6 research outputs found
Numerical Study on the Observational Error of Sea-Surface Winds at Ieodo Ocean Research Station
μμΉν΄μμ ν΅νμ¬ μ΄μ΄λ μ’
ν©ν΄μκ³ΌνκΈ°μ§ κ΅¬μ‘°λ¬Όμ΄ λκΈ° μ λμ λ―ΈμΉλ μν₯μ λΆμνμκ³ , μ΄ κ²°κ³Όλ₯Ό λ°νμΌλ‘ κ³ΌνκΈ°μ§μ μ€μΉλ νμμΌμμμμ μΈ‘μ κ° μ€μ°¨λ₯Ό νκ°νλ μ°κ΅¬λ₯Ό μννμλ€. κ³ΌνκΈ°μ§ νμμ 3μ°¨μμΌλ‘ λͺ¨λΈλ§νμκ³ μμΉν΄μμ μν 격μλ₯Ό μμ±νμ¬, Navier-Stokes λ°©μ μ λ° λλ₯λͺ¨λΈμ μ μ©νμ¬ μμΉν΄μμ μννμλ€. μ μ λ μμ λ₯μ νμκ³Ό νν₯ 쑰건μ λνμ¬ κ³ΌνκΈ°μ§ κ΅¬μ‘°λ¬Όμ μν΄ λ³νλ μ λμ₯μ κ³μ°νκ³ , μ€μ νμμΌμκ° μ€μΉλ μμΉμμμ νμ/νν₯ μ 보μ μμ λ₯λ₯Ό λΉκ΅νμλ€. μ΄λ₯Ό ν΅νμ¬ μμ λ₯ λ°©ν₯ λ° μΈ‘μ μμΉμ λ°λ₯Έ λ°μ΄ν°μ μ νλμ μ λ’°ν μ μλ λ°μ΄ν° λ²μλ₯Ό μμ보μλ€. λ³Έ μ°κ΅¬ κ²°κ³Όλ‘ κ΄μΈ‘λ ν΄μν λ°μ΄ν°μ ꡬ쑰물 κ°μμ μν μ€μ°¨ λ²μλ₯Ό μ λμ μΌλ‘ νμ
ν μ μμμΌλ©°, κ³ΌνκΈ°μ§κ° μμΉν μ§μ μ μ νν ν΄μν λ°μ΄ν° μ 곡μ μν κΈ°μ΄ μλ£λ‘ νμ©λ κ²μΌλ‘ κΈ°λλλ€. = The influence of Ieodo Ocean Research Station structure to surrounding atmospheric flow is carefully investigated using CFD techniques. Moreover, the validation works of computational results are performed by the comparison with the observed data of Ieodo Ocean Research station. In this paper, we performed 3-dimensional CAD modelling of the station, generated the grid system for numerical analysis and carried out flow analyses using Navier-Stokes equations coupled with two-equation turbulence model. For suitable free stream conditions of wind speed and direction, the interference of the research station structure on the flow field is predicted. Beside, the computational results are benchmarked by observed data to confirm the accuracy of measured date and reliable data range of each measuring position according to the wind direction. Through the results of this research, now the quantitative evaluation of the error range of interfered gauge data is possible, which is expected to be applied to provide base data of accurate sea surface wind around research stations.λ³Έ μ°κ΅¬λ νκ΅ν΄μμ°κ΅¬μμ 'μ΄μ΄λ μ’
ν©ν΄μκ³ΌνκΈ°μ§νμ©μ°κ΅¬' μ¬μ
μ μ§μμΌλ‘ μνλμμ
μμΉν΄μμ μ΄μ©ν μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Όμ΄ ν΄μ μ λμ λ―ΈμΉλ μν₯ λΆμκ³Ό ν΄λ₯ κ΄μΈ‘ νκ° λ° λ³΄μ λ°©μ μ°κ΅¬ = Numerical investigation, calibration method of the interaction between Ieodo ocean research station and ocean current
μ΄μ΄λμ 건μ€λ λ€λͺ©μ ν΄μκ³ΌνκΈ°μ§μμλ μ£Όμ λλ₯ λ° ν΄λ₯μ λ°μ΄ν° μμ§μ ν΅ν΄ κΈ°μ, μ΄μ₯μ보 λ±μ κΈ°μ΄ μλ£λ₯Ό μ 곡νλ κ²μ ν κ°μ§ λͺ©μ μΌλ‘ νλ€. κ·Έλ°λ° μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Όμ μν ν΄μ μ λμ λ³νλ κ³ΌνκΈ°μ§μ κ΄μΈ‘ λ°μ΄ν°μ μν₯μ μ£Όμ΄ μ νν μλ£ μμ§μ μ΄λ ΅κ² νλ―λ‘, μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Όμ΄ μ£Όμ μ λμ λ―ΈμΉλ μν₯μ λΆμνκ³ μ λ μ 보 κ΄μΈ‘μ νκ°/보μ νλ λ°©λ²μ λν μ°κ΅¬κ° νμνλ€. λ³Έ μ°κ΅¬μμλ μ΄λ₯Ό μν κΈ°μ΄μ°κ΅¬λ‘, ν΄λ₯μ ꡬ쑰물 μ¬μ΄μ μνΈ μμ©μ λͺ¨μ¬ν μ μλ μκ³ λ¦¬μ¦μ μ°κ΅¬, μ μ©λ°©λ²μ λ
