• 한국지반공학회논문집
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• 제25권6호
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• pp.89-99
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• 2009

다짐재료의 물리적인 지표와 역학적정수와의 관계를 명확히 하고, 설계에 필요한 역학정수를 간극비 및 건조밀도 등의 물리적 지표를 통해 간단히 추정하는 방법을 제시하기 위하여, 화강풍화토를 이용한 다짐시험, 일차원압축시험, 불포화삼축압축시험을 실시하였다. 실험결과, 다짐으로 인해 공시체는 과압밀상태가 되며 다짐 에너지의 증가로 공시체의 강도정수가 증가되는 것이 정량적으로 확인되었고, 다짐재료의 과압밀상태를 평가하는 선행압축이론을 이용하여 다짐 후의 간극비로부터 강도정수를 추정하는 방법을 제시하여 그 공학적 적정성을 확인하였다.

• 한국환경농학회:학술대회논문집
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• 한국환경농학회 2011년도 30주년 정기총회 및 국제심포지엄
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• pp.177-187
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• 2011

This study was conducted to determine some physical and chemical properties of the soil and their relationship to spectroscopic-based (visible range) analytical methods while evaluating soil organic matter fractions and soil quality in degraded and non-degraded soils in a wide range of environments. Soil samples were collected from the different landscape positions of cultivated and noncultivated soils, and the latter from the same landscape positions but with different vegetation, at Songco, Lantapan, Bukidnon. The physical and chemical properties of the soils were determined at the SPAL, CMU, Musuan, Bukidnon while the metagenomic properties were determined at the Laboratory of the University of Missourri, Missourri, USA. Bulk density and air dry soil strength values of the soils from the cultivated areas were generally higher than those of the uncultivated areas. Also, soils at the summit generally had lower bulk density and soil strength values than the other landscape positions. Moreover, soils planted to camote (Ipomoea batatas) had higher bulk density and soil strength values compared to soils grown to pepper under the trees. Exchangeable calcium (Ca), magnesium (Mg), and potassium (K) and cation exchange capacity (CEC) of the soils were generally higher in uncultivated areas than those of the cultivated areas. A similar trend was observed for the potassium permanganate ($KMnO_4$)-oxidizable organic C contents determined by spectroscopic method and the total C contents determined by the Walkley-Black method. The $KMnO_4$-oxidizable organic C contents determined by spectroscopic method and the total C contents determined by the Walkley-Black method were closely related ($r=0.631^{**}$). Hence, the former method shows promise in assessing soil quality as it is a rapid test, relatively low cost and can be distributed as a field kit either with a portable spectrometer or with a color chart.

• 대한토목학회논문집
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• 제30권2C호
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• pp.109-117
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• 2010

해저지반 내에 매장된 가스하이드레이트가 해리될 경우 많은 양의 가스와 물이 발생한다. 이렇게 발생한 가스와 물이 장기간에 걸쳐 외부로 빠져나가거나 주변 지반으로 이동할 경우 토체 안에는 크고 작은 공극이 형성될 수 있다. 그리고 지속적인 강우나 폭우로 인하여 지반 내의 조립질 흙 사이의 세립분이 유실되거나 고결성 지반 내의 일부 고결이 끊어지면서 골격 내에 빈 공간이 형성될 수 있다. 본 연구에서는 가스하이드레이트의 해리로 형성되거나 또는 유수작용으로 인하여 지반 내의 일부 재료가 유실되거나 용해되어 형성된 비교적 큰 공극이 지반의 강도에 미치는 영향을 연구하였다. 가스하이드 레이트를 포함한 토체나 유실성 지반의 골격을 시뮬레이션하기 위하여 입도가 균등한 글라스비즈를 사용하였다. 글라스비즈를 2%의 시멘트비와 7%의 함수비로 혼합하여 몰드 안에 5층으로 나누어 다져 원기둥 모양의 공시체를 만들었다. 흙입자에 비하여 상대적으로 큰 공극은 의약품에 일반적으로 사용되는 빈 캡슐을 넣어 형성하였다. 캡슐을 각층 높이의 중앙부분에 넣고 다음 층을 쌓아 다지는 방식으로 완성하였으며, 캡슐의 개수와 방향, 그리고 캡슐의 길이를 달리하면서 다양한 공시체를 제작하여 2일 동안 양생시킨 다음 일축압축시험을 실시하였다. 공시체 내에 형성된 공극(캡슐)의 체적(개수)과 방향 그리고 공극의 길이에 따라 공시체의 일축압축강도는 차이를 보였으며, 공시체 내에서 공극이 차지하는 체적과 단면적이 강도에 중요한 영향을 미쳤다. 공시체 내에 형성된 큰 공극으로 일축압축강도는 공극이 없는 공시체 강도의 최대 35%까지 감소하였다. 이와 같은 연구 결과는 가스하이드레이트 해리 후 지반의 장기적인 강도 변화와 지반 내의 세립분의 유실로 인한 강도 감소를 예측하는데 사용될 수 있다.

