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Evaluate the surface integral \(\iint_{S} f(x, y, z) d S\) using a parametric description of the surface. \(f(x, y, z)=x^{2}+y^{2},\) where \(S\) is the hemisphere \(x^{2}+y^{2}+z^{2}=36,\) for \(z \geq 0\)

Short Answer

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Question: Evaluate the surface integral \(\iint_{S} f(x, y, z) d S\) with function \(f(x, y, z) = x^{2} + y^{2}\) over the surface \(S\), which is the hemisphere described by the equation \(x^{2} + y^{2} + z^{2} = 36\) with \(z \geq 0\). Answer: The surface integral \(\iint_{S} f(x, y, z) d S = 36^2\pi\).

Step by step solution

01

Parametric description of the surface

We can use spherical coordinates to parametrize the hemisphere, given by the equation: \(x^{2}+y^{2}+z^{2}=36\). We will use the variables \(r\), \(\theta\), and \(\phi\), where \(r=6\), \(0 \leq \theta \leq 2\pi\), and \(0 \leq \phi \leq \frac{\pi}{2}\). Then, we can find the parametric equations for \(x\), \(y\), and \(z\) as follows: $$ x = r\sin{\phi}\cos{\theta} \\ y = r\sin{\phi}\sin{\theta} \\ z = r\cos{\phi} $$ Since \(r = 6\), we can substitute it in the equations to get: $$ x = 6\sin{\phi}\cos{\theta} \\ y = 6\sin{\phi}\sin{\theta} \\ z = 6\cos{\phi} $$
02

Compute the differential area element

Next, we need the differential area element \(dS\). We can find this by computing the cross product of the partial derivatives of the parametric equations with respect to \(\theta\) and \(\phi\). First, we find these partial derivatives: $$ \frac{\partial(x, y, z)}{\partial\theta} = \left(-6\sin{\phi}\sin{\theta}, 6\sin{\phi}\cos{\theta}, 0\right) \\ \frac{\partial(x, y, z)}{\partial\phi} = \left(6\cos{\phi}\cos{\theta}, 6\cos{\phi}\sin{\theta}, -6\sin{\phi}\right) $$ Next, we compute the cross product of these partial derivatives: $$ \frac{\partial(x, y, z)}{\partial\theta} \times \frac{\partial(x, y, z)}{\partial\phi} = \left(-36\sin^2{\phi}\cos{\theta}, -36\sin^2{\phi}\sin{\theta}, 36\sin{\phi}\cos{\phi}\right) $$ Now, we need to find the magnitude of this vector, which will give us the differential area element \(dS\): $$ dS = \sqrt{(-36\sin^2{\phi}\cos{\theta})^2 + (-36\sin^2{\phi}\sin{\theta})^2 + (36\sin{\phi}\cos{\phi})^2}d\theta d\phi $$ Simplifying, we get: $$ dS = 36\sin\phi\, d\theta d\phi $$
03

Substitute the parametric description and the differential area element into the integral

Now, we substitute the values for \(x\), \(y\), \(z\), and \(dS\) into our integral, along with the function \(f(x, y, z) = x^2 + y^2\). We get: $$ \iint_{S} f(x, y, z) d S = \int_0^{2\pi} \int_0^{\frac{\pi}{2}} (6\sin{\phi}\cos{\theta})^2 + (6\sin{\phi}\sin{\theta})^2\cdot 36\sin{\phi} \, d\theta d\phi $$
04