Όμνλ€. κ·Έ κ²°κ³Ό, 3μ°¨μ μ μ°μ 체μνμ μ΄μ©ν μμΉν΄μμ ν΅ν΄ μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Ό λ° μμ€μμ΄κ° μ£Όμ μ λμ λ―ΈμΉλ μν₯μ μ°κ΅¬νκ³ μ νν λ°μ΄ν° μΈ‘μ λ°©λ²μ μ μνλ€. = One of the main function of Ieodo Ocean Research Station is to service the information about the weather and fishing grounds condition which are collected through calibrating convection flow and ocean current around the station. However, due to the influence of the station"s structure below sea level, it is difficult to obtain the exact flow data. Therefore, it is required to research on the effect of the structure and the method to evaluate and revise the observed data. In this paper, as a basic study, it deals with the algorithm that simulate the interaction between ocean current and the station structure, followed by discussions about the way to applicate the algorithm. Through 3-dimensional computational fluid dynamics analyses (using Navier-Stokes equations with K-turbulence model), the influence of the station and submerged rocks are quantitatively evaluated, and we would suggest methods how to obtain accurate flow information from the measured rough data
μμΉν΄μμ μ΄μ©ν μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Όμ΄ ν΄μ μ λμ λ―ΈμΉλ μν₯ λΆμκ³Ό ν΄λ₯ κ΄μΈ‘ νκ° λ° λ³΄μ λ°©μ μ°κ΅¬ = Numerical Investigation, Calibration Method of the Interaction between Ieodo Ocean Research Station and Ocean Current
μ΄μ΄λμ 건μ€λ λ€λͺ©μ ν΄μκ³ΌνκΈ°μ§μμλ μ£Όμ λλ₯ λ° ν΄λ₯μ λ°μ΄ν° μμ§μ ν΅ν΄ κΈ°μ, μ΄μ₯μ보 λ±μ κΈ°μ΄ μλ£λ₯Ό μ 곡νλ κ²μ ν κ°μ§ λͺ©μ μΌλ‘ νλ€. κ·Έλ°λ° μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Όμ μν ν΄μ μ λμ λ³νλ κ³ΌνκΈ°μ§μ κ΄μΈ‘ λ°μ΄ν°μ μν₯μ μ£Όμ΄ μ νν μλ£ μμ§μ μ΄λ ΅κ² νλ―λ‘, μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Όμ΄ μ£Όμ μ λμ λ―ΈμΉλ μν₯μ λΆμνκ³ μ λ μ 보 κ΄μΈ‘μ νκ°/보μ νλ λ°©λ²μ λν μ°κ΅¬κ° νμνλ€. λ³Έ μ°κ΅¬μμλ μ΄λ₯Ό μν κΈ°μ΄μ°κ΅¬λ‘, ν΄λ₯μ ꡬ쑰물 μ¬μ΄μ μνΈ μμ©μ λͺ¨μ¬ν μ μλ μκ³ λ¦¬μ¦μ μ°κ΅¬, μ μ©λ°©λ²μ λ
Όμνλ€. κ·Έ κ²°κ³Ό, 3μ°¨μ μ μ°μ 체μνμ μ΄μ©ν μμΉν΄μμ ν΅ν΄ μ΄μ΄λ κΈ°μ§ κ΅¬μ‘°λ¬Ό λ° μμ€μμ΄κ° μ£Όμ μ λμ λ―ΈμΉλ μν₯μ μ°κ΅¬νκ³ μ νν λ°μ΄ν° μΈ‘μ λ°©λ²μ μ μνλ€. = One of the main function of Ieodo Ocean Research Station is to service the information about the weather and fishing grounds condition which are collected through calibrating convection flow and ocean current around the station. However, due to the influence of the station"s structure below sea level, it is difficult to obtain the exact flow data. Therefore, it is required to research on the effect of the structure and the method to evaluate and revise the observed data. In this paper, as a basic study, it deals with the algorithm that simulate the interaction between ocean current and the station structure, followed by discussions about the way to applicate the algorithm. Through 3-dimensional computational fluid dynamics analyses (using Navier-Stokes equations with K-turbulence model), the influence of the station and submerged rocks are quantitatively evaluated, and we would suggest methods how to obtain accurate flow information from the measured rough data.λ³Έ μ°κ΅¬λ νκ΅ν΄μμ°κ΅¬μμ μ΄μ΄λ μ’