• 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.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2008년도 춘계 학술발표회 초청강연 및 논문집
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• pp.462-471
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• 2008

The quality control for DCM is based on the unconfined compressive strength of laboratory treated soils, the cement contents, setting and checking the strength of in-situ treated soils. Also the strength of in-situ is checked mainly by the core boring. In case of large size construction, it might be considered the distribution of DCM strength data as normal distribution, so it might be employed a statistical method to evaluate DCM strength easily. In Japan, it has been established correlation between the strength of laboratory treated soils, the strength of in-suit treated soil and the design strength. Also It has been employed domestically the correlation suggested by Japan. But the correlation, so called $\lambda$(ratio in the strength of laboratory treated soils and the in-suit) and $\gamma$(ratio in the strength of in-suit and the design strength), might be far different with the domestic due to different DCM system and soil properties. so it might be restrictive to use domestically. Therefore in this paper, It is presented correlation between the strength of laboratory treated soils and in-suit treated soil to be employed domestically by evaluating $\lambda$ based on the domestic in-suit illustrations.

• Geomechanics and Engineering
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• 제22권3호
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• pp.237-244
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• 2020

To achieve a wide suction range, the low suction was imposed on compacted silt specimens by the axis translation technique and the high suction was imposed by the vapor equilibrium technique with saturated salt solutions. Firstly, the results of soil water retention tests on compacted silt show that the soil water retention curves in terms of gravimetric water content versus suction relation are independent of the dry density or void ratio in a high suction range. Therefore, triaxial tests on compacted silt with constant water content at high suctions can be considered as that with constant suction. Secondly, the results of triaxial shear tests on unsaturated compacted silt with the initial void ratio of about 0.75 show a strain-hardening behavior with a slightly shear contraction and then strain-softening behavior with an obviously dilation. As the imposed suction increases, the shear strength increases up to a peak value and then decreases when the suction is beyond a special value corresponding to the peak shear strength. The residual strength increases to fair value and those at high suctions are almost independent of imposed suctions. In addition, the contribution of suction to the strength of compacted silt would not diminish even in a high suction range.

• 한국지반신소재학회논문집
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• 제5권3호
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• pp.25-30
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• 2006

흙 자체의 전단강도와 흙과 직포사이의 접촉면 전단강도를 산정하기 위해서 본 연구에서는 대형직접전단시험기를 사용하였다. 두 종류의 흙(모래와 점토)과 한 종류의 직포를 실험에서 사용하였다. 본 연구에서는 총 9번의 시험을 수행하였다. 그 결과, 모래 자체는 $30^{\circ}$의 내부마찰각을 나타내었다. 직포와 모래의 접촉면 마찰각은 $26^{\circ}$로 87%의 효율을 나타내었다. 이와 비슷하게 직포와 점토의 접촉면 마찰각은 $7.7^{\circ}$를 나타내었다.

• 한국농공학회지
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• 제31권2호
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• pp.43-53
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• 1989

In this research programs, a series test was conducted to show the effects of freeze/thaw process on the various soil properties. The tests were carried out taken from the west sea shore of Korean peninsular and the west sea shore of Scotland, and their results are as follows; 1. There was a positive total heave in a freezing run, although water may he expelled for the sample initially. The water flow must he reverse' from expulsion to intake. 2. The confining pressure had an overriding influence on the heave and frost penetration, a sudden change of the axial strain at failure with strain rate was observed occuring at a strain rate between 10-5 and 10-6, and the initial friction angle of frozen clay was appeared zero. 3. There was shown a significant decrease in liquid limit of soil which was subjected to freeze/thaw process for the initial value of about 20% because of soil particles aggregation. 4. The cyclic freeze/thaw caused a sinificant reduction in shear strength and its thixotropic regain. The frozen/thawed soil exibited negative strength regain, particularly at high freeze/thaw cycles. 5. The freezing temperature greatly influenced on the failure strength of soils and this. Trend was more pronounced the lower the freezing temperature and shown the ductile failure with indistinct peaks.

• 한국농공학회지
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• 제43권3호
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• pp.77-84
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• 2001

A few study has been performed on the durability of subbase treated with geo-cement for the farm road although many papers for the road treated with soil-cement were published. The objectives of the study are to develop the stabilizing method of subbase using additives of cement groups and 2nd additives such as gypsum and MgO, etc. A series of test was performed to investigate possible mixing ratios with geo-cement A, B, C, D and 2nd additives on the various soft soils from the rice paddy. Based on test results, durability index was greatly affected by geo-cement D which was mainly composed with gypsum. Compressive strength of clayey soil such as Soil I was less than threshold strength(30kgf/$\textrm{cm}^2$) but the strength was increased as addition of gypsum and MgO. It is recommended that geo-cement for soil stabilization has to be carefully chosen because strength characteristics of subbase are varied not only with soils but also with addition of geo-cement and 2nd additives. The developed method in this study can be used subbase treatment of low-cost agricultural roads.

• Structural Engineering and Mechanics
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• 제86권5호
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• pp.663-671
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• 2023

Freeze-thaw cycles induce strength loss at the frozen soil-concrete interface and deterioration of bonding, which causes construction engineering problems. To clarify the deterioration characteristics of the interface under the freeze-thaw cycle, a frozen soil-concrete sample was used as the research object, an interface scanning electron microscope test under the freeze-thaw cycle was carried out to identify the micro index information, and an interface shear test was carried out to explore the loss law of interface shear strength under the freeze-thaw cycle. The results showed that the integrity of the interface was destroyed, and the pore number and pore size of the interface increased significantly with the number of freeze-thaw cycles. The connection form gradually deteriorates from surface-to-surface contact to point-to-surface contact and point-to-point contact, and the interfacial shear strength decreases the most at 0-3 freeze-thaw cycles, with small decreases from to 3-8 cycles. After 12 freeze-thaw cycles, the interfacial shear strength tends to be stable, and shear the failure occurs internally in the soil.