• 한국농공학회논문집
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• 제51권1호
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• pp.11-20
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• 2009

Flow pump technique was used in order to determine the soil-water characteristic curve of weathered granite soils in Pocheon area. This technique enables measurement to be more convenient and accurate as it is based on the CU condition of triaxial compression test. Besides, it is also able to measure dry and moisture curves continuously since the test is controled by means of a computer automatically. In this study, not only a hydraulic conductivity of weathered granite soils at fully saturated state in Pocheon area, but also a soil-water characteristic curve throughout unsaturate flow tests were determined. In addition, Brooks and Corey's model and Genuchten's model were used to simulate the soil-water characteristic curve. On the basis of the simulation an unsaturate hydraulic conductivity was predicted.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2002년도 봄 학술발표회 논문집
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• pp.743-750
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• 2002

Unsaturated soil has a possibility to induce a negative pore water pressure. Until now, saturated soil is mainly focused on the research of soil mechanics. Recently, soil mechanics is researched on two major parts such as saturated and unsaturated soil mechanics. Negative pore water pressure has a non-linear relationship with the water content changes. Soil-water characteristic curves of soil in Korea are not determined. There is no proper characteristic value such as air-entry value and residual water content. In this study, the characteristic curves of reclaimed soil, sand, and weathered granite soil were determined by laboratory tests. Air-entry value and residual water content were determined by fitting methods. Soil-water characteristic curves were estimated based on the particle-size distribution and compared with the laboratory test results. The results of soil-water characteristic curves estimation indicated that Fredlund and Wilson's model is excellent for sand and weathered granite soil. Arya and Paris's model is excellent for reclaimed soil.

• 한국지반공학회논문집
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• 제22권7호
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• pp.55-64
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• 2006

풍화 사면은 지속적인 강우로 인하여 얕은층에서 파괴가 일어나고 있다. 이러한 파괴들은 주로 강우 침투로 지표면에서의 습윤대의 형성과 이로 인한 흡수력의 감소에 기인한다. 본 연구에서는 대표적인 풍화사면인 화강 풍화토 및 편마풍화토에 대한 함수특성곡선의 건조-습윤 이력과 선행강우 조건을 활용하여 시간에 따른 불포화 침투 해석을 인공적인 강우 강도와 지속시간을 설정하여 실시하였다. 그 결과 풍화 사면의 불포화 침투는 깊이별로 선행 강우에 의한 초기 흡수력과 이력에 따른 불포화 투수계수에 많은 영향을 받는 것으로 나타났다. 또한 화강풍화토가 편마풍화토 보다 상대적으로 작은 공기 함입값, 잔류 흡수력, 그리고 습윤 전면 흡수력을 가지고 있으며 이력 loop가 작아서 침투에 대한 흡수력의 변화 반응이 매우 빠름을 확인할 수 있었다.

• 한국지반공학회지:지반
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• 제13권6호
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• pp.13-24
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• 1997

화강풍화토는 국내 지반의 2/3이상을 차지할 정도로 광범위하게 분포하며 도로, 지하철, 사면조성, 건물의 기초설치 등 여러 건설현장에서 빈번히 접할 수 있다. 화강풍화토의 입자구조는 풍화정도와 모암의 구성광물에 의해 영향을 받고 특히 보통의 구속 암에서도 입자 파쇄가 발생하며 비교란 지반의 특성과 다짐토 지반의 특성이 큰 차이가 있다. 본 연구에서는 현장에서 직접 삼축시험용 비교란 화강풍화토시료를 채취할 수 있는 시료채취기를 개발하였고 이를 이용하여 채취한 비교란 시료와 정적으로 다져진 시료에 대하여 공진주/비틂 전단시험과 삼축압축시험을 수행하였다. 시험결과로부터 미소한 변형률에서의 거동특성과 비교란 및 다짐 화강풍화토의 강도특성을 검토하였다. 대상으로 한 지반의 경우 1% 이내의 미소한 변형률 영역에서는 다짐시료와 비교란시료의 탄성계수가 거의 일치하였으며 강도의 뚜렷한 차이 또한 발견할 수 없었다. 비교란화강풍화토의 경우는 시료의 불균일성 등으로 인하여 파괴시의 변형률이 매우 넘게 분포하였다.

