• 제목/요약/키워드: surface and subsurface interaction

검색결과 26건 처리시간 0.033초

유한요소법을 이용한 미끄럼 접촉시 내부 복수 수평균열 전파해석 (Finite Element Analysis of Subsurface Multiple Horizontal Cracks Propagation in a Half-space Due to Sliding Contact)

  • 이상윤;김석삼;권영두
    • Tribology and Lubricants
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    • 제16권5호
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    • pp.373-380
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    • 2000
  • Finite element analysis is performed on the subsurface crack propagation in brittle materials due to sliding contact. The sliding contact is simulated by a rigid asperity moving across the surface of an elastic half-surface containing single and multiple cracks. The single crack, coplanar cracks and parallel cracks are modeled to investigate the interaction effects on the crack growth in contact fatigue. The crack location is fixed and the friction coefficients between asperity and half-space are varied to analyze the effect of surface friction on stress intensity factor for horizontal cracks. The crack propagation direction is predicted based on the maximum range of shear and tensile stress intensity factors. With a coplanar crack, the stress intensity factor was increased. However, with a parallel crack, the stress intensity factor was decreased. These results indicate that the interaction of a coplanar crack increases fatigue crack propagation, whereas that of a parallel crack decreases it.

Calibration and uncertainty analysis of integrated surface-subsurface model using iterative ensemble smoother for regional scale surface water-groundwater interaction modeling

  • Bisrat Ayalew Yifru;Seoro Lee;Woon Ji Park;Kyoung Jae Lim
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2023년도 학술발표회
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    • pp.287-287
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    • 2023
  • Surface water-groundwater interaction (SWGI) is an important hydrological process that influences both the quantity and quality of water resources. However, regional scale SWGI model calibration and uncertainty analysis have been a challenge because integrated models inherently carry a vast number of parameters, modeling assumptions, and inputs, potentially leaving little time and budget to explore questions related to model performance and forecasting. In this study, we have proposed the application of iterative ensemble smoother (IES) for uncertainty analysis and calibration of the widely used integrated surface-subsurface model, SWAT-MODFLOW. SWAT-MODFLOW integrates Soil and Water Assessment Tool (SWAT) and a three-dimensional finite difference model (MODFLOW). The model was calibrated using a parameter estimation tool (PEST). The major advantage of the employed IES is that the number of model runs required for the calibration of an ensemble is independent of the number of adjustable parameters. The pilot point approach was followed to calibrate the aquifer parameters, namely hydraulic conductivity, specific storage, and specific yield. The parameter estimation process for the SWAT model focused primarily on surface-related parameters. The uncertainties both in the streamflow and groundwater level were assessed. The work presented provides valuable insights for future endeavors in coupled surface-subsurface modeling, data collection, model development, and informed decision-making.

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대도시 복합유역의 지표 및 지표하 유출해석기법 개발 (I)- 이론 및 모듈의 개발 - (A Development of Method for Surface and Subsurface Runoff Analysis in Urban Composite Watershed (I) - Theory and Development of Module -)

  • 곽창재;이재준
    • 한국수자원학회논문집
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    • 제45권1호
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    • pp.39-52
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    • 2012
  • 유역내에서 발생하는 유출은 지표 유출과 지표하 유출이 있으며, 서로 상호작용 상태를 유지하게 된다. 일반적으로 지표와 지표하 둘 중 한 가지 알고리즘으로 해석이 힘든 유역에 대해 지표와 지표하 사이의 동적인 관계를 상세하게 모의해야 하는 경우 상호작용에 관한 요소를 고려하여야 한다. 동적인 상호작용 시스템의 구동에서는 시 공간적인 매개변수가 중요하며, 적절한 모의를 위해시 공간적인 매개변수는 시스템 상에서 지표와 지표하 항에 대한 복합적인 메카니즘으로 구성되어야 한다. 본 연구에서는 이러한 지표 및 지표하 유출의상호작용에 관한 알고리즘을 위해 2차원 확산파 방정식을 이용하여 지표 유출을 해석하고, Darcy의 법칙과 Dupuit-Forchheimer의 가정을 이용한 Boussinesq 방정식을 적용하여 포화상태의 지표하 유출의 알고리즘을 구성하였다. 커플링 방정식으로 공간에 대해서는 유한체적법을 사용하고, 시간에 대해서는 Crank-Nicolson 방법을 이용하였으며, 지표와 지표하 흐름의 상호작용에 대해서는 질량보존의 법칙에 기반하여 구성하였다. 이상의 과정을 통하여 지표 유출해석, 지표하 유출해석, 상호작용, 수치해석 부분의 4가지 주요 모듈을 만들었으며, 4가지 주요 모듈을 통합하여 복합유역의 지표 및 지표하 유출해석 모듈을 개발하였다.

