grahas
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How is this done? My textbook only specifies integrating polar graphs with respect to theta.
This discussion focuses on integrating polar graphs with respect to the radius (r) rather than the angle (θ). The participants suggest using annuli instead of trapezoids for area estimation, emphasizing that the area can be expressed as A(r) = 8∫₀ʳ 2πρθ(ρ) dρ. The conversation also touches on converting polar equations into parametric forms, with suggestions to derive θ(r) using arccos functions. The integration approach aims to graph the area A versus r, relevant for understanding spatial distributions in polar coordinates.
PREREQUISITESMathematicians, physics students, and data scientists interested in spatial analysis and integration techniques in polar coordinates.
No need for trapezoids. For infinitesimal dh rectangles are enoughgrahas said:Well to integrate with respect to r my best guess was to use trapezoids to estimate the area.
right. From symmetry, finding one point suffices.The points on the trapezoid are calculated from intersection points with a circle of radius r
Not correct. Can you see why not ?and the thickness of the trapezoid is dr
Yes. My charcoal englishHendrik Boom said:Integrating with respect to r, wouldn't you be dealing with rings or arcs instead of straight lines?
Hehe, PF culture insists that you do the work and we help by asking, hinting etceteragrahas said:How could this be generalized to a formula that could be graphed?
Isn't ##\left (\cos 2\theta\right )^2 - r = 0## good enough ? if you want to integrate over ##dr## all you need to do is work this around to a function ##\theta(r)##, something with an ##\arccos##, I suppose...grahas said:how to convert the polar graph to a parametric one