• 한국산학기술학회논문지
• /
• 제19권5호
• /
• pp.146-152
• /
• 2018

본 연구에서는 국내에서 주로 발생하는 소성변형에 대한 아스팔트 혼합물의 성능개선을 위해 분말형 및 액상형 재료를 혼합한 복합 개질제를 이용하였다. 주요 구성 물질은 분말형인 규조토, 운모 및 카본블랙, 액상형 고형분 70% SBR(Styrene-Butanaiene Rubber) 라텍스 등을 이용하였다. 시험에 사용된 2종류의 표층용 혼합물에 대한 인장강도비는 국토교통부(2017) 아스팔트 혼합물 생산 및 시공지침 기준인 0.80 이상을 만족하였다. 복합개질제를 첨가한 경우 건조상태에서의 인장강도 증가효과가 약 14% 이상 나타났다. 휠트레킹 시험 하중에 의한 분당변형속도는 0.07-0.14 정도로 복합 개질제 사용 시 분당 변형속도가 개선되었고, 동적안정도의 경우 295에서 590으로 거의 100% 정도 향상되었다. 또한, 최종 침하량은 11.38mm에서 9.57mm로 저감되었다. 동삼축압축시험을 이용한 소성변형 시험결과, 2단계 구간이 끝나고 3단계 소성변형파괴구간에 진입하는 변형량의 크기는 평균 1.50mm에서 1.76mm,나타났다. 또한, 2단계 구간의 시간당 변형 기울기는 기존 아스팔트 혼합물은 0.007 mm/sec 이고, 복합 개질제를 혼합한 아스팔트 혼합물의 평균기울기는 0.005 mm/sec 정도로 도로포장체가 안정적인 공용성능을 발휘하는 구간에서 교통하중에 의한 소성변형 속도가 상대적으로 작음을 알 수 있다.

• 한국지반환경공학회 논문집
• /
• 제23권8호
• /
• pp.23-28
• /
• 2022

우리나라 지형조건은 산악이 70%를 차지하고 있어 철도 및 도로공사 시 구조물이 차지하는 비중이 높다. 특히, 최근 들어 고속주행을 위한 고속철도와 고속도로 건설이 급증하고 있고 이와 더불어 터널 건설도 증가하고 있고 터널 굴착 완료 후 장기변형이 발생하는 터널 시공사례가 증가하는 추세이다. 이러한 터널 구조물의 안정성은 터널 굴착 주변 암반특성에 전적으로 좌우된다. 본 연구에서 대상인 화산쇄설암의 경우, 전반적으로 풍화에 취약하고 장기간에 걸쳐 강도가 저하되는 특성이 있어서 이를 고려한 터널 설계 및 시공계획 수립이 반드시 필요하다. 본 연구는 화산쇄설암 구간에 터널 현장에서 발생 된 과다변형 사례를 분석하여 향후 화산쇄설암 구간에서는 인버트 설치 및 하부보강을 고려한 방안을 제시하였다.

• 토지주택연구
• /
• 제11권2호
• /
• pp.95-104
• /
• 2020

This study aims to explore a purely mechanistic pavement analysis approach where viscoelasticity and fracture of asphalt mixtures are considered to accurately predict deformation and damage behavior of flexible pavements. To do so, the viscoelastic and fracture properties of designated pavement materials are obtained through experiments and a fully mechanistic damage analysis is carried out using a finite element method (FEM). While modeling crack development can be done in various ways, this study uses the cohesive zone approach, which is a well-known fracture mechanics approach to efficiently model crack initiation and propagation. Different pavement configurations and traffic loads are considered based on three main functional classes of roads suggested by FHWA i.e., arterial, collector and local. For each road type, three different material combinations for asphalt concrete (AC) and base layers are considered to study damage behavior of pavement. A concept of the approach is presented and a case study where three different material combinations for AC and base layers are considered is exemplified to investigate progressive damage behavior of pavements when mixture properties and layer configurations were altered. Overall, it can be concluded that mechanistic pavement modeling attempted in this study could differentiate the performance of pavement sections due to varying design inputs. The promising results, although limited yet to be considered a fully practical method, infer that a few mixture tests can be integrated with the finite element modeling of the mixture tests and subsequent structural modeling of pavements to better design mixtures and pavements in a purely mechanistic manner.

• 대한원격탐사학회:학술대회논문집
• /
• 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
• /
• pp.460-464
• /
• 2002

Multitemporal interferometric SAR has became an useful geodetic tool for monitoring Earth's surface deformation, generation of precise DEM, and land cover classification even though there still exist certain constraints such as temporal and spatial decorrelation effects, atmospheric artifacts and inaccurate orbit information. The Korea where nearly all areas are heavily vegetated, JERS-1 SAR has advantages in monitoring surface deformations and environmental changes in that it uses 4-times longer wavelength than ERS-l/2 or RADARSAT SAR system. For generating differential SAR interferogram and differential coherence image fer deformation mapping and temporal change detection, respectively, topographic phase removal process is required utilizing a reference inteferogram or external DEM simulation. Because the SAR antenna baseline parameter for JERS-1 is less accurate than those of ERS-l/2, one can not estimate topographic phases from an external DEM and the residual phase appears in differential interferogram. In this paper, we examined topographic phase retrieval method utilizing an external DEM. The baseline refinement is carried out by minimizing the differences between the measured unwrapped phase and the reference points of the DEM.

• Journal of Ecology and Environment
• /
• 제39권1호
• /
• pp.11-16
• /
• 2016

Declines in amphibian populations are occurring worldwide, and have been attributed to many factors, including anthropogenic environmental changes. One of the ramifications of such declines is abnormalities in many amphibian species. A strong association has been detected between human activities and abnormalities in amphibian populations, but studies on this association are largely focused on lentic species. In this study, it was analyzed whether the degree of local human activity was associated with the rate of abnormalities in Bombina orientalis which inhabited lotic environments. We found that the proportions of abnormalities in wild populations of B. orientalis increased, when i) the closest human land use was located within 100 m from the frogs' habitat, and ii) the proportion of human land use within a 300-m radius was high. Our findings suggest that human activity has a negative impact on the fitness of nearby amphibian populations, and that wild populations very close to human-induced disturbance are affected.

• 대한원격탐사학회:학술대회논문집
• /
• 대한원격탐사학회 2008년도 International Symposium on Remote Sensing
• /
• pp.414-417
• /
• 2008

We have extracted a surface deformation map of a part of Canisteo Peninsula on Amundsen Sea in West Antarctica by applying 4-pass DInSAR technique to two ERS-1/2 tandem pairs obtained on October 21-22, 1995 (diff-pair) and March 9-10, 1996 (topo-pair), and analyzed changes of glaciers, sea ice, ice shelves, and their kinematic interactions. We observed fast motion of glaciers pushing the adjoining sea ice. Some interferometric phases indicate the up-rise of sea ice of which type is thought to be land-fast ice to exert repulsive force against the pushing glacier. There were other glaciers and sea ice that moved to the same direction, suggesting that the sea ice in these regions was land-fast ice weakly harnessed to sea bottom or pack ice not harnessed at all. Several small circular fringes in ice shelves suggested that islands or seamounts on the bottom of ice shelves deterred the movement of ice shelves, resulting in the rise of ice surface.

• 토지주택연구
• /
• 제4권1호
• /
• pp.125-131
• /
• 2013

얕은 기초 설계와 시공을 위해 실시하는 평판재하시험 결과로부터 실제 기초지반의 침하량을 산정하고 있는데 국내에서 많이 시공되는 화강풍화토나 풍화암에 대한 현장 예측식이 없는 실정이다. 따라서, 본 연구에서는 화강풍화토와 풍화암을 대상으로 현장 평판 재하시험을 실시하여 기초 크기별 침하량 거동을 분석하였다. 모형토조와 현장 재하시험에서 측정한 하중 ~ 침하 곡선을 일반적인 항복하중 판정법을 사용하지 않고 하중 ~ 상대침하(s/B, s : 침하량, B : 재하판폭) 관계로 정규화(Normalization)하여 분석하였다. 즉, 하중 ~ 상대 침하 개념으로 정규화한 결과, 재하판 직경에 관계없이 일정한 형태의 곡선을 나타내므로 현장의 지반조건과 상관성을 제시하였다.

• Geomechanics and Engineering
• /
• 제13권1호
• /
• pp.1-23
• /
• 2017

A coupled liquid-gas-solid three-phase model, linking two numerical codes (TOUGH2/EOS3 and $FLAC^{3D}$), was firstly established and validated by simulating an in-situ air flow test in Essen. Then the coupled model was employed to investigate responses of multiphase flow and soil skeleton deformation to compressed air or freshwater injection using the same simulation conditions in an aquifer of Tianjin, China. The simulation results show that with injecting pressurized fluids, the vertical effective stress in some area decreases owing to the pore pressure increasing, an expansion of soil skeleton appears, and land uplift occurs due to support actions from lower deformed soils. After fluids injection stops, soil deformation decreases overall due to injecting fluids dissipating. With the same applied pressure, changes in multiphase flow and geo-mechanical deformation caused by compressed air injection are relatively greater than those by freshwater injection. Furthermore, the expansion of soil skeleton induced by compressed air injection transfers upward and laterally continuously with time, while during and after freshwater injection, this expansion reaches rapidly a quasi-steady state. These differences induced by two fluids injection are mainly because air could spread upward and laterally easily for its lower density and phase state transition appears for compressed air injection.

• 대한원격탐사학회지
• /
• 제33권1호
• /
• pp.37-46
• /
• 2017

Sinabung volcano in Indonesia was formed due to the subduction between the Eurasian and Indo-Australian plates along the Pacific Ring of Fire. After being dormant for about 400 years, Sinabung volcano erupted on the 29th of August, 2010 and most recently on the 1st of November, 2016. We measured the deformation of Sinabung volcano using Advanced Land Observing Satellite/Phased Array type L-band Synthetic Aperture Radar(ALOS/PALSAR) interferometric synthetic aperture radar(InSAR) images acquired from February 2007 to January 2011. Based on multi-temporal InSAR processing, we mapped the ground surface deformation before, during, and after the 2010 eruption with time-series InSAR technique. During the 3 years before the 2010 eruption, the volcano inflated at an average rate of ~1.7 cm/yr with a markedly higher rate of 6.6 cm/yr during the 6 months prior to the 2010 eruption. The inflation was constrained to the top of the volcano. From the 2010 eruption to January 2011,the volcano subsided by approximately 3 cm (~6 cm/yr). We interpreted that the inflation was due to magma accumulation in a shallow reservoir beneath Sinabung. The deflation was attributed to magma withdrawal from the shallow reservoir during the eruption as well as thermo-elastic compaction of erupted material. This result demonstrates once again the utility of InSAR for volcano monitoring.

• 대한원격탐사학회지
• /
• 제21권1호
• /
• pp.73-81
• /
• 2005

We construct improved geocentric digital elevation model (DEM), estimate tidal dynamics and ice stream velocity over Sulzberger Ice Shelf, West Antarctica employing differential interferograms from 12 ERS tandem mission Synthetic Aperture Radar (SAR) images acquired in austral fall of 1996. Ice, Cloud, and land Elevation Satellite (ICESat) laser altimetry profiles acquired in the same season as the SAR scenes in 2004 are used as ground control points (GCPs) for Interferometric SAR (InSAR) DEM generation. 20 additional ICESat profiles acquired in 2003-2004 are then used to assess the accuracy of the DEM. The vertical accuracy of the OEM is estimated by comparing elevations with laser altimetry data from ICESat. The mean height difference between all ICESat data and DEM is -0.57m with a standard deviation of 5.88m. We demonstrate that ICESat elevations can be successfully used as GCPs to improve the accuracy of an InSAR derived DEM. In addition, the magnitude and the direction of tidal changes estimated from interferogram are compared with those predicted tidal differences from four ocean tide models. Tidal deformation measured in InSAR is -16.7cm and it agrees well within 3cm with predicted ones from tide models. Lastly, ice surface velocity is estimated by combining speckle matching technique and InSAR line-of-sight measurement. This study shows that the maximum speed and mean speed are 509 m/yr and 131 m/yr, respectively. Our results can be useful for the mass balance study in this area and sea level change.