PlanetPhysics/Centre of Mass of Half Disc

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Let E be the upper half-disc of the disc\, x2+y2R\, in 2 with a constant surface-density 1. By the symmetry, its [[../CenterOfGravity/|centre of mass]] locates on its medium radius, and therefore we only have to calculate the ordinate Y of the centre of mass. For doing that, one can use in this [[../CoriolisEffect/|two-dimensional]] case instead a triple integral the double integral Y=1ν(E)Eydxdy, where\, ν(E)=πR22\, is the area (and the [[../Mass/|mass]]) of the half-disc. The region of integration is defined by E={(x,y)2RxR,0yR2x2}. Accordingly, we may write Failed to parse (unknown function "\sijoitus"): {\displaystyle Y = \frac{2}{\pi R^2}\!\int_{-R}^R\!dx\int_0^{\sqrt{R^2-x^2}}\!y\,dy = \frac{2}{\pi R^2}\!\int_{-R}^R\frac{R^2\!-\!x^2}{2}\,dx = \frac{2}{\pi R^2}\sijoitus{-R}{\quad R}\left(\frac{R^2x}{2}-\frac{x^3}{6}\right) = \frac{4R}{3\pi}.} Thus the centre of mass is the point\, (0,4R3π).

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