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Polar Calculus - Interactive Lesson | Study Mondo
Polar Calculus - Complete Interactive Lesson Part 1: Core Concepts Polar Calculus
Part 1 of 7 — Polar Coordinates & Conversions
In polar coordinates, each point is described by ( r , θ ) (r, \theta) ( r , θ ) : a distance r r r from the origin and an angle θ \theta θ from the positive x x x -axis.
Conversion Formulas
x = r cos θ , y = r sin θ \boxed{x = r\cos\theta, \quad y = r\sin\theta} x = r cos θ , y = r sin θ
r = x 2 + y 2 , tan θ = y x \boxed{r = \sqrt{x^2+y^2}, \quad \tan\theta = \frac{y}{x}} r = x 2 + y 2
Cartesian Polar ( 1 , 1 ) (1, 1) ( 1 , 1 ) ( 2 , π / 4 ) (\sqrt{2},\, \pi/4) ( 2
Key Fact: A point ( r , θ ) (r, \theta) ( r , θ ) can also be written as ( − r , θ + π ) (-r, \theta + \pi) ( − r , θ + π ) or ( r , θ + 2 π ) (r, \theta + 2\pi) ( r , . Polar representations are NOT unique!
Common Polar Equations
Equation Shape r = a r = a r = a Circle of radius $ θ = c \theta = c θ = c Line through origin at angle c c c r = 2 a
Key Takeaways
Polar coordinates ( r , θ ) (r, \theta) ( r , θ ) locate points by distance and angle
Convert with x = r cos θ x = r\cos\theta x = r cos θ , y = r sin θ y = r\sin\theta y = r and
Part 2: Worked Examples Polar Calculus
Part 2 of 7 — Graphing Polar Curves & Symmetry
Graphing Strategy
To sketch r = f ( θ ) r = f(\theta) r = f ( θ ) :
Make a table of θ \theta θ vs. r r r values
Plot points in polar coordinates
Check for symmetry to reduce work
Note where r = 0 r = 0 (curve passes through origin)
Part 3: Problem-Solving Patterns Polar Calculus
Part 3 of 7 — Area in Polar Coordinates
The Polar Area Formula
The area enclosed by r = f ( θ ) r = f(\theta) r = f ( θ ) from θ = α \theta = \alpha θ = α to θ = β \theta = \beta θ = :
Part 4: Graphs and Interpretation Polar Calculus
Part 4 of 7 — Slopes of Polar Curves
To find d y / d x dy/dx d y / d x for a polar curve r = f ( θ ) r = f(\theta) r = f ( θ ) , treat it as parametric with parameter θ \theta θ :
x = r cos θ
Part 5: Applications Polar Calculus
Part 5 of 7 — Arc Length in Polar Coordinates
The Polar Arc Length Formula
For r = f ( θ ) r = f(\theta) r = f ( θ ) from θ = α \theta = \alpha θ = α to θ = β \theta = \beta θ = :
Part 6: Exam Strategy Polar Calculus
Part 6 of 7 — Problem-Solving Workshop
Mixed practice covering polar coordinates, graphing, area, slopes, and arc length.
AP FRQ-Style Problem
Consider r = 2 cos θ r = 2\cos\theta r = 2 cos θ for 0 ≤ θ ≤ π / 2 0 \le \theta \le \pi/2 0 ≤ θ ≤ π /2 .
Find the area of the region.
