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Ch. 6 - Applications of Integration
Briggs - Calculus: Early Transcendentals 3rd Edition
Briggs3rd EditionCalculus: Early TranscendentalsISBN: 9780136847243Not the one you use?Change textbook
Chapter 6, Problem 6.1.46a

Flow rates in the Spokane River The daily discharge of the Spokane River as it flows through Spokane, Washington, in April and June is modeled by the functions
r1(t) = 0.25t²+37.46t+722.47 (April) and
r2(t) = 0.90t²−69.06t+2053.12 (June), where the discharge is measured in millions of cubic feet per day, and t=0 corresponds to the beginning of the first day of the month (see figure).
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a. Determine the total amount of water that flows through Spokane in April (30 days). 

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Identify the function that models the daily discharge for April, which is given as \(r_1(t) = 0.25t^2 + 37.46t + 722.47\), where \(t\) is the number of days from the start of April and \(r_1(t)\) is the discharge in millions of cubic feet per day.
Understand that the total amount of water discharged over the 30 days of April is the integral of the discharge rate function \(r_1(t)\) from \(t=0\) to \(t=30\). This is because integration sums up the continuous flow over time.
Set up the definite integral to find the total discharge: \(\int_0^{30} (0.25t^2 + 37.46t + 722.47) \, dt\).
Integrate the function term-by-term: the integral of \$0.25t^2\( is \(\frac{0.25}{3}t^3\), the integral of \)37.46t\( is \(\frac{37.46}{2}t^2\), and the integral of \(722.47\) is \)722.47t$.
Evaluate the resulting antiderivative at the upper limit \(t=30\) and subtract the value at the lower limit \(t=0\) to find the total volume of water discharged in April.

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Key Concepts

Here are the essential concepts you must grasp in order to answer the question correctly.

Definite Integral as Total Accumulation

The definite integral of a rate function over a time interval gives the total accumulated quantity during that period. In this problem, integrating the discharge rate r1(t) over 30 days calculates the total volume of water flowing through the river in April.
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Interpreting Quadratic Functions

The discharge rates r1(t) and r2(t) are modeled by quadratic functions, which describe how the flow changes over time. Understanding the shape and behavior of these parabolas helps in setting up the integral limits and interpreting the physical meaning of the flow rates.
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Units and Context in Integration

The discharge rates are given in millions of cubic feet per day, and time t is in days. When integrating, it is important to keep track of units to ensure the final result represents the total volume of water in millions of cubic feet over the specified time.
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A culture of bacteria in a Petri dish has an initial population of 1500 cells and grows at a rate (in cells/day) of N′(t) = 100e^−0.25t. Assume t is measured in days.


a. What is the population after 20 days? After 40 days?

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Blood flow A typical human heart pumps 70 mL of blood (the stroke volume) with each beat. Assuming a heart rate of 60 beats/min (1 beat/s), a reasonable model for the outflow rate of the heart is V′(t)=70(1+sin 2πt), where V(t) is the amount of blood (in milliliters) pumped over the interval [0,t],V(0)=0 and t is measured in seconds.


a. Verify that the amount of blood pumped over a one-second interval is 70 mL.

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Textbook Question

Region R is revolved about the line y=1 to form a solid of revolution.


a. What is the radius of a cross section of the solid at a point x in [0, 4]?

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Textbook Question

Consider the region R in the first quadrant bounded by y=x^1/n and y=x^n, where n>1 is a positive number.


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Textbook Question

21–30. {Use of Tech} Arc length by calculator


a. Write and simplify the integral that gives the arc length of the following curves on the given interval. 

y = x³/3, for −1≤x≤1

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For the given regions R₁ and R₂, complete the following steps.


a. Find the area of region R₁.


R₁ is the region in the first quadrant bounded by the y-axis and the curves y=2x^2 and y=3−x; R₂ is the region in the first quadrant bounded by the x-axis and the curves y=2x^2 and y=3−x(see figure).

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