• 한국지반공학회지:지반
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• 제12권6호
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• pp.139-152
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• 1996

불포화토에 대한 흐름문제를 해석하기 위해서는 비선형으로 표시되는 부간극수압과 함수비 사이의 관계를 알아야 한다. 본 논문에서는 주문진 표준사, 한강모래 및 세립함유율이 다른 몇가지 화강풍화토에 대하여 2가지 실험기구로 이 관계를 측정하고 그 특성을 규명하였다. 여기서 얻은 자료를 이용하여 이 관계를 실험없이 추정가능한 경험식에 쓰이는 경험상수들을 얻었다. 몇가지 경험식중 van Genuchten(1980)의 것이 실험곡선과 잘 부합된다. 화강풍화토에 대해서는 세립함유율(No.200체 통과율)의 증가에 따라 경험상수들도 거의 일정하게 증가하는 경향을 보인다는 것을 알게 되었다. 따라서 이 관계를 이용하여 화강풍화토에 대한 함수특성곡선의 추정이 가능하다.

• 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.

• 터널과지하공간
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• 제5권4호
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• pp.336-346
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• 1995

Geotechnical Information System (GTIS) for efficient management of three dimensional borehole data has been developed. Some problems were raised during the input process of borehole data, and alternative solutions were sought. According to the previous geotechnical reports, there is no unified weathering classification scheme. A criterion, 100 times/30cm from SPT, was turned out inappropriate to the discrimination of weathered rock from weathered soil. It has also been suggested that weathered soil, weathered rock, soft rock, and hard rock should be defined as CW, HW, MW, and SW~fresh condition. For better comparison of RQD, the use of NX size coring is recommended for the whole area although BX size coring has been used in excavated area. The limit of drilling depth up to 1 m from the top of surface of hard rock should be extended to avoid possible wrong interpretation of rock head due to the existence of corestone. The input data were analysed by geostatistical methods. It is found that the range in semivariogram is about 300m, and the variance of gneiss is greater than that of granite. It is because the granite data analysed came from almost single uniform rock mass(i.e.Seoul granite), but gneiss data came from the rock mass(i.e. Gyeonggi gneiss complex experienced several metamorphic metamorphic processes.

• 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.

• 지질공학
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• 제27권4호
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• pp.451-462
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• 2017

Physical weathering caused by external forces and chemical weathering caused by the decomposition or alteration of constituent materials are the two factors that dominate the mechanical properties of rocks. In this study, a field investigation was undertaken to identify the physical and chemical weathering characteristics of the biotite granite and granitic weathered soils in Gyeongju, South Korea. Samples were collected according to their grade of weathering and subjected to modal analysis, XRD analysis, XRF analysis, physical property tests, particle size distribution tests, and slake durability tests. Modal and XRD analysis identified these rocks as biotite granite; secondary alteration minerals were not observed. Physical property tests and particle size distribution analyses indicate an average porosity of 41.28% and a sand content of > 90 wt.%. These values are somewhat higher than those of granites in general. The results of the slake durability test and XRF analyses show that the physical and chemical weathering indices of the samples vary with the degree of weathering.

• 한국지형학회지
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• 제19권4호
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• pp.27-37
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• 2012

본 연구는 강원도 철원군 명성산 화강암과 현무암 용암대지 사이의 접촉대인 한탄강 승일교 인근 지역의 독특한 경관을 형성하고 있는 화강암 하천 침식 및 퇴적 지형과 풍화 지형 분석을 다루고 있다. 주요 화강암 지형으로서는 심층풍화된 구릉, 면상침식지형, 고지형면 및 고토양, 하천작용과 관련된 미지형으로 돌개구멍과 그루브, 램 파트형의 암괴, 사주와 사력퇴, 그리고 구하상 등이 있다. 그리고 풍화가 덜 진전된 구릉의 일부로 하천의 측방이동을 방해하는 화강암 하식애 지형이 있다.