Part 7: Mixed Review Polar Calculus
Part 7 of 7 — Comprehensive Review
Complete Polar Formula Sheet
Formula Expression Conversion x = r cos θ x = r\cos\theta x = r cos θ , y = r sin θ y = r\sin\theta y = r sin θ Area
,
tan
θ
=
x y
,
π
/4
)
( 0 , 3 ) (0, 3) ( 0 , 3 ) ( 3 , π / 2 ) (3,\, \pi/2) ( 3 , π /2 )
( − 1 , 3 ) (-1, \sqrt{3}) ( − 1 , 3 ) ( 2 , 2 π / 3 ) (2,\, 2\pi/3) ( 2 , 2 π /3 )
( 3 , 0 ) (3, 0) ( 3 , 0 ) ( 3 , 0 ) (3,\, 0) ( 3 , 0 )
θ
+
2 π )
cos θ r = 2a\cos\theta r = 2 a cos θ
r = 2 a sin θ r = 2a\sin\theta r = 2 a sin θ Circle of radius $
r = a + b cos θ r = a + b\cos\theta r = a + b cos θ Lima\c{c}on (with loop if $
r = a cos ( n θ ) r = a\cos(n\theta) r = a cos ( n θ ) Rose (n n n petals if odd, 2 n 2n 2 n if even)
r = 2 cos θ r = 2\cos\theta r = 2 cos θ : multiply both sides by r r r : r 2 = 2 r cos θ ⟹ x 2 + y 2 = 2 x r^2 = 2r\cos\theta \implies x^2+y^2 = 2x r 2 = 2 r cos θ ⟹ x 2 + y 2 = 2 x
sin
θ
r 2 = x 2 + y 2 r^2 = x^2+y^2 r 2 = x 2 + y 2 Representations are not unique: ( r , θ ) = ( − r , θ + π ) = ( r , θ + 2 π ) (r, \theta) = (-r, \theta+\pi) = (r, \theta+2\pi) ( r , θ ) = ( − r , θ + π ) = ( r , θ + 2 π )
Know the standard curves: circles, cardioids, roses, lima\c{c}ons
Next: Part 2 covers graphing polar curves and symmetry analysis.
r
=
0
Note where r < 0 r < 0 r < 0 (point is reflected through origin)
Symmetry Tests Symmetry Test Replace About x x x -axis f ( − θ ) = f ( θ ) f(-\theta) = f(\theta) f ( − θ ) = f ( θ ) θ → − θ \theta \to -\theta θ → − θ About y y y -axis f ( π − θ ) = f ( θ ) f(\pi - \theta) = f(\theta) f ( π − θ ) = f ( θ ) θ → π − θ \theta \to \pi - \theta θ → About origin f ( θ + π ) = f ( θ ) f(\theta + \pi) = f(\theta) f ( θ + π ) = f ( θ ) θ → θ + π \theta \to \theta + \pi θ → θ + π
Important: These are sufficient but not necessary conditions. A curve may have symmetry that the test does not detect.
Graphing Examples
Cardioid r = 1 + cos θ r = 1 + \cos\theta r = 1 + cos θ :
θ \theta θ 0 0 0 π / 3 \pi/3 π /3 π / 2 \pi/2 π /2 2 π / 3 2\pi/3 2 π /3 π \pi π r r r 2 2 2 3 / 2 3/2 3/2 1 1 1 1 / 2 1/2 1/2 0 0
Symmetric about the x x x -axis (since cos ( − θ ) = cos θ \cos(-\theta) = \cos\theta cos ( − θ ) = cos θ ).
Rose r = sin ( 3 θ ) r = \sin(3\theta) r = sin ( 3 θ ) :
r = 0 r = 0 r = 0 when 3 θ = n π 3\theta = n\pi 3 θ = nπ , i.e., θ = 0 , π / 3 , 2 π / 3 , π \theta = 0, \pi/3, 2\pi/3, \pi θ = 0 , π /3 ,
Lemniscate r 2 = 4 cos ( 2 θ ) r^2 = 4\cos(2\theta) r 2 = 4 cos ( 2 θ ) :
Only exists when cos ( 2 θ ) ≥ 0 \cos(2\theta) \ge 0 cos ( 2 θ ) ≥ 0 : − π / 4 ≤ θ ≤ π / 4 -\pi/4 \le \theta \le \pi/4 − π /4 ≤ θ ≤ π /4 and 3 π / 4 ≤ θ ≤ 5 π / 4 3\pi/4 \le \theta \le 5\pi/4
Key Takeaways
Graph polar curves by making a θ \theta θ -r r r table and plotting
Use symmetry tests to reduce graphing work
Know the shapes: circles, cardioids, lima\c{c}ons, roses, lemniscates, spirals
Negative r r r values reflect the point through the origin
Next: Part 3 covers polar area with the integral formula.
