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Mission Design for the CubeSat OUFTI-1

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CHAPTER 9.THERMAL-CONTROL SYSTEMFigure 9.1: Nodes model <strong>for</strong> <strong>the</strong>rmal analysis• <strong>the</strong> green resistances represent <strong>the</strong> infrared radiation between <strong>the</strong> facewatching <strong>the</strong> earth and <strong>the</strong> earth.The sun light and <strong>the</strong> albedo are flux on <strong>the</strong> corresponding faces (node 2and 8 <strong>for</strong> <strong>the</strong> sun flux, nodes 5 and 11 <strong>for</strong> <strong>the</strong> albedo):Q sun = CsαSQ albedo = 0.3CsαS = 0.3Q sun(9.5)The factor 0.3 keeps into account <strong>the</strong> average reflectivity of <strong>the</strong> earth whereseas and continents have different values: in fact <strong>the</strong> albedo is <strong>the</strong> solar visibleflux reflected by <strong>the</strong> planet.9.3.2 Equivalent resistancesThe heat transfer between two parts of a body with different temperatures T 2and T 1 situated at distance L is ruled by <strong>the</strong> Fourier’s law:{ρc p∂T∂t⃗q = −k ⃗ ∇T= ⃗ ∇⃗q + σ(9.6)Galli Stefania 89 University of Liège

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