How to Find Shaded Areas in Polar Coordinates

Finding shaded areas in polar coordinates can seem tricky at first, but it’s quite manageable once you understand the process. Polar coordinates use angles and radii to define points, making them particularly useful for dealing with circular and spiral shapes.

Understanding Polar Coordinates

In polar coordinates, a point is represented by $(r, theta)$, where $r$ is the radius (distance from the origin) and $theta$ is the angle measured from the positive x-axis. For example, the point $(3, frac{pi}{4})$ means a radius of 3 units and an angle of $frac{pi}{4}$ radians.

Formula for Area in Polar Coordinates

To find the area of a region in polar coordinates, we use integration. The general formula for the area of a region bounded by a curve $r = f(theta)$ from $theta = alpha$ to $theta = beta$ is:

$A = frac{1}{2} int_{alpha}^{beta} r^2 , dtheta$

This formula comes from dividing the region into infinitesimally small sectors, each resembling a triangle with area $frac{1}{2} r^2 , dtheta$

Finding the Shaded Area Between Two Curves

Often, you need to find the area between two curves, $r_{outer} = f(theta)$ and $r_{inner} = g(theta)$. In this case, the area is given by:

$A = frac{1}{2} int_{alpha}^{beta} left( r_{outer}^2 – r_{inner}^2 right) , dtheta$

Example Problem

Let’s find the shaded area between two polar curves: $r_{outer} = 2 + cos theta$ and $r_{inner} = 1$ from $theta = 0$ to $theta = pi$

  1. Set up the integral:

$A = frac{1}{2} int_{0}^{pi} left( (2 + cos theta)^2 – 1^2 right) , dtheta$

  1. Simplify the integrand:

$(2 + cos theta)^2 = 4 + 4cos theta + cos^2 theta$

So the integral becomes:

$A = frac{1}{2} int_{0}^{pi} left( 4 + 4cos theta + cos^2 theta – 1 right) , dtheta$

$A = frac{1}{2} int_{0}^{pi} left( 3 + 4cos theta + cos^2 theta right) , dtheta$

  1. Integrate:

To integrate $cos^2 theta$, use the identity $cos^2 theta = frac{1 + cos 2theta}{2}$

$A = frac{1}{2} int_{0}^{pi} left( 3 + 4cos theta + frac{1 + cos 2theta}{2} right) , dtheta$

$A = frac{1}{2} left[ 3theta + 4sin theta + frac{theta}{2} + frac{sin 2theta}{4} right]_{0}^{pi}$

  1. Evaluate:

$A = frac{1}{2} left[ 3pi + 4sin pi + frac{pi}{2} + frac{sin 2pi}{4} – (3cdot0 + 4sin0 + frac{0}{2} + frac{sin 0}{4}) right]$

Since $sin pi = 0$ and $sin 0 = 0$:

$A = frac{1}{2} left( 3pi + frac{pi}{2} right) = frac{1}{2} cdot frac{7pi}{2} = frac{7pi}{4}$

Conclusion

By understanding the formula and practicing a few examples, you can confidently find shaded areas in polar coordinates. Remember, the key is to set up your integral correctly and simplify step-by-step.

Citations

  1. 1. Khan Academy – Polar Coordinates
  2. 2. Paul’s Online Math Notes – Polar Coordinates
  3. 3. MIT OpenCourseWare – Polar Coordinates

Related

(2) O3 + H → O2 + OH k2 = 1.78×10^-11 cm^3 s^-1 (3) O + OH → O2 + H k3 = 4.40×10^-11 cm^3 s^-1 (5) O + HO2 → O2 + OH k5 = 3.50×10^-11 cm^3 s^-1 (6) H + HO2 → O2 + H2 k6 = 5.40×10^-12 cm^3 s^-1 (9) OH + HO2 → O2 + H2O2 k9 = 4.00×10^-11 cm^3 s^-1 (10) HO2 + HO2 → O2 + H2O2 k10 = 2.50×10^-12 cm s^-1 (11) O + O2 + M → O3 + M k11 = 1.05×10^-34 cm^6 s^-1 (14) H + O2 + M → HO2 + M k14 = 8.08×10^-32 cm^6 s^-1 (15) H + H + M → H2O + M k15 = 3.31×10^-27 cm^6 s^-1 (16) O2 + hv → 2 O k16 = (1.26×10^-8 s^-1) φ (17) H2O + hv → H + OH k17 = (3.4×10^-6 s^-1) φ (18) O3 + hv → O2 + O k18 = (7.10×10^-5 s^-1) φ