β
A = 1 2 ∫ α β r 2 d θ = 1 2 ∫ α β [ f ( θ ) ] 2 d θ \boxed{A = \frac{1}{2}\int_{\alpha}^{\beta} r^2\,d\theta = \frac{1}{2}\int_{\alpha}^{\beta} [f(\theta)]^2\,d\theta} A = 2 1 ∫ α β r 2 d θ = 2 1 ∫ α β [ f ( θ ) ] 2 d θ
Why 1 2 r 2 \frac{1}{2}r^2 2 1 r 2 ? Each thin sector has area 1 2 r 2 d θ \frac{1}{2}r^2\,d\theta 2 1 r 2 d θ (like a triangle with base r d θ r\,d\theta r d θ and height r r r ).
Critical: Choose α \alpha α and β \beta β carefully. The curve must trace the region exactly once. Symmetry can reduce the integral.
Example 1: Area of a Cardioid
Find the area enclosed by r = 1 + cos θ r = 1 + \cos\theta r = 1 + cos θ .
Full curve: 0 ≤ θ ≤ 2 π 0 \le \theta \le 2\pi 0 ≤ θ ≤ 2 π . By symmetry about the x x x -axis: A = 2 ⋅ 1 2 ∫ 0 π ( 1 + cos θ ) 2 d θ A = 2 \cdot \frac{1}{2}\int_0^{\pi}(1+\cos\theta)^2\,d\theta A = 2 ⋅ 2 1 ∫ 0 .
= ∫ 0 π ( 1 + 2 cos θ + cos 2 θ ) d θ = ∫ 0 π ( 3 2 + 2 cos θ + cos 2 θ 2 ) d θ = \int_0^{\pi}(1 + 2\cos\theta + \cos^2\theta)\,d\theta = \int_0^{\pi}\left(\frac{3}{2} + 2\cos\theta + \frac{\cos 2\theta}{2}\right)d\theta = ∫ 0 π ( 1 + 2
= [ 3 θ 2 + 2 sin θ + sin 2 θ 4 ] 0 π = 3 π 2 = \left[\frac{3\theta}{2} + 2\sin\theta + \frac{\sin 2\theta}{4}\right]_0^{\pi} = \frac{3\pi}{2} = [ 2 3 θ + 2 sin θ +
Example 2: Area of One Petal
One petal of r = sin ( 2 θ ) r = \sin(2\theta) r = sin ( 2 θ ) : the first petal spans 0 ≤ θ ≤ π / 2 0 \le \theta \le \pi/2 0 ≤ θ ≤ π /2 .
A = 1 2 ∫ 0 π / 2 sin 2 ( 2 θ ) d θ = 1 2 ∫ 0 π / 2 1 − cos 4 θ 2 d θ = π 8 A = \frac{1}{2}\int_0^{\pi/2}\sin^2(2\theta)\,d\theta = \frac{1}{2}\int_0^{\pi/2}\frac{1-\cos 4\theta}{2}\,d\theta = \frac{\pi}{8} A = 2 1 ∫
Key Takeaways
Polar area: A = 1 2 ∫ α β r 2 d θ A = \frac{1}{2}\int_{\alpha}^{\beta}r^2\,d\theta A = 2 1 ∫ α β r 2 d θ
Between curves: 1 2 ∫ ( r outer 2 − r inner 2 ) d θ \frac{1}{2}\int(r_{\text{outer}}^2 - r_{\text{inner}}^2)\,d\theta 2 1 ∫ ( r outer 2
Use half-angle identities: cos 2 θ = 1 + cos 2 θ 2 \cos^2\theta = \frac{1+\cos 2\theta}{2} cos 2 θ = 2 1 + c o s 2 θ ,
Exploit symmetry to simplify calculations
Next: Part 4 covers slopes of polar curves (d y / d x dy/dx d y / d x in polar).
