/*! This file is auto-generated */ .wp-block-button__link{color:#fff;background-color:#32373c;border-radius:9999px;box-shadow:none;text-decoration:none;padding:calc(.667em + 2px) calc(1.333em + 2px);font-size:1.125em}.wp-block-file__button{background:#32373c;color:#fff;text-decoration:none} Problem 17 Evaluate \(\int_{C} x y d x+(x+y... [FREE SOLUTION] | 91Ó°ÊÓ

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Evaluate \(\int_{C} x y d x+(x+y) d y\) along the curve \(y=x^{2}\) from \((-1,1)\) to \((2,4) .\)

Short Answer

Expert verified
The integral evaluates to \(\frac{207}{12}\).

Step by step solution

01

Understand the Curve

The given curve is defined by the equation \(y = x^2\). This means that as \(x\) changes, \(y\) is determined by \(y = x^2\). We will use this in order to substitute \(y\) into the integrand.
02

Parametrize the Curve

Since \(y = x^2\), the curve can be parametrized with \(x = t\) and \(y = t^2\) from \(t = -1\) to \(t = 2\). This sets our parameter domain and expressions for \(x\) and \(y\).
03

Differentiate for Integration

Calculate \(dy\) in terms of \(dt\) as \(dy = 2t \, dt\). Since \(dx = dt\) directly from the parametrization \(x = t\). Use these to express the differentials in terms of \(t\).
04

Substitution into the Integral

Substitute \(x = t\), \(y = t^2\), \(dx = dt\), and \(dy = 2t \, dt\) into the line integral: \[\int_{-1}^{2} (t \, t^2 \, dt + (t + t^2) \, 2t \, dt)\]
05

Simplify the Integrand

Simplify the expression inside the integral:\[\int_{-1}^{2} (t^3 \, dt + (t + t^2) 2t \, dt) = \int_{-1}^{2} (t^3 + 2t^2 + 2t^3) \, dt= \int_{-1}^{2} (3t^3 + 2t^2) \, dt\]
06

Integrate with Respect to t

Calculate the integral:\[\int_{-1}^{2} (3t^3 + 2t^2) \, dt = \left[\frac{3}{4}t^4 + \frac{2}{3}t^3 \right]_{-1}^{2}\]Evaluate this expression at the bounds: \(\left. \frac{3}{4}t^4 + \frac{2}{3}t^3 \right|_{-1}^{2} = \left( \frac{3}{4}(2)^4 + \frac{2}{3}(2)^3 \right) - \left( \frac{3}{4}(-1)^4 + \frac{2}{3}(-1)^3 \right)\).
07

Calculate the Result

Calculate the values:For \(t = 2\): \[\frac{3}{4}(2)^4 + \frac{2}{3}(2)^3 = \frac{3}{4}(16) + \frac{2}{3}(8) = 12 + \frac{16}{3} = \frac{52}{3}\]For \(t = -1\): \[\frac{3}{4}(-1)^4 + \frac{2}{3}(-1)^3 = \frac{3}{4}(1) + \frac{2}{3}(-1) = \frac{3}{4} - \frac{2}{3} = \frac{1}{12}\]Now, subtract the evaluated terms: \[\frac{52}{3} - \frac{1}{12} = \frac{207}{12}\].

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Key Concepts

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

Parametrization
Parametrization is a powerful technique in calculus used to simplify complex integrations, especially those involving curves. When dealing with line integrals, we often encounter curves represented by equations like \( y = x^2 \). This presents a challenge when integrating directly with respect to \(x\) or \(y\). By using a parameter, usually denoted as \(t\), we express both \(x\) and \(y\) in terms of \(t\).

For example, in the exercise, the curve \( y = x^2 \) can be parametrized by setting \( x = t \) and \( y = t^2 \). This transformation allows us to work within a familiar interval for \( t \), here from \(-1\) to \(2\). This process not only simplifies the expression but maintains the geometric nature of the problem.

  • Convert any complex equation into simpler forms using parameters.
  • Set limits for the parameter, which directly translate to limits in integration.
  • Ensure that all expressions are consistently transformed, including differential elements.
This is a crucial step because a well-chosen parametrization can make integration straightforward, reducing the problem to a single-variable calculus scenario.
Curve Integration
Curve integration, particularly line integrals, is central when working with vector fields and paths in vector calculus. Understanding curve integration helps evaluate functions over a path, instead of along the usual axis. In our scenario, we aimed to evaluate the line integral of \( \int_{C} x y \, dx + (x+y) \, dy \) along the curve \( y = x^2 \).

To start, after parametrizing the curve as \( x = t \), \( y = t^2 \), we substitute these into the integral. This creates a new expression involving the derivatives \( dx = dt \) and \( dy = 2t \, dt \).

By substituting:
  • \( x = t \)
  • \( y = t^2 \)
  • \( dx = dt \)
  • \( dy = 2t \, dt \)
the line integral becomes \( \int_{-1}^{2} (t t^2 \, dt + (t + t^2) \, 2t \, dt) \). Thus, the complicated path \( C \) is simplified, allowing a direct calculation using standard integral techniques.