Evaluate the integral

We can now proceed to evaluate the integral. First, we notice that the integrand is separable, so we can rewrite the integral as a product of two separate integrals: $$ \int_0^{2\pi} \int_0^{\frac{\pi}{2}} (36\sin^2{\phi}\cos^2{\theta} + 36\sin^2{\phi}\sin^2{\theta})\cdot 36\sin{\phi} \, d\theta d\phi \\ = 36^2\int_0^{2\pi}(\cos^2\theta+\sin^2\theta)\, d\theta \int_0^{\frac{\pi}{2}}\sin^3\phi\, d\phi $$ We will now evaluate the two separate integrals: 1) \(\int_0^{2\pi} (\cos^2\theta+\sin^2\theta) \, d\theta\): $$ =\int_0^{2\pi} 1 \, d\theta \\ = \theta\Bigg|_0^{2\pi} \\ = 2\pi $$ 2) \(\int_0^{\frac{\pi}{2}} \sin^3\phi \, d\phi\). To compute this integral, use the power reduction formula: \(\sin^2\phi = \frac{1}{2}(1 - \cos{2\phi})\) $$ \int_0^{\frac{\pi}{2}} \sin\phi\sin^2\phi \, d\phi = \int_0^{\frac{\pi}{2}} \sin\phi\cdot \frac{1}{2}(1 - \cos{2\phi}) \, d\phi \\ = \frac{1}{2}\int_0^{\frac{\pi}{2}} \sin\phi - \sin\phi\cos{2\phi} \, d\phi \\ = \frac{1}{2}\left[(-\cos\phi)\Bigg|^{\frac{\pi}{2}}_0 + \frac{1}{2}\sin{2\phi}\Bigg|^{\frac{\pi}{2}}_0\right]\\ = \frac{1}{2}\left[ \left(-\cos{\frac{\pi}{2}} + \cos{0} \right) + \frac{1}{2}\left(\sin{2\cdot\frac{\pi}{2}} - \sin{0}\right)\right] \\ = \frac{1}{2}(1)\\\ By multiplying the two integrals, we find the value of the surface integral: $$ \iint_{S} f(x, y, z) d S = 36^2(2\pi)\left(\frac{1}{2}\right) = 36^2\pi $$ Therefore, the surface integral \(\iint_{S} f(x, y, z) d S = 36^2\pi\).

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Key Concepts

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

Spherical Coordinates
When encountering complex surface integrals, especially ones that involve symmetric surfaces such as spheres, cones, or cylinders, translating the problem into spherical coordinates can greatly simplify the process. In a three-dimensional space, instead of using the Cartesian coordinates \(x, y, z\), we can describe a point by its distance from the origin \(r\), the angle \(\theta\) from the x-axis in the xy-plane, and the angle \(\phi\) from the positive z-axis towards the xy-plane.

In the case of a hemisphere with radius 6, like in our problem, the spherical coordinates for any point on the surface are \(r=6\), \(\theta\) ranging from \(0\) to \(2\pi\), and \(\phi\) from \(0\) to \(\frac{\pi}{2}\). Converting the hemispherical equation using spherical coordinates allows the integration boundaries to be clearly defined and more manageable, aiding in the calculation of the surface integral.
Parametric Equations
Parametric equations open up a streamlined path to describe geometric surfaces. Rather than fixating on a single equation, we employ a set of equations that each capture a separate variable as a function of one or more parameters. This can be particularly adept for defining curves and surfaces where the Cartesian approach might become unwieldy.

For our hemisphere, the parametric equations in terms of spherical coordinates are: \[ x = r\sin{\phi}\cos{\theta} \] \[ y = r\sin{\phi}\sin{\theta} \] \[ z = r\cos{\phi} \] where \(r\) remains constant at 6. These equations beautifully encapsulate every point on the hemispherical surface by varying \(\theta\) and \(\phi\), enabling us to express the surface integral in terms of these new variables.
Differential Area Element
The differential area element is a crucial concept in surface integration, serving as the infinitesimal element of area over the surface to be integrated. Think of it as a tiny patch of area on the surface, and what we're doing through integration is summing up all these tiny patches over the entire surface.

In the spherical coordinate system, after finding the parametric representation of our hemisphere, we obtain the differential area element by considering the cross product of the partial derivatives of the parametric equations with respect to \(\theta\) and \(\phi\). The resulting vector's magnitude yields the area element \(dS\), which, in our exercise, simplifies to \[ dS = 36\sin\phi\, d\theta d\phi \] This formula represents the size of each infinitesimal patch of the hemisphere's surface in terms of \(\theta\) and \(\phi\), allowing for the integration over the entire surface.
Power Reduction Formula
The power reduction formula is a particularly handy tool in integral calculus, especially when dealing with trigonometric integrals involving powers. It simplifies calculations by reducing powers of sine and cosine to first powers times a trigonometric function.

When faced with an integrand like \(\sin^3\phi\), as in our exercise, the power reduction formula \(\sin^2\phi = \frac{1}{2}(1 - \cos{2\phi})\) is used to transform the integral of the third power into an integral involving the first power and a cosine term. Once we apply this simplification, integrating becomes much more straightforward, leading to the evaluation of the integral and, subsequently, determining the value of the original surface integral.

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Most popular questions from this chapter

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