to the results, it was examined that most weathering degrees represented such as VR, Li, CIA, MWPI and WIP were decreased with increasing depth with exception of RR and CWI. For weathered residual soils in Hongsung, the $V_S's$ determined from borehole seismic tests were slightly increased with increasing depth, and were similar to those from resonant column tests. Furthermore, the $V_S$ values were independent on the weathering degrees, which were decreased with depth.

• 한국농공학회지
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• 제23권4호
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• pp.53-59
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• 1981

This experiment was carried out to find out the effectiveness of soil cement stabilization about the Song-I in Cheju province. The results are summarized as follows; 1.The increasing ratio of unconfined compressive strength according to the increment of cement content was markedly low compared with the weathered granite soil, so the effect of stabilization was low. 2.The moisture content of the sample of Song-I indicates the maximum unconfined compressive strength showed at the 5% or so of dry side than the optimum moisture content and the change of the unconfined compressive strength according to the change of moisture content was not sensitive compared with the weathered granite soil. 3.Generally the primary strength of curing age within 7 days of the sulfate resisting cement was low compared with the normal portland cement and the strength of 28 curing days showed a similar tendency, especially in case of Song-I, and it seemed that the sulfate resisting cement was a little more effective than the normal portland cement. 4.As the unconfined compressive strength of grain size controlled Song-I was low compared with the weathered granite soil, so the rate of weight loss by the durability test was great, therefore it was thought that the durability was weak.

• 한국농공학회논문집
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• 제57권3호
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• pp.93-100
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• 2015

The object of this paper is to study the shear characteristics of the weathered granite soil. To this end, a series of consolidated undrained triaxial compression tests are carried out to investigate the shear parameters-cohesion and internal friction angle-for the degree of saturation and degree of weathering. From the results, it is found that the shear parameters of weathered granite soil are influenced on the degree of saturation, degree of weathering and disturbance. Especially, internal friction angle is more influenced on the upper factors than cohesion. And shear parameters are more acted on the degree of saturation than the degree of weathering in the test range. It is, therefore, recommended that must be considered the conditions of granite soil-degree of saturation, degree of weathering and disturbance etc-in case of the calculation of bearing capacity, stability analysis and other designs with shear parameters.

• 물과 미래
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• 제7권2호
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• pp.83-91
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• 1974

Fill Type Dam에 있어서 일반적으로 축조재료는 경제성을 감안하여 Dam Site 부근에서 구해야하므로 Core 용재료로서는 차수성의 문제만 해결된다면 마시토도 사용가능할 것이라는 전제하에 본문에서는 마사토를 단독 또는 혼합재료로서 각종시험을 실시하여 사용가능성 여부를 검토하고 기사용범위를 정함으로써 앞으로의 사용자들에게 편의를 제공코저 한다.

• 농업과학연구
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• 제12권1호
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• pp.86-100
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• 1985

불포화상태(不飽和狀態)에서의 화강암질풍화토(花崗岩質風化土)의 강도특성(强度特性)을 구명(究明)하기 위(爲)하여 5종류(種類)의 화강암질풍화토(花崗岩質風化土)와 1종류(種類)의 보통(普通)흙(사질(砂質)롬)을 택(擇)하여 불교란시료(不攪亂試料) 및 교란시료(攪亂試料)를 채취(採取)하여 삼축압축시험(三軸壓縮試驗)을 한 결과(結果)를 요약(要略)하면 다음과 같다. 1. 자연상태(自然狀態)에서의 건조밀도(乾操密度)는 다짐 시험(試驗)에서 구(求)한 최대건조밀도(最大乾操密度)보다 작은 값을 나타냈고 입도배합(粒度配合)이 양호(良好)한 흙에서 건조밀도(乾操密度)는 큰값을 나타냈다. 2. 함수비(含水比)의 증가(增加)에 따라 파괴강도(破壞强度)는 감소(減少)하였고 이 현상(現象)은 점착력(粘着力)이 큰 보통(普通)흙에서 더욱 현저하게 나타났다. 3. 화강암질풍화토(花崗岩質風化土)의 강도정수중(强度定數中) 점착력(粘着力)은 작고 내부마찰각(內部摩擦角)은 컸으며 함수비(含水比)의 증가(增加)에 따라 점착력(粘着力)보다 내부마찰각(內部摩擦角)에서 감소현상(減少現象)이 크게 나타났다. 4. 변형계수(變形係數)는 함수비(含水比)의 증가(增加)에 따라서 감소(減少)하였고 이 현상(現象)은 화강암질풍화토(花崗岩質風化土)보다 보통(普通)흙에서 더욱 크게 나타났다. 5. 파괴강도(破壞强度)는 액압(液壓)이 증가(增加)함에 따라 증가(增加)하였고 이 현상(現象)은 저함수비(低含水比)에서 더욱 현저하게 나타났다.