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Mission Design for the CubeSat OUFTI-1

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CHAPTER 5- The squares of <strong>the</strong> orbital period of planets are directly proportional to<strong>the</strong> cube of <strong>the</strong> semi-major axes of <strong>the</strong>ir orbit.The same laws can be applied to <strong>the</strong> motion of a satellite around a planet.In orbital mechanics, <strong>the</strong> spacecraft and <strong>the</strong> central body are considered aspoints with mass but without dimensions. As to describe <strong>the</strong> position and <strong>the</strong>speed of a point in a tridimensional space we need six parameters, to completelycharacterize <strong>the</strong> motion of <strong>the</strong> satellite over an orbit we need <strong>the</strong> six so-calledorbital elements: <strong>the</strong> semi-major axis a, <strong>the</strong> eccentricity e, <strong>the</strong> true anomalyϑ or ν, <strong>the</strong> inclination i, <strong>the</strong> longitude or right ascension of ascending nodeΩ or RAAN and <strong>the</strong> argument of perigee ω. As shown in fig.5.8, <strong>the</strong> firsttwo describe <strong>the</strong> orbit shape and <strong>the</strong> last three <strong>the</strong> position of <strong>the</strong> orbit planerespect to <strong>the</strong> earth. The true anomaly, sometimes substituted by <strong>the</strong> time sinceperigee passage, introduces <strong>the</strong> position of <strong>the</strong> satellite on <strong>the</strong> orbit starting from<strong>the</strong> perigee: it’a <strong>the</strong> only parameter that varies along <strong>the</strong> orbit as long as wemaintain <strong>the</strong> hypo<strong>the</strong>sis of ideal motion.Figure 5.8: Orbital ParametersThe motion is in fact considered to be ideal and determined only by <strong>the</strong>gravity <strong>for</strong>ce between <strong>the</strong> masses and <strong>the</strong> fictitious centrifugal <strong>for</strong>ce, withoutany perturbation as <strong>the</strong> aerodynamic drag and <strong>the</strong> presence of o<strong>the</strong>rs bodies.Starting from <strong>the</strong> Newton’s laws and from <strong>the</strong> gravitational laws, we can defines<strong>the</strong> orbital elements and some o<strong>the</strong>r parameters that can be useful <strong>for</strong> <strong>the</strong>continuation.We place ourself on <strong>the</strong> orbit plane and we call r p and r a <strong>the</strong> radius respectivelyof perigee and apogee and µ <strong>the</strong> earth gravitational constant. We define<strong>the</strong>n <strong>the</strong> following parameters that remain constant:Galli Stefania 34 University of Liège

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