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Green's Theorem, circulation form Consider the following regions \(R\)and vector fields \(\mathbf{F}\) a. Compute the two-dimensional curl of the vector field. b. Evaluate both integrals in Green's Theorem and check for consistency. $$\mathbf{F}=\left\langle 0, x^{2}+y^{2}\right\rangle ; R=\left\\{(x, y): x^{2}+y^{2} \leq 1\right\\}$$

Short Answer

Expert verified
Question: Verify the Green's theorem for the vector field F and the region R, where F=<0, x^2+y^2> and R is the unit circle x^2+y^2≤1. Answer: By applying Green's theorem for the given vector field F=<0, x^2+y^2> and the region R, which is the unit circle x^2+y^2≤1, we found that both line integral and double integral were equal to 0, demonstrating that Green's theorem holds true for this vector field and region.

Step by step solution

01

Calculate Two-Dimensional Curl

Compute the partial derivatives of the functions \(P\) and \(Q\) and then find the two-dimensional curl as follows: $$Q = x^{2}+y^{2} \Rightarrow \frac{\partial Q}{\partial x} = 2x$$ $$P = 0 \Rightarrow \frac{\partial P}{\partial y} = 0$$ The two-dimensional curl of the vector field \(\mathbf{F}\) is: $$Curl(\mathbf{F}) = \frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y} = 2x - 0 = 2x$$
02

Evaluate the Line Integral

Now, we need to parametrize the boundary curve of region \(R\). Since \(R\) is a unit circle, we can define the parametric equations as: $$x(\theta) = \cos\theta$$ $$y(\theta) = \sin\theta$$ where \(0 \leq \theta \leq 2\pi\) Calculate derivatives of the parametric equations: $$\frac{dx}{d \theta} = \frac{\partial x}{\partial\theta}=-\sin\theta$$ $$\frac{dy}{d \theta} = \frac{\partial y}{\partial\theta}=\cos\theta$$ Substitute the parametric equations into the vector field: $$\mathbf{F}(x(\theta), y(\theta))= \langle 0, \cos^2\theta + \sin^2\theta \rangle =\langle 0, 1 \rangle$$ So, the line integral is: $$\oint_{C} P dx + Q dy = \int_{0}^{2\pi}\langle 0, 1 \rangle \cdot (-\sin\theta, \cos\theta) d\theta = \int_{0}^{2\pi}\cos\theta d \theta $$ Evaluate the integral: $$\int_{0}^{2\pi}\cos\theta d \theta = \left[\sin\theta\right]_0^{2\pi} = 0$$
03

Evaluate the Double Integral

The double integral of the two-dimensional curl over region \(R\) can be computed as: $$\iint_{R} Curl(\mathbf{F}) dA = \iint_{R} 2x dA$$ To evaluate this, we will use polar coordinates. In polar coordinates, \(dA = r dr d\theta\), and \(x = r \cos\theta\). So, the integral becomes: $$\iint_{R} 2x dA = \int_{0}^{2\pi} \int_{0}^{1} 2r\cos\theta r dr d\theta$$ Evaluate the integral: $$\int_{0}^{2\pi} \int_{0}^{1} 2r^2\cos\theta dr d\theta = \left(\int_{0}^{2\pi} \cos\theta d\theta\right)\left(\int_{0}^{1} 2r^2 dr\right) = \left[\sin\theta\right]_0^{2\pi} \left[\frac{2}{3}r^3\right]_0^1$$ $$= 0 \cdot \left(\frac{2}{3}\right) = 0$$
04

