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Polar coordinate system
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====Generalization==== Using [[Cartesian coordinates]], an infinitesimal area element can be calculated as ''dA'' = ''dx'' ''dy''. The [[integration by substitution#Substitution for multiple variables|substitution rule for multiple integrals]] states that, when using other coordinates, the [[Jacobian matrix and determinant|Jacobian]] determinant of the coordinate conversion formula has to be considered: <math display="block">J = \det \frac{\partial(x, y)}{\partial(r, \varphi)} = \begin{vmatrix} \frac{\partial x}{\partial r} & \frac{\partial x}{\partial \varphi} \\[2pt] \frac{\partial y}{\partial r} & \frac{\partial y}{\partial \varphi} \end{vmatrix} = \begin{vmatrix} \cos\varphi & -r\sin\varphi \\ \sin\varphi & r\cos\varphi \end{vmatrix} = r\cos^2\varphi + r\sin^2\varphi = r. </math> Hence, an area element in polar coordinates can be written as <math display="block">dA = dx\,dy\ = J\,dr\,d\varphi = r\,dr\,d\varphi.</math> Now, a function, that is given in polar coordinates, can be integrated as follows: <math display="block">\iint_R f(x, y)\, dA = \int_a^b \int_0^{r(\varphi)} f(r, \varphi)\,r\,dr\,d\varphi.</math> Here, ''R'' is the same region as above, namely, the region enclosed by a curve ''r''(''Ο'') and the rays ''Ο'' = ''a'' and ''Ο'' = ''b''. The formula for the area of ''R'' is retrieved by taking ''f'' identically equal to 1. [[Image:E^(-x^2).svg|thumb|right|A graph of <math>f(x) = e^{-x^2}</math> and the area between the function and the <math>x</math>-axis, which is equal to <math>\sqrt{\pi}</math>.]] A more surprising application of this result yields the [[Gaussian integral]]: <math display="block">\int_{-\infty}^\infty e^{-x^2} \, dx = \sqrt\pi.</math>
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