= f ( θ ) cos θ , y = r sin θ = f ( θ ) sin θ x = r\cos\theta = f(\theta)\cos\theta, \quad y = r\sin\theta = f(\theta)\sin\theta x = r cos θ = f ( θ ) cos θ , y = r sin θ = f ( θ ) sin θ
The Slope Formula d y d x = d r d θ sin θ + r cos θ d r d θ cos θ − r sin θ \boxed{\frac{dy}{dx} = \frac{\frac{dr}{d\theta}\sin\theta + r\cos\theta}{\frac{dr}{d\theta}\cos\theta - r\sin\theta}} d x d y = d θ d r cos θ − r sin θ d θ
This comes from the product rule:
d x / d θ = f ′ cos θ − f sin θ dx/d\theta = f'\cos\theta - f\sin\theta d x / d θ = f ′ cos θ − f sin θ
d y / d θ = f ′ sin θ + f cos θ dy/d\theta = f'\sin\theta + f\cos\theta d y / d θ = f ′ sin θ + f cos θ
Worked Example
Find the slope of r = 1 + cos θ r = 1 + \cos\theta r = 1 + cos θ at θ = π / 3 \theta = \pi/3 θ = π /3 .
r = 1 + cos ( π / 3 ) = 3 / 2 r = 1 + \cos(\pi/3) = 3/2 r = 1 + cos ( π /3 ) = 3/2 , d r / d θ = − sin ( π / 3 ) = − 3 / 2 dr/d\theta = -\sin(\pi/3) = -\sqrt{3}/2 d r / d θ = − sin ( π /3 ) = − 3
d y d x = ( − 3 / 2 ) sin ( π / 3 ) + ( 3 / 2 ) cos ( π / 3 ) ( − 3 / 2 ) cos ( π / 3 ) − ( 3 / 2 ) sin ( π / 3 ) \frac{dy}{dx} = \frac{(-\sqrt{3}/2)\sin(\pi/3) + (3/2)\cos(\pi/3)}{(-\sqrt{3}/2)\cos(\pi/3) - (3/2)\sin(\pi/3)} d x d
= ( − 3 / 2 ) ( 3 / 2 ) + ( 3 / 2 ) ( 1 / 2 ) ( − 3 / 2 ) ( 1 / 2 ) − ( 3 / 2 ) ( 3 / 2 ) = − 3 / 4 + 3 / 4 − 3 / 4 − 3 3 / 4 = 0 − 3 = 0 = \frac{(-\sqrt{3}/2)(\sqrt{3}/2) + (3/2)(1/2)}{(-\sqrt{3}/2)(1/2) - (3/2)(\sqrt{3}/2)} = \frac{-3/4 + 3/4}{-\sqrt{3}/4 - 3\sqrt{3}/4} = \frac{0}{-\sqrt{3}} = 0 =
The tangent is horizontal at θ = π / 3 \theta = \pi/3 θ = π /3 !
AP Tip: Horizontal tangents occur when d y / d θ = 0 dy/d\theta = 0 d y / d θ = 0 and d x / d θ ≠ 0 dx/d\theta \ne 0 d x / d θ = 0 . Vertical tangents when d x / d θ and .
Key Takeaways
Polar slope: d y d x = ( d r / d θ ) sin θ + r cos θ ( d r / d θ ) cos θ − r sin θ \frac{dy}{dx} = \frac{(dr/d\theta)\sin\theta + r\cos\theta}{(dr/d\theta)\cos\theta - r\sin\theta} d x d y = ( d r / d θ ) c o s θ − r s i n θ ( d r / d θ ) s i n θ + r c o s θ
Treat polar as parametric with θ \theta θ as the parameter
Horizontal tangent: numerator = 0 = 0 = 0 , denominator ≠ 0 \ne 0 = 0
At the origin: tangent line has slope tan θ 0 \tan\theta_0 tan θ 0 where f ( θ 0 ) = 0 f(\theta_0) = 0 f ( θ 0 ) = 0
Next: Part 5 covers arc length in polar coordinates.