Table 1 Reactions, rate constants and activation energies used in the model* No. Reaction kopt (M⁻¹ s⁻¹) 1 OH + H₂ → H + H₂O 3.74 x 10⁷ 2 OH + HO₂ → HO₂ + OH⁻ 5 x 10⁹ 3 OH + H₂O₂ → HO₂ + H₂O 3.8 x 10⁷ 4 OH + O₂ → O₂ + OH 9.96 x 10⁹ 5 OH + HO₂ → O₂ + H₂O 7.1 x 10⁹ 6 OH + OH → H₂O₂ 5.3 x 10⁹ 7 OH + e⁻aq → OH⁻ 3 x 10¹⁰ 8 H + O₂ → HO₂ 2.0 x 10¹⁰ 9 H + HO₂ → H₂O₂ 2.0 x 10¹⁰ 10 H + H₂O₂ → OH + H₂O 3.44 x 10⁷ 11 H + OH → H₂O 1.4 x 10¹⁰ 12 H + H → H₂ 1.94 x 10¹⁰ 13 e⁻aq + O₂ → O₂⁻ 1.9 x 10¹⁰ 14 e⁻aq + O₂ → HO₂⁻ + OH⁻ 1.3 x 10¹⁰ 15 e⁻aq + HO₂ 2.0 x 10¹⁰ 16 e⁻aq + H₂O₂ 1.1 x 10¹⁰ 17 e⁻aq + HO₂ → OH + OH⁻ 1.3 x 10¹⁰ 18 e⁻aq + H⁺ → H 2.3 x 10¹⁰ 19 e⁻aq + e⁻aq → H₂ + OH⁻ + OH⁻ 2.5 x 10⁹ 20 HO₂ + O₂ → O₂ + HO₂ 1.3 x 10⁹ 21 HO₂ + HO₂ → O₂ + H₂O₂ 8.3 x 10⁵ 22 HO₂ + HO₂ → O₂ + OH + H₂O 3.7 23 HO₂ + HO₂ → O₂ + O₂ + OH + H₂O 7 x 10⁵ s⁻¹ 24 H⁺ + O₂⁻ → HO₂ 4.5 x 10¹⁰ 25 H⁺ + O₂⁻ → O₂ 2.0 x 10¹⁰ 26 H⁺ + OH⁻ 1.4 x 10¹¹ 27 H⁺ + HO₂⁻ 2 x 10¹⁰ 28 H₂O₂ → HO₂ + H⁺ + OH⁻ 2.5 x 10⁻⁵ s⁻¹ 29 H₂O₂ → H⁺ + OH⁻ 1.4 x 10⁻⁷ s⁻¹ 30 O₂ + O₂ → O₂ + HO₂ + OH⁻ 0.3 31 O₂ + H₂O₂ → O₂ + OH + OH 16 32

(2) O3 + H → O2 + OH k2 = 1.78×10^-11 cm^3 s^-1 (3) O + OH → O2 + H k3 = 4.40×10^-11 cm^3 s^-1 (5) O + HO2 → O2 + OH k5 = 3.50×10^-11 cm^3 s^-1 (6) H2O + O → 2 OH k6 = 5.40×10^-12 cm^3 s^-1 (9) OH + HO2 → O2 + H2O k9 = 4.00×10^-11 cm^3 s^-1 (10) HO2 + HO2 → O2 + H2O2 k10 = 2.50×10^-12 cm s^-1 (11) O + O2 + M → O3 + M k11 = 1.05×10^-34 cm^6 s^-1 (14) H + O2 + M → HO2 + M k14 = 8.08×10^-32 cm^6 s^-1 (15) OH + H + M → H2O + M k15 = 3.31×10^-27 cm^6 s^-1 (16) O2 + hv → 2 O k16 = (1.26×10^-8 s^-1) φ (17) H2O + hv → H + OH k17 = (3.4×10^-6 s^-1) φ (18) O3 + hv → O2 + O k18 = (7.10×10^-8 s^-1) φ