Check for Consistency

We have calculated the line integral and the double integral as follows: $$\oint_{C} P dx + Q dy = 0$$ $$\iint_{R} Curl(\mathbf{F}) dA = 0$$ Since both integrals have the same value, we can conclude that the results are consistent, and Green's Theorem holds true for this vector field and region.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Vector Fields
In mathematics, a vector field is a map that assigns a vector to every point in a given space. In the context of Green's Theorem, we typically deal with planar (or 2-dimensional) vector fields. For our example, the vector field \( \mathbf{F} \) is represented as \( \langle 0, x^2 + y^2 \rangle \).
This means that for every point \((x, y)\) on the plane, the vector \( \mathbf{F} \) is purely vertical, with a magnitude determined by \( x^2 + y^2 \).
There are key components to understanding vector fields like:
  • Direction and Magnitude: The direction of the vector field is determined by how the vectors point, and magnitude refers to their length.
  • Visualization: You can visualize a vector field by drawing arrows on a plane where the direction and length of each arrow represent the vector at that point.
This foundational concept is crucial while applying Green's Theorem as it links the concepts of line integrals and surfaces.
Two-Dimensional Curl
The curl of a vector field measures how much and in what manner the field tends to rotate around a point. In 2-dimensions, the curl is a scalar value rather than a vector.
Calculating Two-Dimensional Curl:
  • For a vector field \( \mathbf{F} = \langle P, Q \rangle \), the curl is given by the expression \( Curl(\mathbf{F}) = \frac{\partial Q}{\partial x} - \frac{\partial P}{\partial y} \).
  • In this exercise, with \( P = 0 \) and \( Q = x^2 + y^2 \), the curl simplifies to \( 2x \).
Hence, the curl provides insight into the rotational tendency of \( \mathbf{F} \) at any point in region \( R \). This is a pivotal step in understanding how the line and double integrals relate through Green's Theorem.
Line Integral
A line integral represents the integration of a function along a curve. This is a central piece of Green's Theorem that relates the integral around a closed curve to the area inside.
Understanding Line Integrals:
  • The vector field \( \mathbf{F} = \langle 0, x^2 + y^2 \rangle \) should be evaluated over a boundary curve which, in this exercise, is a unit circle defined by \( x^2 + y^2 = 1 \).
  • Using parametric equations \( x(\theta) = \cos\theta \), \( y(\theta) = \sin\theta \), one calculates derivatives and substitutes back into the integral.
  • The integral becomes \( \int_{0}^{2\pi} \cos\theta \, d\theta \), which evaluates to zero.
This result indicates that the overall effect of the vector field along this particular path sums to zero, aligning perfectly with what the double integral shows.
Double Integral
A double integral extends the idea of a single integral to functions of two variables, often used to find areas or volumes. In Green's Theorem, the double integral involves integrating the curl over the area enclosed by a curve.
Working with Double Integrals:
  • Here, we take the curl calculated as \( 2x \) and use polar coordinates to simplify integration over the circular region \( R \).
  • Transforming the integral into polar coordinates, we set \( x = r\cos\theta \) and the area element \( dA = r\, dr\, d\theta \).
  • Hence, the integral becomes \( \int_{0}^{2\pi} \int_{0}^{1} 2r^2\cos\theta \, dr \, d\theta \), also evaluating to zero.
Much like the line integral, this zero result confirms the absence of net rotation, demonstrating consistency through Green's Theorem.

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Most popular questions from this chapter

Mass and center of mass Let \(S\) be a surface that represents a thin shell with density \(\rho .\) The moments about the coordinate planes (see Section 16.6 ) are \(M_{y z}=\iint_{S} x \rho(x, y, z) d S, M_{x z}=\iint_{S} y \rho(x, y, z) d S\) and \(M_{x y}=\iint_{S} z \rho(x, y, z) d S .\) The coordinates of the center of mass of the shell are \(\bar{x}=\frac{M_{y z}}{m}, \bar{y}=\frac{M_{x z}}{m},\) and \(\bar{z}=\frac{M_{x y}}{m},\) where \(m\) is the mass of the shell. Find the mass and center of mass of the following shells. Use symmetry whenever possible. The constant-density hemispherical shell \(x^{2}+y^{2}+z^{2}=a^{2}\) \(z \geq 0\)

Alternative construction of potential functions in \(\mathbb{R}^{2}\) Assume the vector field \(\mathbf{F}\) is conservative on \(\mathbb{R}^{2}\), so that the line integral \(\int_{C} \mathbf{F} \cdot d \mathbf{r}\) is independent of path. Use the following procedure to construct a potential function \(\varphi\) for the vector field \(\mathbf{F}=\langle f, g\rangle=\langle 2 x-y,-x+2 y\rangle\) a. Let \(A\) be (0,0) and let \(B\) be an arbitrary point \((x, y) .\) Define \(\varphi(x, y)\) to be the work required to move an object from \(A\) to \(B\) where \(\varphi(A)=0 .\) Let \(C_{1}\) be the path from \(A\) to \((x, 0)\) to \(B\), and let \(C_{2}\) be the path from \(A\) to \((0, y)\) to \(B\). Draw a picture. b. Evaluate \(\int_{C_{1}} \mathbf{F} \cdot d \mathbf{r}=\int_{C_{1}} f d x+g d y\) and conclude that \(\varphi(x, y)=x^{2}-x y+y^{2}\). c. Verify that the same potential function is obtained by evaluating the line integral over \(C_{2}\).

Surface area of a torus a. Show that a torus with radii \(R > r\) (see figure) may be described parametrically by \(\mathbf{r}(u, v)=\langle(R+r \cos u) \cos v\) \((R+r \cos u) \sin v, r \sin u\rangle,\) for \(0 \leq u \leq 2 \pi, 0 \leq v \leq 2 \pi\) b. Show that the surface area of the torus is \(4 \pi^{2} R r\)

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