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RISS 인기검색어
- 검색키워드
- 저자 : Sueng-Won Jeong (검색결과 19 건)
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Shear and viscous characteristics of gravels in ring shear tests
Sueng Won Jeong,Sung-Sik Park,Hiroshi Fukuoka 한국지질과학협의회 2018 Geosciences Journal Vol.22 No.1
The shear and viscous characteristics of a material are strongly dependent on the material’s properties, such as cementation, density and grain size distribution, as well as the testing conditions, such as drainage and shearing speed. More complex shear behaviors can occur when the tested materials have diverse grain sizes. The shear and viscous characteristics of gravels are examined in terms of drainage and shear velocity under the constant normal stress using a ring shear apparatus, in which the materials used can be sheared under a large deformation. In this study, the materials used are commercial aquarium gravels with mean diameter of 6 mm. Test results show that the materials typically exhibited strain-hardening behavior when subjected to low shear velocity (i.e., ≤ 0.01 mm/sec) and strain-softening behavior when subjected to high shear velocity (i.e., > 0.1 mm/sec) in the ring shear torque measuring system. As expected, higher shear velocities correspond to higher shear stresses, regardless of the drainage condition. For a given shear velocity (V) ranging from 0.01 to 1 mm/sec, a gradual decrease in shear stress is observed in the drained condition; however, a relatively constant shear stress is observed in undrained shear stress. It is clearly exhibited that the vertical displacement is large in the drained condition but relatively unchanged in the undrained condition. The grain crushing is significant for both drainage conditions when the materials experienced a large deformation. There are two regions: (a) non-dominant grain crushing and (b) dominant grain crushing (with a large amount of sand and fine contents) as a function of shear velocity. For both drainage conditions, a large shear resistance occurred when the shear velocity reaches 1 mm/sec. Through the contraction-particle rearrangement-grain crushing process during shear, when V ≥ 1 mm/sec, it appears that the shear stress is easily reached to the residual state of shear. The amounts of fine contents from grain crushing are much larger in the drained condition than in the undrained condition. In the extreme case that grains are highly crushed, it may result in a high mobilization of materials in natural hazards.
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Grain size dependent rheology on the mobility of debris flows
Sueng Won Jeong 한국지질과학협의회 2010 Geosciences Journal Vol.14 No.4
When dealing with natural geo-hazards it is important to understand the influence of flow characteristics on the submarine landslides, because the flow characteristics of fine-grained soils are most likely governed by the rheological properties. It may further relate to the mobility analysis of debris flow. Geotechnical and rheological investigation on the clay-rich materials were compared with those of silt-rich materials. For the examined fine-grained soils, the flow behavior depends on the volumetric concentration of solid and surface phenomenon, particularly for non-swelling materials. Assuming that the debris flow materials behave as the Bingham fluid, a possible relationship between geotechnical and rheological properties are proposed. From an empirical relationship between yield stress and plastic viscosity, a comparison emphasizes the grain size effect on the rheology of geomaterials encountered in various environments. The larger the particle size involved in the matrix, the lower the value of viscosity which is in the order of 10 times. Debris flow mobility with respect to rheology concerning the large particle size is emphasized.
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정승원,Jeong, Sueng Won 대한토목학회 2014 대한토목학회논문집 Vol.34 No.4