β
L = ∫ α β r 2 + ( d r d θ ) 2 d θ \boxed{L = \int_{\alpha}^{\beta}\sqrt{r^2 + \left(\frac{dr}{d\theta}\right)^2}\,d\theta} L = ∫ α β r 2 + ( d θ d r ) 2 d θ
Derivation: From the parametric formula with x = r cos θ x = r\cos\theta x = r cos θ , y = r sin θ y = r\sin\theta y = r sin θ :
( d x / d θ ) 2 + ( d y / d θ ) 2 = ( r ′ ) 2 cos 2 θ − 2 r r ′ cos θ sin θ + r 2 sin 2 θ (dx/d\theta)^2 + (dy/d\theta)^2 = (r')^2\cos^2\theta - 2rr'\cos\theta\sin\theta + r^2\sin^2\theta ( d x / d θ ) 2 + ( d y / d θ ) 2 = ( r ′ ) 2 cos 2 θ − 2 r r ′ cos θ sin θ + r 2 sin 2 θ
+ ( r ′ ) 2 sin 2 θ + 2 r r ′ sin θ cos θ + r 2 cos 2 θ = ( r ′ ) 2 + r 2 + (r')^2\sin^2\theta + 2rr'\sin\theta\cos\theta + r^2\cos^2\theta = (r')^2 + r^2 + ( r ′ ) 2 sin 2
Key Fact: The polar arc length formula is simpler than the parametric one because the cross terms cancel!
Example 1: Arc Length of a Circle
r = a r = a r = a (constant). d r / d θ = 0 dr/d\theta = 0 d r / d θ = 0 .
L = ∫ 0 2 π a 2 + 0 d θ = a ⋅ 2 π = 2 π a ✓ L = \int_0^{2\pi}\sqrt{a^2+0}\,d\theta = a \cdot 2\pi = 2\pi a \checkmark L = ∫ 0 2 π a 2 + 0 d a ⋅ 2 π = 2 πa ✓
Example 2: Cardioid r = 1 + cos θ r = 1 + \cos\theta r = 1 + cos θ
d r / d θ = − sin θ dr/d\theta = -\sin\theta d r / d θ = − sin θ
L = ∫ 0 2 π ( 1 + cos θ ) 2 + sin 2 θ d θ L = \int_0^{2\pi}\sqrt{(1+\cos\theta)^2 + \sin^2\theta}\,d\theta L = ∫ 0 2 π ( 1 + cos θ
= ∫ 0 2 π 2 + 2 cos θ d θ = ∫ 0 2 π 4 cos 2 ( θ / 2 ) d θ = ∫ 0 2 π 2 ∣ cos ( θ / 2 ) ∣ d θ = \int_0^{2\pi}\sqrt{2 + 2\cos\theta}\,d\theta = \int_0^{2\pi}\sqrt{4\cos^2(\theta/2)}\,d\theta = \int_0^{2\pi}2|\cos(\theta/2)|\,d\theta = ∫ 0 2 π
Using symmetry: = 4 ∫ 0 π cos ( θ / 2 ) d θ = 4 [ 2 sin ( θ / 2 ) ] 0 π = 8 = 4\int_0^{\pi}\cos(\theta/2)\,d\theta = 4[2\sin(\theta/2)]_0^{\pi} = 8 = 4 ∫ 0 π cos ( θ /2 ) d θ =
AP Note: The half-angle identity 1 + cos θ = 2 cos 2 ( θ / 2 ) 1 + \cos\theta = 2\cos^2(\theta/2) 1 + cos θ = 2 cos 2 ( θ /2 ) is essential for cardioid problems.
Key Takeaways
Polar arc length: L = ∫ r 2 + ( d r / d θ ) 2 d θ L = \int\sqrt{r^2 + (dr/d\theta)^2}\,d\theta L = ∫ r 2 + ( d r / d θ ) 2 d θ
For a circle r = a r = a r = a : arc length on [ α , β ] [\alpha, \beta] [ α , β ] is a ( β − α ) a(\beta - \alpha) a ( β − α )
Half-angle identities simplify cardioid integrals
Logarithmic spiral r = e θ r = e^\theta r = e θ : integrand is e θ 2 e^\theta\sqrt{2} e θ 2 (nice!)