ν©ν΄μκ³ΌνκΈ°μ§κ΅¬μΆ λ° νμ©μ°κ΅¬(KORDI PM43000)μ¬μ
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Pseudo-compressibility λ°©λ²μμ μ΄μμ λ ν΄μμ μν Level Set λ°©λ²μ μ μ© = Level Set Method Applied On Pseudo-compressibility Method for the Analysis of Two-phase Flow
Level Set λ°©λ²μ μ¬μ©νμ¬ μ‘체μ 기체μ μλ‘ λ€λ₯Έ μμ ν¨κ» ν΄μνλ μ°κ΅¬λ₯Ό μννμλ€. Level Set ν¨μλ μμ κ²½κ³λ©΄μμλΆν° λΆνΈλ₯Ό κ°λ 거리ν¨μλ‘ μ μλλ©°, κ³μ° 격μμμ ν¨μ κ°μ λΆνΈμ λ°λΌ κ° μμ ꡬλΆνκ³ λ¬Όμ±μΉλ₯Ό λΆμ¬νλ€. λ³Έ λ
Όλ¬Έμμλ λΉμμΆμ± μ 체μ 보쑴μμ Level Set ν¨μμ μ΄λμμ μ°κ³νμ¬ μ΄μμ λμ λͺ¨μ¬νλ μ§λ°°λ°©μ μμ ꡬμ±νμμΌλ©°, μ΄λ₯Ό pseudo-compressibility λ°©λ²μΌλ‘ ν¨κ» νμλ€. μ΄ λ λ€μν λ¬Έμ μ μ μ©μ΄ κ°λ₯νλλ‘ μΌλ° 곑μ μ’νκ³μμ μμ μ λνμκ³ , μμΉν΄μμ μν νλ ¬μλ€μ ν¨κ» μ λνμλ€. κ°λ°λ ν΄μ μ½λλ₯Ό νλ©΄μ₯λ ₯μ΄ μλ κΈ°ν¬ λμν λ¬Έμ μ μμ€μ΅μ μν νλ λ°μ λ¬Έμ μ μ μ©νμ¬ νλΉν κ²°κ³Όλ₯Ό μ»μ μ μμλ€. = In order to analyze incompressible two-phase flow, Level Set method was applied on pseudo-compressibility formulation. Level Set function is defined as a signed distance function from the phase interface, and gives the information of the each phase location and the geometric data to the flow. In this study, Level Set function transport equation was coupled with flow conservation equations, and owing to pseudo-compressibility technique we could solve the resultant vector equation iteratively. Two-phase flow analysis code was developed on general curvilinear coordinate, and numerical tests of bubble dynamics and surging wave problems demonstrate its capability successfully.λ³Έ μ°κ΅¬λ νκ΅ν΄μμ°κ΅¬μμ 'μ΄μ΄λ μ’
ν©ν΄μκ³ΌνκΈ°μ§νμ©μ°κ΅¬(KORDI PE29200)' μ¬μ
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Level Set Method Applied on Pseudo-compressibility Method for the Analysis of Two-phase Flow
In order to analyze incompressible two-phase flow, Level Set method was applied on pseudo-compressibility formulation. Level Set function is defined as a signed distance function from the phase interface,and gives the information of the each phase location and the geometric data to the flow. In this study, Level Settechnique we could solve the resultant vector equation iteratively. Two-phase flow analysis code was developedon general curvilinear coordinate, and numerical tests of bubble dynamics and surging wave problems demon-strate its capability successfully.N
Study on Wind Tunnel Test and 3 Dimensional Numerical Analysis of EARDO Ocean Research Station
OAIID:oai:osos.snu.ac.kr:snu2002-01/102/0000004648/43SEQ:43PERF_CD:SNU2002-01EVAL_ITEM_CD:102USER_ID:0000004648ADJUST_YN:NEMP_ID:A001138DEPT_CD:446CITE_RATE:0FILENAME:μ΄μ΄λ_μ’
ν©ν΄μκ³ΌνκΈ°μ§_νλμ€ν_λ°_3μ°¨μ_μμΉν΄μμ_κ΄ν_μ°κ΅¬.pdfDEPT_NM:κΈ°κ³ν곡곡νλΆEMAIL:[email protected]_YN:NCONFIRM: