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Mathematics LibreTexts

10.2: Slopes in Polar Coordinates

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When we describe a curve using polar coordinates, it is still a curve in thexy plane. We would like to be able to compute slopes and areas for these curves using polar coordinates.

We have seen that x=rcosθ and y=rsinθ describe the relationship between polar and rectangular coordinates. If in turn we are interested in a curve given by r=f(θ), then we can write x=f(θ)cosθ and y=f(θ)sinθ, describing x and y in terms of θ alone. The first of these equations describes θ implicitly in terms of x, so using the chain rule we may compute

dydx=dydθdθdx.

Since dθ/dx=1/(dx/dθ), we can instead compute

dydx=dy/dθdx/dθ=f(θ)cosθ+f(θ)sinθf(θ)sinθ+f(θ)cosθ.

Example 10.2.1:

Find the points at which the curve given by r=1+cosθ has a vertical or horizontal tangent line. Since this function has period 2π, we may restrict our attention to the interval [0,2π) or (π,π], as convenience dictates. First, we compute the slope:

dydx=(1+cosθ)cosθsinθsinθ(1+cosθ)sinθsinθcosθ=cosθ+cos2θsin2θsinθ2sinθcosθ.

This fraction is zero when the numerator is zero (and the denominator is not zero). The numerator is 2cos2θ+cosθ1 so by the quadratic formula cosθ=1±1+424=1or12. This means θ is π or ±π/3. However, when θ=π, the denominator is also 0, so we cannot conclude that the tangent line is horizontal.

Setting the denominator to zero we get θ2sinθcosθ=0sinθ(1+2cosθ)=0, so either sinθ=0 or cosθ=1/2. The first is true when θ is 0 or π, the second when θ)is\(2π/3 or 4π/3. However, as above, when θ=π, the numerator is also 0, so we cannot conclude that the tangent line is vertical. Figure 10.2.1 shows points corresponding to θ equal to 0, ±π/3, 2π/3 and 4π/3 on the graph of the function. Note that when θ=π the curve hits the origin and does not have a tangent line.

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Figure 10.2.1. Points of vertical and horizontal tangency for r=1+cosθ.

We know that the second derivative f(x) is useful in describing functions, namely, in describing concavity. We can compute f(x) in terms of polar coordinates as well. We already know how to write dy/dx=y in terms of θ, then

ddxdydx=dydx=dydθdθdx=dy/dθdx/dθ.

The ellipsis here represents rather a substantial amount of algebra. We know from above that the cardioid has horizontal tangents at ±π/3; substituting these values into the second derivative we get y(π/3)=3/2 and y(π/3)=3/2, indicating concave down and concave up respectively. This agrees with the graph of the function.

Contributors

David Guichard (Whitman College)

  • Integrated by Justin Marshall.


This page titled 10.2: Slopes in Polar Coordinates is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by David Guichard via source content that was edited to the style and standards of the LibreTexts platform.

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