Next: Part 6 is a Problem-Solving Workshop with mixed polar problems.
(a)
A = 1 2 ∫ 0 π / 2 4 cos 2 θ d θ = 2 ∫ 0 π / 2 1 + cos 2 θ 2 d θ = [ θ + sin 2 θ 2 ] 0 π / 2 = π 2 A = \frac{1}{2}\int_0^{\pi/2}4\cos^2\theta\,d\theta = 2\int_0^{\pi/2}\frac{1+\cos 2\theta}{2}\,d\theta = [\theta + \frac{\sin 2\theta}{2}]_0^{\pi/2} = \frac{\pi}{2} A = 2 1 ∫ 0 π /2 4 cos 2 θ d θ = 2 ∫ 0 π /2 2 1 + c o s 2 θ d θ = [ θ + 2 s i n 2 θ ] 0 π /2 = 2 π
(b) Find d y / d x dy/dx d y / d x at θ = π / 6 \theta = \pi/6 θ = π /6 .
r = 3 r = \sqrt{3} r = 3 , d r / d θ = − 2 sin ( π / 6 ) = − 1 dr/d\theta = -2\sin(\pi/6) = -1 d r / d θ = − 2 sin ( π /6 ) = − 1
d y d x = ( − 1 ) ( 1 / 2 ) + 3 ( 3 / 2 ) ( − 1 ) ( 3 / 2 ) − 3 ( 1 / 2 ) = − 1 / 2 + 3 / 2 − 3 / 2 − 3 / 2 = 1 − 3 = − 1 3 \frac{dy}{dx} = \frac{(-1)(1/2) + \sqrt{3}(\sqrt{3}/2)}{(-1)(\sqrt{3}/2) - \sqrt{3}(1/2)} = \frac{-1/2 + 3/2}{-\sqrt{3}/2 - \sqrt{3}/2} = \frac{1}{-\sqrt{3}} = -\frac{1}{\sqrt{3}} d x d y = ( − 1 ) ( 3 /2 ) − 3 − 3 /2 − 3 − 3 1 = − 3 1
L = ∫ 0 π / 2 4 cos 2 θ + 4 sin 2 θ d θ = ∫ 0 π / 2 2 d θ = π L = \int_0^{\pi/2}\sqrt{4\cos^2\theta + 4\sin^2\theta}\,d\theta = \int_0^{\pi/2}2\,d\theta = \pi L = ∫ 0 π /2 4 cos 2 θ + 4 sin 2 θ d θ = ∫ 0 π /2 2 d θ = π
Workshop Recap
Polar Problem Checklist:
Identify the curve type (circle, cardioid, rose, etc.)
Determine symmetry and appropriate limits
Set up the correct integral (area: 1 2 r 2 \frac{1}{2}r^2 2 1 r 2 ; arc length: r 2 + ( r ′ ) 2 \sqrt{r^2+(r')^2} r 2 + ( r ′ ) 2 )
Use trig identities to evaluate
Check your answer against geometric intuition
Coming Up: Part 7 is the Comprehensive Review of polar calculus.
