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月球坑內(nèi)空間環(huán)境熱流的分布研究

Analysis on Heat Flux Distribution in Lunar Craters

  • 摘要: 文章推導獲得了月面陽光矢量和月球坑內(nèi)探測器表面關系的表達式,采用蒙特卡羅法數(shù)值計算探測器各表面的輻射熱流,分析了月球坑內(nèi)環(huán)境輻射熱流的分布特征。討論了月面緯度、月球坑尺寸、月面發(fā)射率等參數(shù)對探測器表面熱流的影響。計算表明:月面緯度增加及月球坑坑口半徑的減小均會導致某些時刻陽光無法照射到坑底,從而與其他工況有較大的計算差別,兩參數(shù)對探測器各面熱流的影響規(guī)律不同;月面發(fā)射率對探測器表面熱流的影響作用較大,增加月面發(fā)射率能明顯降低探測器某些表面的輻射熱流。

     

    Abstract: The relationship between the direction vectors of the sun light at the lunar surface and those at the detector surfaces in a lunar crater are derived through a coordinate transformation. Radiative heat fluxes at the detector surfaces are numerically computed using the Monte Carlo method, and the ambient radiative heat flux distribution in lunar craters is analyzed. Spacial and temporal distribution characteristics of radiative heat fluxes at the detector surfaces and the influences of some parameters on the flux distribution are discussed, including the lunar latitude, the crater diameter, the lunar surface emittance. Computational results show that both the increase in the lunar latitude and the decrease in the crater diameter will make the sun light unattainable in the crater bottom during a certain time periods, resulting a significant difference in the operating conditions. But these two parameters influence the detector surface fluxes in different ways. In addition, the detector surface fluxes are influenced significantly by the lunar surface emittance. With the increase in the lunar surface emittance, the radiative heat fluxes on certain detector surfaces decrease obviously.

     

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