• Title/Summary/Keyword: 상향 수평등온면

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Numerical Analysis of Natural Convection from a Horizontal Surface Immersed in Cold Water (저온의 물속에 잠겨있는 수평 평면에 의하여 야기되는 자연대류의 수치해석)

  • 유갑종;예용택;권혁용
    • Transactions of the Korean Society of Mechanical Engineers
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    • v.16 no.6
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    • pp.1195-1204
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    • 1992
  • The natural convection from upward and downward facing horizontal isothermal plate immersed in water is studied numerically. The temperature of the plate is from 0.0 .deg. C to 8.0 .deg. C and the ambient water temperature is from 1.0 .deg. C to 10.0 .deg. C. Numerical results are presented for the velocity profiles, temperature profiles, local heat transfer coefficients, and average Nusselt numbers over the entire flow fields. Flow patterns are shown in the upward and downward facing surfaces at different ambient water temperatures. For the upward facing surface, there are upflow and unsteady flow. And the regions of the ambient water temperatures which give rise to the upflow are more extensive as the temperatures of the isothermal surface become more distant from the density extremum temperature. For the downward facing surface, only the downflow region is shown. For the upward facing horizontal isothermal surface, the average Nusselt number(= N $u_{1}$$^{*}$) is 28.86(Ra)$^{0.01}$. And for the downward facing surface, the average Nusselt number(= N $u_{2}$$^{*}$) is $C_{2}$(Ra)$^{0.2}$ and the values of $C_{2}$ are enlarged in the range of 0.785 .leq. $C_{2}$ .leq. 1.250 as increasing of the temperatures of the isothermal surface.ace.ace.

Numerical analysis of natural convection from a horizontal isothermal surface immersed in water near its density extremum (최대밀도점 부근의 물속에 잠겨있는 수평등온도면에 의하여 야기되는 자연대류의 수치해석)

  • 김병하;조승환;유갑종
    • Transactions of the Korean Society of Mechanical Engineers
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    • v.14 no.1
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    • pp.197-206
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    • 1990
  • Numerical results of heat transfer from a horizontal isothermal surface are presented for wall temperature T$_{w}$ = 0 .deg. C and ambient water temperature, T$_{\infty}$, from 1 .deg. C to 15 .deg. C. They include streamlines, temperature profiles, local heat transfer coefficients and average Nusselt numbers for the entire flow fields. For a upward-facing horizontal isothermal surface, the results show steady two dimensional flow regimes for T$_{\infty}$ .leg. 4.4 .deg. C, but no solution was obtained above T$_{\infty}$ = 4.4 .deg. C. For a downward-facing horizontal isothermal surface, the flow regimes are steady two dimensional flow for T$_{\infty}$ .geq. 4.9 .deg. C, and the numerical calculation was failed below this ambient water temperature. The mean Nusselt number has its maximum value at about T$_{\infty}$ = 3.4 .deg. C for upward-facing horizontal isothermal surface. For the case of downward-facing horizontal isothermal surface, the mean Nusselt number increases as the ambient water temperature increases.es.s.s.

Natural Convective Heat Transfer Adjacent to Slightly Inclined Isothermal Surface Immersed in Cold Pure Water (수평으로부터 약간 경사진 등온면이 저온의 순수물 속에 잠겨있을때 일어나는 자연대류 열전달)

  • 유갑종;엄용균
    • Transactions of the Korean Society of Mechanical Engineers
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    • v.15 no.3
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    • pp.1001-1010
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    • 1991
  • 본 연구에서는 천이유동의 존재를 밝히고 천이영역과 경사각의 관계, 유동 및 열전달특성을 구명하고자 한다.이를 위해 유한차분방법(FDM)으로 수치해석하고 실 험결과와 비교, 검토하였다.