휴 폐광산지역은 복합지질재해지역으로 집중호우에 의해 토사재해와 산성광산배수를 발생시킨다. 본 연구는 폐석적치장 전반에 걸쳐 토사재해가 관측된 임기광산에 대해 지반공학적 유변학적 시험을 수행하고 얻어진 시험결과를 토대로 1-D 토석류 수치해석을 수행함으로써 토석류의 확산성을 조사하였다. 모래와 자갈로 구성된 광산폐석 시료의 유변학적 특성을 조사하기 위해 베인관입형 레오미터(Vane-penetrated rheometer)를 사용하였으며, 전단응력 제어를 통한 전단응력(${\tau}$)-전단속도(${\dot{\gamma}}$)와 점도(${\eta}$)-전단속도(${\dot{\gamma}}$) 간의 상관관계를 얻었다. 또한 광산폐석 시료에 대해 잘 알려진 유변학적 모델들(Bingham, Herschel-Bulkley, Power-law, bilinear 및 Papanastasiou 모델)을 적용함으로써 수치해석에 필요한 유변학적 매개변수(항복응력과 소성점도)를 결정하였다. 실험결과에 따르면, 체적농도에 무관하게 전형적인 전단담화(shear thinning) 거동이 관측되었으며, 함수비가 증가할수록 Bingham 유체처럼 거동하는 것으로 나타났다. 또한 사용된 모든 유변학적 모델들은 파괴 후 거동에 적합한 모델들로 밝혀졌다. 토석류 흐름특성을 조사하기 위해 실험결과를 토대로 토석류 크기(5 m, 10 m 및 15 m)와 항복응력(100 Pa, 200 Pa, 300 Pa 및 500 Pa)을 선정하여 1-D BING을 통해 수치해석을 수행하였다. 그 결과, 토석류 이동거리와 이동속도는 항복응력의 크기에 반비례한 것으로 나타났으며, 토석류 항복응력이 500 Pa 이하인 경우 대부분의 토사는 계곡부까지 흘러갈 수 있는 것으로 나타났다. 따라서 집중호우 기간에 산악지역에 방치된 광산폐석은 토사재해에 취약하고 2차적으로 인근 수계로 유입되어 환경적 문제를 야기시킬 수 있는 것으로 나타났다. Abandoned mines often cause environmental problems, such as alteration of landscape, metal contamination, and landslides due to a heavy rainfall. Geotechnical and rheological tests were performed on waste materials corrected from Imgi waste rock dump, located in Busan Metropolitan City. Debris flow mobility was examined with the help of 1-D BING model which was often simulated in both subaerial and subaqueous environments. To determine flow curve, we used a vane-penetrated rheometer. The shear stress (${\tau}$)-shear rate (${\dot{\gamma}}$) and viscosity(${\eta}$)-shear rate (${\dot{\gamma}}$) relationships were plotted using a shear stress control mode. Well-known rheological models, such as Bingham, bilinear, Herschel-Bulkley, Power-law, and Papanastasiou concepts, were compared to the rheological data. From the test results, we found that the tested waste materials exhibited a typical shear shinning behavior in ${\tau}$-${\dot{\gamma}}$ and and ${\eta}$-${\dot{\gamma}}$ plots, but the Bingham behavior is often observed when the water contents increased. The test results show that experimental data are in good agreement with rheological models in the post-failure stage during shearing. Based on the rheological properties (i.e., Bingham yield stress and viscosity as a function of the volumetric concentration of sediment) of waste materials, initial flowing shape (5 m, 10 m, and 15 m) and yield stress (100 Pa, 200 Pa, 300 Pa, and 500 Pa) were input to simulate the debris flow motion. As a result, the runout distance and front velocity of debris flow are in inverse propositional to yield stress. In particular, when the yield stress is less than 500 Pa, most of failed masses can flow into the stream, resulting in a water contamination.
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정승원,Jeong, Sueng-Won 한국지반공학회 2013 한국지반공학회논문집 Vol.29 No.1
기후변화에 따른 토석류 발생과 그로 인한 피해가 세계적으로 증가 추세에 있다. 토석류 연구는 역학적 관점에서 파괴 후(post-failure) 거동에 해당하며 지반강도와 유동특성을 분석함으로써 특성화할 수 있다. 본 연구는 국내의 토석류 발생지역인 상주(화강암 풍화토), 인제(편마암 풍화토), 포항(이암 및 셰일) 지역을 대상으로 지반의 물성-전단강도 상관관계와 토석류의 유동특성을 평가하였다. 본 연구지역을 대상으로 스웨덴 낙하 콘(Swedish Fall cone) 시험장치를 이용하여 지반의 물성 및 지반강도 사이에 일정한 상관관계가 있음을 밝혔다. 실험결과에 따르면, 인제, 상주, 포항지역에서 채취된 시료에 대해 액성지수(IL)와 비배수 전단강도($C_{ur}$) 사이에 $C_{ur}=(1.2/I_L)^{3.3}$의 관계식이 성립한다. 토석류 흐름을 지배하는 항복응력은 재성형 비배수 전단강도에 상응하는 것으로 간주하고, Bingham 모델과 액성지수-항복응력 관계식을 이용하여 토석류의 유동성을 조사하였다. 유동해석은 국내 풍화토와 낮은 활성점토를 구분하여 적용하였다. 이때 액성지수는 액성한계를 기준으로 $I_L=1$, 1.5, 3.0으로 구분하여 비교분석하였다. 동일한 액성지수($I_L=1$)에 대해, 토석류의 발생 5분 경과 후 최대 이동거리는 250m에 다다른다. 액성지수가 3으로 증가 될 경우, 토석류의 이동거리를 5분까지 살펴본 결과, 국내 풍화토는 낮은 활성점토에 비해 2배 이상 큰 유동성이 있음을 알 수 있었다. 본 유동성 평가기술은 토석류 피해저감기술 전략수립에 활용할 수 있을 것으로 기대된다. The risks of debris flows caused by climate change have increased significantly around the world. Recently, landslide disaster prevention technology is more focused on the failure and post-failure dynamics to mitigate the hazards in flow-prone area. In particular, we should define the soil strength and flow characteristics to estimate the debris flow mobility in the mountainous regions in Korea. To do so, we selected known ancient landslides area: Inje, Pohang and Sangju debris flows. Firstly we measured physical and mechanical properties: liquidity index and undrained shear strength by fall cone penetrometer. From the test results, we found that there is a possible relationship between liquidity index and undrained shear strength, $C_{ur}=(1.2/I_L)^{3.3}$, in the selected areas, even though they were different in geological compositions. Assuming that the yield stress is equal to the undrained shear strength at the initiation of sliding, we examined the flow characteristics of weathered soils in Korea. When liquidity index is given as 1, 1.5 and 3.0, the debris flow motion of weathered soils is compared with that of mud-rich sediments, which are known as low-activity clays. At $I_L=1$, it seems that debris flow could reach approximately 250m after 5 minutes. As liquidity index increased from 1 to 3, the debris flow propagation of weathered soils is twice than that of low-activity clays. It may be due to the fact that soil masses mixed with the ambient water and then highly fragmented during flow, thereby leading to the high mobility. The results may help to predict the debris flow propagation and to develop disaster prevention technology at similar geological settings, especially for the weathered soils, in Korea.
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정승원 ( Sueng Won Jeong ) 대한지질공학회 2016 지질공학 Vol.26 No.3
흙의 전단특성을 조사하기 위하여 다양한 전단시험장치가 사용되고 있다. 특히 흙의 무한변형에 따른 잔류전단강도(residualshear strength)를 측정하고자 할 경우 링전단시험장치가 사용된다. 본 연구는 배수, 압밀 및 전단속도 제어가 가능한 비배수전단강도 측정용 링전단시험장치를 사용하여 전단동안 발생하는 누수현상(water leakage)이 전단특성에 미치는 영향성에 대하여 조사하였다. 실험은 비배수조건에서 동일한 수직응력(50 kPa)을 재하하고 전단속도(0.01, 0.1, 1 mm/sec)를 3단계로 구분하여 적용하였다. 실험결과에 따르면, 동일한 수직응력에서 비배수전단강도는 전단속도에 의존하는 것으로 나타났다. 하지만, 상대적으로 낮은 전단속도(V = 0.01 mm/sec)에서는 변형률 경화 거동(strain hardening behavior)을 보였고 상대적으로 높은 전단속도(V≥ 0.1 mm/sec)에서는 변형률 연화 거동(strain softening behavior)을 보였다. 시험기 성능평가를 통하여 누수가 발생할 경우 전단속도 크기에 관계없이 전단응력은 증가하는 것으로 나타났다. 누수가 크면 클수록 전단응력이 증가된다. 이러한 실험결과는 전단동안 발생하는 누수로 인한 흙 입자의 재배열과 다짐도의 증가에 따른 것으로 판단된다. 따라서 육안조사 및 반복적인 포화와 압밀과정을 통하여 실험오차를 최소화할 수 있는 작업이 필요하다. Shear characteristics of soils can be investigated using various types of shear stress measuring apparatus. Ring shear tests are often applied for examining the residual shear strength under the unlimited deformation. This paper presents drainage-consolidation- shear velocity dependent undrained shear strengths measured in terms of water leakage. A series of ring shear tests were performed under the constant normal stress (50 kPa) and controled shear velocity ranging from 0.01~1 mm/sec under the undrained condition. As a result, undrained shear strengths are dependent on shear velocity. It exhibits that straining hardening behavior is observed for the shear velocity lower than 0.1 mm/sec; however, the strain softening behavior is observed for the shear velocity higher than 0.1 mm/sec. Water leakage can cause the increase in shear stress irrespective of shear velocity. Shear stress increases with increasing amount of water leakage. It is due to the fact that the small grains and water flow out through the rubble edge in the ring shear box. Repetitive saturation and consolidation processes may minimize the error.
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전승원(Jeong, Sueng-Won) 한국지반공학회 2013 한국지반공학회논문집 Vol.29 No.1
The risks of debris flows caused by climate change have increased significantly around the world. Recently, landslide disaster prevention technology is more focused on the failure and post-failure dynamics to mitigate the hazards in flow-prone area. In particular, we should define the soil strength and flow characteristics to estimate the debris flow mobility in the mountainous regions in Korea. To do so, we selected known ancient landslides area: Inje Pohang and Sangju debris flows. Firstly we measured physical and mechanical properties: liquidity index and undrained shear strength by fall cone penetrometer. From the test results, we found that there is a possible relationship between liquidity index and undrained shear strength, C<sub>ur</sub>=( 1.2/I<sub>L</sub>)<sup>3.3</sup>, in the selected areas, even though they were different in geological compositions. Assuming that the yield stress is equal to the undrained shear strength at the initiation of sliding, we examined the flow characteristics of weathered soils in Korea. When liquidity index is given as 1, 1.5 and 3.0, the debris flow motion of weathered soils is compared with that of mud-rich sediments, which are known as low-activity clays. At I<sub>L</sub> = 1, it seems that debris flow could reach approximately 250m after 5 minutes. As liquidity index increased from 1 to 3, the debris flow propagation of weathered soils is twice than that of low-activity clays. It may be due to the fact that soil masses mixed with the ambient water and then highly fragmented during flow, thereby leading to the high mobility. The results may help to predict the debris flow propagation and to develop disaster prevention technology at similar geological settings, especially for the weathered soils, in Korea.
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