A = 1 2 ∫ α β r 2 d θ A = \frac{1}{2}\int_{\alpha}^{\beta}r^2\,d\theta A = 2 1 ∫ α β r 2 d θ
Area between curves 1 2 ∫ ( r out 2 − r in 2 ) d θ \frac{1}{2}\int(r_{\text{out}}^2 - r_{\text{in}}^2)\,d\theta 2 1 ∫ ( r out 2 − r in 2 ) d θ
Slope d y d x = r ′ sin θ + r cos θ r ′ cos θ − r sin θ \frac{dy}{dx} = \frac{r'\sin\theta + r\cos\theta}{r'\cos\theta - r\sin\theta} d x d y = r ′ c o s θ − r s i n θ r ′ s i n θ + r c o s θ
Arc length L = ∫ r 2 + ( r ′ ) 2 d θ L = \int\sqrt{r^2+(r')^2}\,d\theta L = ∫ r 2 + ( r ′ ) 2 d θ
Horizontal tangent d y / d θ = 0 dy/d\theta = 0 d y / d θ = 0 , d x / d θ ≠ 0 dx/d\theta \ne 0 d x / d θ = 0
Vertical tangent d x / d θ = 0 dx/d\theta = 0 d x / d θ = 0 , d y / d θ ≠ 0 dy/d\theta \ne 0 d y / d θ = 0
Curve Classification Summary
Equation Type Petals/Loops r = a r = a r = a Circle (origin-centered) — r = 2 a cos θ r = 2a\cos\theta r = 2 a cos θ Circle through origin — r = a + a cos θ r = a + a\cos\theta r = a + a cos θ Cardioid 0 loops r = a + b cos θ r = a + b\cos\theta r = a + b cos θ , $a > r = a + b cos θ r = a + b\cos\theta r = a + b cos θ , $a < r = a cos ( n θ ) r = a\cos(n\theta) r = a cos ( n θ ) , n n n oddRose n n n petalsr = a cos ( n θ ) r = a\cos(n\theta) r = a cos ( n θ ) , n n n evenRose 2 n 2n 2 n petalsr 2 = a cos ( 2 θ ) r^2 = a\cos(2\theta) r 2 = a cos ( 2 θ ) Lemniscate 2 loops
Polar Calculus Complete!
You have mastered:
Polar coordinates and conversions
Graphing polar curves and symmetry analysis
Polar area formula and area between curves
Slopes of polar curves via parametric conversion
Arc length in polar coordinates
AP Exam Note: The polar/parametric FRQ is one of the most predictable on the BC exam. Practice setting up area and arc length integrals with correct limits. Always check for intersections at the origin separately!
π
−
θ
0
2
π
/3
,
π
3 3 3 petals (odd coefficient), each spanning π / 3 \pi/3 π /3 radiansFirst petal: 0 ≤ θ ≤ π / 3 0 \le \theta \le \pi/3 0 ≤ θ ≤ π /3 , max r = 1 r = 1 r = 1 at θ = π / 6 \theta = \pi/6 θ = π /6 3 π /4 ≤ θ ≤ 5 π /4
Figure-eight shape through the origin
π
(
1
+
cos θ ) 2 d θ
cos
θ
+
cos 2 θ ) d θ =
∫ 0 π ( 2 3 + 2 cos θ + 2 c o s 2 θ ) d θ
4 s i n 2 θ
]
0 π
=
2 3 π
0 π /2
sin 2
(
2
θ
)
d
θ
=
2 1 ∫ 0 π /2 2 1 − c o s 4 θ d θ =
8 π
−
r inner 2 ) d θ
sin 2 θ = 1 − cos 2 θ 2 \sin^2\theta = \frac{1-\cos 2\theta}{2} sin 2 θ = 2 1 − c o s 2 θ
d r
sin
θ
+
r
cos
θ
/2
y
=
( − 3 /2 ) c o s ( π /3 ) − ( 3/2 ) s i n ( π /3 ) ( − 3 /2 ) s i n ( π /3 ) + ( 3/2 ) c o s ( π /3 )
=
0
= 0 dx/d\theta = 0 d x / d θ = 0
d y / d θ ≠ 0 dy/d\theta \ne 0 d y / d θ = 0
θ
+
2 r r ′ sin θ cos θ +
r 2 cos 2 θ =
( r ′ ) 2 +
r 2
θ
=
) 2
+
sin 2
θ
d
θ
d
θ
=
∫ 0 2 π 2∣ cos ( θ /2 ) ∣ d θ
4 [ 2 sin ( θ /2 ) ] 0 π =
8
(
1/2
)
=
/2
− 1/2 + 3/2
=