Synthetic storm sewer network for complex drainage system as used for urban flood simulation

  • Dasallas, Lea;An, Hyunuk;Lee, Seungsoo
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2021년도 학술발표회
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    • pp.142-142
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    • 2021
  • An arbitrary representation of an urban drainage sewer system was devised using a geographic information system (GIS) tool in order to calculate the surface and subsurface flow interaction for simulating urban flood. The proposed methodology is a mean to supplement the unavailability of systematized drainage system using high-resolution digital elevation(DEM) data in under-developed countries. A modified DEM was also developed to represent the flood propagation through buildings and road system from digital surface models (DSM) and barely visible streams in digital terrain models (DTM). The manhole, sewer pipe and storm drain parameters are obtained through field validation and followed the guidelines from the Plumbing law of the Philippines. The flow discharge from surface to the devised sewer pipes through the storm drains are calculated. The resulting flood simulation using the modified DEM was validated using the observed flood inundation during a rainfall event. The proposed methodology for constructing a hypothetical drainage system allows parameter adjustments such as size, elevation, location, slope, etc. which permits the flood depth prediction for variable factors the Plumbing law. The research can therefore be employed to simulate urban flood forecasts that can be utilized from traffic advisories to early warning procedures during extreme rainfall events.

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A self-consistent model for the formation and eruption of a solar prominence

  • Magara, Tetsuya
    • 천문학회보
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    • 제46권2호
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    • pp.47.2-47.2
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    • 2021
  • The present study is focused on origins of the flow and magnetic structure involved in the formation and eruption of a solar prominence. To clarify them, we performed an MHD simulation based on the 3-dimensional emerging flux tube (3DEFT) model, in which self-consistent evolution of a flow and magnetic field passing freely through the solar surface was obtained by seamlessly connecting subsurface dynamics with surface dynamics. By analyzing Lagrangian displacements of magnetized plasma elements, we demonstrate the flow structure which is naturally incorporated to the magnetic structure of the prominence formed via dynamic interaction between the flow and magnetic field.

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Chemical Bonding and Surface Electronic Structures of Pt3Co (111), Pt3Ni (111) Single Crystals

  • Kim, Yong-Su;Jeon, Sang-Ho;Bostwick, Aaron;Rotenberg, Eli;Ross, Philip N.;Stamenkovic, Vojislav R.;Markovic, Nenad M.;Noh, Tae-Won;Han, Seung-Wu;Mun, Bong-Jin Simon
    • 한국진공학회:학술대회논문집
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    • 한국진공학회 2012년도 제43회 하계 정기 학술대회 초록집
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    • pp.139-139
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    • 2012
  • With angle resolved photoemission spectroscopy (ARPES), the surface electronic band structures of Pt3Co (111) and Pt3Ni (111) single crystals are investigated, which allow to study the bonding interaction between chemically absorbed atomic oxygen and its surfaces. The d-band electrons of subsurface TM are separated from the direct chemical bonding with atomic oxygen. That is, the TM does not contribute to direct chemical bonding with oxygen. From the density functional theory (DFT) calculations, it is identified that the main origin of improved oxygen absorption property, i.e. softening of Pt-O bonding, is due to the suppression of Pt surface-states which is generated from change of interlayer potential, i.e. charge polarization, between Pt-top and TM-subsurface. Our results point out the critical roles of subsurface TM in modifying surface electronic structures, which in turn can be utilized to tune surface chemical properties.

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대규모 육지수문모형에서 사용 가능한 지표면 및 지표하 연계 물흐름 모형의 개발: II. 모형적용 (Development of a Conjunctive Surface-Subsurface Flow Model for Use in Land Surface Models at a Large Scale: Part II. Model Implementation)

  • 최현일
    • 한국방재학회 논문집
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    • 제8권3호
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    • pp.23-27
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    • 2008
  • 대규모 육지수문모형(Land Surface Model, LSM)에서 종합적인 육지 물흐름 및 에너지흐름의 예측을 위해 새로운 지표면-지표하 연계 물흐름 모형이 지표하 물흐름 모의를 위한 3차원 체적평균 토양수분 이송방정식(Volume Averaged Soil-moisture Transpor, VAST)을 지표수 흐름모의를 위한 1차원 확산방정식과 연계하여 개발되었다. 각 흐름특성에 맞는 복합적인 수치해석법이 적용되어, 시간분할 방법에 의해 3차원 VAST 방정식의 종방향 흐름이 완전음해법에 의해 해석된 후, 횡방향 흐름이 양해법으로 구해지며, 그 후에 1차원 확산방정식은 MacCormack 유한차분법으로 계산한다. 이 새로운 흐름연계모형은 최신의 육지수문모형인 CLM(Common Land Model)내의 기존 1차원 수리수문계산부분을 대체하게 된다. CLM과 결합된 새로운 연계흐름모형은 오하이오 계곡부근의 시험유역에 적용되었으며, 모의결과는 지표면-지표하 물흐름 상호작용의 모의와 지표수 흐름추적방법을 사용한 새로운 모형의 유출예측이 실측치에 더 근접함을 보여준다. 이 개선된 육지수문모형은 지역적, 대륙적, 그리고 지구전체를 다루는 수문기상연구와 기후변화로 인한 재해예방을 위하여 기상모형인 CWRF(Climate extension of the next-generation Weather Research and Forecasting)와 연계될 예정이다.

분포형 유역 모델을 이용한 하천-지하수 상호작용의 시공간적 변동 해석: 영국 Tarland Burn 유역에 대한 사례 연구 (Analysis of Temporal and Spatial Variations of Channel-Aquifer Interaction Using a Distributed Catchment Model: A Case Study for the Tarland Burn Catchment in the UK)

  • 구본경
    • 한국수자원학회:학술대회논문집
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    • 한국수자원학회 2007년도 학술발표회 논문집
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    • pp.253-257
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    • 2007
  • Channel-aquifer interaction is one of the key hydrological processes that determine water flows in the stream/river channel. Field measurements of channel-aquifer interaction, however, is very difficult and costly, particularly when one intends to understand its variations across a catchment for a long period. Hydrological simulations using a catchment model are a relatively easier and cheaper alternative provided the model structure is appropriate for describing channel-aquifer interaction. In this study, a catchment model called CAMEL (Chemicals from Agricultural Management and Erosion Losses) is used for estimating channel-aquifer interaction over time and space. CAMEL is a distributed catchment model to simulate transformation and transport processes of sediment and pollutants as well as water flows at the catchment scale. In the model, a catchment is represented using a network of square columns each of which is comprised of various storages of water. CAMEL explicitly simulates both surface and subsurface processes including channel-aquifer interaction. This paper presents an application study results of CAMEL for the Tarland Burn Catchment, a small (catchment area $52\;km^2$) rural catchment in Scotland, UK, demonstrating some of the channel-aquifer interaction dynamics across the catchment during a 2-year period.

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급경사면의 세류간 침식에서 빗물튀김과 면상흐름의 상호작용 (Interaction between Raindrops Splash and Sheet Flow in Interrill Erosion of Steep Hillslopes)

  • 남명준;박상덕;이승규;신승숙
    • 한국수자원학회논문집
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    • 제48권7호
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    • pp.595-604
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    • 2015
  • 강우에 의한 세류간 토양침식은 운동에너지를 갖는 빗방울이 지표면을 타격하여 발생하는 빗물튀김의 박리현상과 지표유출수의 면상흐름에 의한 토사입자의 운반으로 구분할 수 있다. 강우운동에너지는 토양입자를 토양체로부터 분리시키기 위한 강우의 잠재적인 능력의 지표로 널리 사용되고 있다. 본 연구에서는 강우운동에너지가 세류간 토양침식에 미치는 영향을 파악하기 위해 강우의 충돌을 제어하는 스트립 커버를 이용한 토양침식 강우모의 실험을 수행하였다. 강우모의에 의한 강우운동에너지는 자연강우에 비해 0.58배 규모로 재현되었다. 강우강도가 증가함에 따라 지표유출량은 증가하고 지표하유출량은 상대적으로 감소하였다. 지표커버가 없는 사면으로부터 발생한 지표유출량이 지표커버가 있는 경우에 비해 평균 1.82배 증가하였다. 강우운동에너지는 지표유출 및 지표하유출 발생시간에도 영향을 끼쳤다. 빗물튀김과 면상흐름의 상호작용으로 토사유출량이 3.6~5.9배 증가하였으며 그 증가폭은 강우강도의 증가에 따라 감소하였다. 단위수류력과 토사유출량의 관계분석 결과 강우운동에너지는 빗물튀김에 의한 토양입자의 분리침식을 증가시킬 뿐만 아니라 지표유출수 증가에 따른 토사이송능력을 가중시켜 토사유출량을 크게 증가시키는 것으로 확인되었다.

CAE 증착기술에 의해 TiN이 증착된 보론주철의 마모거동 (Wear Characterisitics of TiN-coated Boron Cast Iron by Arc Evaporation Process)

  • 송건;윤의성;안효석
    • Tribology and Lubricants
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    • 제8권1호
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    • pp.63-69
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    • 1992
  • In order to gain better understanding of wear behaviors of TiN-coated boron cast iron, tests and analyses were conducted with block-on disc type tribometer. TiN layer of thickness $2 \mu m$ and $4 \mu m$, coated by cathodic arc evaporation process, were experimentally investigated with the variation of applied load and sliding speed under dry sliding condition. Wear characteristics were expressed in terms of the three-dimentional wear map as well as the wear rate vs sliding speed and load. Comparisons of wear and friction characteristics between coated cast irons and uncoated cast irns were also made. Wear mechanism of TiN layer was explained in view of surface interaction between the mating surfaces. The thicker coating exhibited higher hardness and adhesion strength. the significance of stresses at the surface and in the subsurface was briefly discussed in relation to the wear behavior.