Analyze polar curves across selected intervals confidently. Get integrals, area, arc length, and export summaries. Useful for lessons, homework, verification, and deeper curve insight.
Choose a polar model, set the interval, then compute integral, area, arc length, and summary metrics in one step.
These examples show how different polar models affect the definite integral, sector area, and arc length across selected intervals.
| Function | Interval | Definite Integral | Sector Area | Arc Length |
|---|---|---|---|---|
| r(θ) = 3 + 2 sin(θ) | 0 to π/2 | 6.712389 | 14.639380 | 7.105739 |
| r(θ) = 1 + 0.5θ | 0 to π | 5.608994 | 5.330126 | 5.838850 |
| r(θ) = θ² | 0 to 1 | 0.333333 | 0.100000 | 1.060113 |
Definite integral: I = ∫θ₁θ₂ r(θ) dθ
Polar sector area: A = 1/2 ∫θ₁θ₂ [r(θ)]² dθ
Average radius: r̄ = I / (θ₂ - θ₁)
RMS radius: rrms = √[(1 / (θ₂ - θ₁)) ∫θ₁θ₂ [r(θ)]² dθ]
Arc length: L = ∫θ₁θ₂ √([r(θ)]² + [dr/dθ]²) dθ
This calculator evaluates the chosen polar model numerically with Simpson’s rule. That method is accurate for smooth functions and works well for trigonometric, polynomial, linear, exponential, and mixed expressions.
The integral reports the accumulation of radius over angle. The area reports the swept region, while the arc length follows the actual curve traced by the polar function.
It calculates the definite integral of r(θ), polar sector area, arc length, average radius, RMS radius, and sampled radius values over your chosen angular interval.
Different polar models need different parameters. Unused coefficients can stay at zero or default values without affecting models that do not reference them.
Use degrees when your problem statement is written in degrees. Use radians when formulas, graphing tools, or theoretical work already use radian measure.
Simpson’s rule approximates the integral by fitting smooth parabolic segments across many small subintervals. It generally gives strong accuracy for well-behaved polar functions.
The calculator uses an ordered interval for clear geometric interpretation. Requiring a larger ending angle avoids confusion in area, arc length, and summary statistics.
Yes. Polar curves can produce negative radius values, which reflect points across the origin. The integral uses the actual signed radius, while the area squares it.
Start with 1000 for smooth curves. Increase the count when the curve oscillates rapidly or contains steep changes, then compare whether the results stabilize.
The exports include the selected model, interval, summary metrics, and the sample angle-radius table so you can save, share, or reuse the analysis.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.