Problem 41
Question
Average distance to a given point inside a disk Let \(P_{0}\) be a point inside a circle of radius \(a\) and let \(h\) denote the distance from \(P_{0}\) to the center of the circle. Let \(d\) denote the distance from an arbitrary point \(P\) to \(P_{0} .\) Find the average value of \(d^{2}\) over the region enclosed by the circle. (Hint: Simplify your work by placing the center of the circle at the origin and \(P_{0}\) on the \(x\) -axis.)
Step-by-Step Solution
Verified Answer
The average of \(d^2\) over the disk is \(\frac{a^2}{2} + h^2\)."
1Step 1: Set Up the Coordinate System
Place the center of the circle at the origin of a coordinate system. Assume that point \(P_0\) is located at \((h,0)\) on the \(x\)-axis, which simplifies calculations due to symmetry.
2Step 2: Define Points and Distances
Let an arbitrary point \(P\) in the disk be denoted by its coordinates \((x,y)\). The distance \(d\) from \(P\) to \(P_0\) is given by the Euclidean distance formula: \(d^2 = (x-h)^2 + y^2\).
3Step 3: Integrate Over the Circle
We need to calculate the average value of \(d^2\) over the disk of radius \(a\). This requires integrating \(d^2\) over the circular region \(x^2 + y^2 \leq a^2\):\[\frac{1}{\pi a^2} \int_{x^2 + y^2 \leq a^2} ((x-h)^2 + y^2) \, dx \, dy\].
4Step 4: Convert to Polar Coordinates
Transform the integral from Cartesian \(x,y\) to polar coordinates \(r,\theta\) where \((x,y) = (r \cos \theta, r \sin \theta)\). Limits for \(r\) will be from 0 to a and for \(\theta\) from 0 to \(2\pi\). The distance formula becomes: \[(r \cos \theta - h)^2 + (r \sin \theta)^2 = r^2 - 2hr \cos \theta + h^2\].
5Step 5: Calculate the Polar Integrals
Compute the integral for each component separately: 1. \(\int_0^{2\pi}\int_0^a r^2 \cdot r \, dr \, d\theta\)2. \(\int_0^{2\pi}\int_0^a -2hr \cos \theta \cdot r \, dr \, d\theta\)3. \(\int_0^{2\pi}\int_0^a h^2 \cdot r \, dr \, d\theta\)Each integral will be solved and summed to find the average \(d^2\).
6Step 6: Solve the Integrals
1. Solve \(\int_0^{2\pi}\int_0^a r^3 \, dr \, d\theta = 2\pi\frac{a^4}{4}\)2. Solve \(\int_0^{2\pi}\int_0^a -2hr^2 \cos \theta \, dr \, d\theta = 0\) because \(\int_0^{2\pi} \cos \theta \, d\theta = 0\)3. Solve \(\int_0^{2\pi}\int_0^a h^2r \, dr \, d\theta = h^2\pi a^2\)
7Step 7: Combine Results and Average
Add the results: \[\frac{1}{\pi a^2} \left(\pi \frac{a^4}{2} + h^2 \pi a^2\right) = \frac{a^2}{2} + h^2\].This is the average value of \(d^2\).
Key Concepts
Polar Coordinates IntegrationEuclidean Distance FormulaCircle GeometryIntegration in Polar Coordinates
Polar Coordinates Integration
Polar coordinates allow us to describe the location of a point using radius and angle. In our case, polar coordinates simplify the integration process over a circular region, because circular shapes naturally align with polar symmetry. Rather than defining a point by its Cartesian coordinates
When integrating in polar coordinates, it's important to account for the "differential area element" in polar coordinates, which is \(r \, dr \, d\theta\). This arises because the tiny sectors of our circular region become slightly larger as \(r\) increases. This is reflected in the formula for area in polar integrations.
Switching to polar coordinates is particularly advantageous since it aligns perfectly with the geometry of the disk, making the evaluation of such integrals straightforward.
- \(x = r \cos \theta\)
- \(y = r \sin \theta\)
When integrating in polar coordinates, it's important to account for the "differential area element" in polar coordinates, which is \(r \, dr \, d\theta\). This arises because the tiny sectors of our circular region become slightly larger as \(r\) increases. This is reflected in the formula for area in polar integrations.
Switching to polar coordinates is particularly advantageous since it aligns perfectly with the geometry of the disk, making the evaluation of such integrals straightforward.
Euclidean Distance Formula
The Euclidean distance formula measures the straight-line distance between two points in a plane. It's a fundamental concept in geometry and crucial for problems involving average distances.
For a point \(P\) located at coordinates \((x, y)\) and a point \(P_0\) at \((h, 0)\), the Euclidean distance \(d\) is defined as:
For a point \(P\) located at coordinates \((x, y)\) and a point \(P_0\) at \((h, 0)\), the Euclidean distance \(d\) is defined as:
- \(d = \sqrt{(x - h)^2 + y^2}\)
- \(d^2 = (x - h)^2 + y^2\)
Circle Geometry
Understanding circle geometry is essential, particularly when the region of interest is circular in shape. A circle is defined by its radius and center point, with every point lying a fixed distance (the radius) from this center.
Thanks to the circle's inherent symmetry, issues like polar symmetry ease the transition to polar coordinates. For integration, knowing that the geometric properties remain consistent can save significant time and help intuitively grasp integration boundaries.
- The equation \(x^2 + y^2 \leq a^2\) defines the interior of a circle with radius \(a\) centered at the origin.
- Many geometrical properties, such as symmetry, can simplify integration problems over circular regions.
Thanks to the circle's inherent symmetry, issues like polar symmetry ease the transition to polar coordinates. For integration, knowing that the geometric properties remain consistent can save significant time and help intuitively grasp integration boundaries.
Integration in Polar Coordinates
Integration in polar coordinates is a method particularly useful for problems involving circles or sectors of circles. By shifting from Cartesian coordinates, we align with the natural symmetry of circular objects, easing calculation and facilitating understanding.
When converting a Cartesian integral to polar coordinates, certain steps should be followed:
When converting a Cartesian integral to polar coordinates, certain steps should be followed:
- Define each \(x, y\) term in terms of \(r, \theta\).
- Replace \(dx \, dy\) with \(r \, dr \, d\theta\).
- Adjust limits to match \(r\) from 0 to the radius of the circle, and \(\theta\) from 0 to \(2\pi\).
Other exercises in this chapter
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