This step allows us to deal with integrals involving paths not parallel to axes, using the outlines provided by the curve itself in the parameter domain.
Fundamental Theorem of Calculus
The Fundamental Theorem of Calculus plays a pivotal role in simplifying the evaluation of integrals, turning complex definite integrals into a simple subtraction of two function values. Once we have parametrized the curve and substituted all necessary components into the integral, we end with an expression \( \int_{-1}^{2} (3t^3 + 2t^2) \, dt \).

Applying the Fundamental Theorem, we find the antiderivative, \( \frac{3}{4}t^4 + \frac{2}{3}t^3 \). The final step involves evaluating this antiderivative at the endpoints, \(-1\) and \(2\).

Calculate:
  • For \( t = 2 \): \( \frac{3}{4}(2)^4 + \frac{2}{3}(2)^3 \)
  • For \( t = -1 \): \( \frac{3}{4}(-1)^4 + \frac{2}{3}(-1)^3 \)
Subtract these results to find the solution to the integral: \( \left( \frac{52}{3} \right) - \left( \frac{1}{12} \right) = \frac{207}{12} \).

This theorem thus streamlines the final evaluation process, turning multi-step integration problems into a more manageable exercise, relying entirely on evaluating the differences of the function's antiderivatives.

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Most popular questions from this chapter

Conservation of mass \(\quad\) Let \(\mathbf{v}(t, x, y, z)\) be a continuously differ- entiable vector field over the region \(D\) in space and let \(p(t, x, y, z)\) be a continuously differentiable scalar function. The variable \(t\) represents the time domain. The Law of Conservation of Mass asserts that $$\frac{d}{d t} \iiint_{D} p(t, x, y, z) d V=-\iint_{S} p \mathbf{v} \cdot \mathbf{n} d \sigma$$ where \(S\) is the surface enclosing \(D\) a. Give a physical interpretation of the conservation of mass law if \(v\) is a velocity flow field and \(p\) represents the density of the fluid at point \((x, y, z)\) at time \(t .\) b. Use the Divergence Theorem and Leibniz's Rule, $$\frac{d}{d t} \iiint_{D} p(t, x, y, z) d V=\iiint_{D} \frac{\partial p}{\partial t} d V$$ to show that the Law of Conservation of Mass is equivalent to the continuity equation, $$\nabla \cdot p \mathbf{v}+\frac{\partial p}{\partial t}=0$$ (In the first term \(\nabla \cdot p \mathbf{v}\) , the variable \(t\) is held fixed, and in the second term \(\partial p / \partial t,\) it is assumed that the point \((x, y, z)\) in \(D\) is held fixed.)

In Exercises \(35-44,\) use a parametrization to find the flux \(\iint_{S} \mathbf{F} \cdot \mathbf{n} d \sigma\) across the surface in the given direction. Cylinder \(\mathbf{F}=x \mathbf{i}+y \mathbf{j}+z \mathbf{k}\) outward through the portion of the cylinder \(x^{2}+y^{2}=1\) cut by the planes \(z=0\) and \(z=a\)

Let \(S\) be the portion of the cylinder \(y=e^{x}\) in the first octant that projects parallel to the \(x\) -axis onto the rectangle \(R_{y z} : 1 \leq y \leq 2\) \(0 \leq z \leq 1\) in the \(y z\) -plane (see the accompanying figure). Let \(\mathbf{n}\) be the unit vector normal to \(S\) that points away from the \(y z\) -plane. Find the flux of the field \(\mathbf{F}(x, y, z)=-2 \mathbf{i}+2 y \mathbf{j}+z \mathbf{k}\) across \(S\) in the direction of \(\mathbf{n} .\)

Bendixson's criterion The streamlines of a planar fluid flow are the smooth curves traced by the fluid's individual particles. The vectors \(\mathbf{F}=M(x, y) \mathbf{i}+N(x, y) \mathbf{j}\) of the flow's velocity field are the tangent vectors of the streamlines. Show that if the flow takes place over a simply connected region \(R\) (no holes or missing points) and that if \(M_{x}+N_{y} \neq 0\) throughout \(R\) , then none of the streamlines in \(R\) is closed. In other words, no particle of fluid ever has a closed trajectory in \(R .\) The criterion \(M_{x}+N_{y} \neq 0\) is called Bendixson's criterion for the nonexistence of closed trajectories.

In Exercises \(37-40, \mathbf{F}\) is the velocity field of a fluid flowing through a region in space. Find the flow along the given curve in the direction of increasing \(t .\) $$ \begin{array}{l}{\mathbf{F}=(x-z) \mathbf{i}+x \mathbf{k}} \\\ {\mathbf{r}(t)=(\cos t) \mathbf{i}+(\sin t) \mathbf{k}, \quad 0 \leq t \leq \pi}\end{array} $$

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