/*! 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 30 During the 1970 s and 1980 s, th... [FREE SOLUTION] | 91Ó°ÊÓ

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During the 1970 s and 1980 s, the build up of chlorofluorocarbons (CFCs) created a hole in the ozone layer over Antarctica. After the 1987 Montreal Protocol, an agreement to phase out CFC production, the ozone hole has shrunk. The ODGI (ozone depleting gas index) shows the level of CFCs present. \(^{8}\) Let \(O(t)\) be the ODGI for Antarctica in year \(t ;\) then \(O(2000)=95\) and \(O^{\prime}(2000)=\) -1.25. Assuming that the ODGI decreases at a constant rate, estimate when the ozone hole will have recovered, which occurs when ODGI = 0.

Short Answer

Expert verified
The ozone hole is estimated to recover by the year 2076.

Step by step solution

01

Understanding the Problem

We're given the ODGI function \( O(t) \) and know its value and rate of change at the year 2000, which are \( O(2000) = 95 \) and \( O'(2000) = -1.25 \), respectively. We need to find the year when \( O(t) = 0 \).
02

Setup a Linear Equation

Since the ODGI is assumed to decrease at a constant rate, we can express \( O(t) \) as a linear function: \( O(t) = mt + b \), where \( m = O'(2000) = -1.25 \) is the slope, and \( b \) can be found using \( O(2000) = 95 \).
03

Find the Y-Intercept

Plug \( t = 2000 \) into the function \( O(t) = -1.25t + b \) and solve for \( b \) using \( O(2000) = 95 \): \[ 95 = -1.25 \times 2000 + b \]. Calculate to find \( b \).
04

Calculate the Y-Intercept Value

Solving \( 95 = -1.25 \times 2000 + b \) gives:\[ 95 = -2500 + b \]. Solve for \( b \):\[ b = 95 + 2500 = 2595 \]. Thus, the equation is now \( O(t) = -1.25t + 2595 \).
05

Solve for the Recovery Year

To find when the ODGI becomes 0, solve \( O(t) = 0 \):\[ 0 = -1.25t + 2595 \]. Rearrange to find \( t \): \[ 1.25t = 2595 \]. Divide both sides by 1.25 to get \( t \).
06

Calculate the Year

Solving for \( t \):\[ t = \frac{2595}{1.25} = 2076 \]. Thus, the ozone hole is estimated to recover in the year 2076.

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Key Concepts

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

Rate of Change
The concept of rate of change is essential in understanding how variables, like the ODGI or ozone-depleting gas index, evolve over time. In this context, it's all about how fast or slow the ODGI is decreasing over the years.
The rate of change is denoted by the derivative of a function, so in our case, it was given as \( O'(2000) = -1.25 \). This negative value indicates a decrease, meaning the ODGI is reducing by 1.25 units every year.

When we see rate of change in environmental mathematics, it’s often linked with natural phenomena or human-induced processes, where predicting future conditions is crucial.
  • A positive rate means an increase over time.
  • A negative rate, like here, signals a decrease.
  • The specific unit change depends on the context—here it is the yearly reduction of the ODGI.
By knowing the rate of change, we can estimate future values or conditions, which is vital in environmental prediction and planning.
Slope-Intercept Form
The slope-intercept form of a linear equation is a standard way to express straight-line equations. It is written as \( y = mx + b \), where \( m \) is the slope of the line, and \( b \) is the y-intercept. This form helps in quickly identifying the rate of change and starting value of a function.

In our exercise, we have the function \( O(t) = -1.25t + 2595 \). Here:
  • \( m = -1.25 \) (the slope) tells us how steep the line is, showing the ODGI's yearly decline.
  • \( b = 2595 \) (the y-intercept) is the function's starting point when \( t = 0 \), but practically adjusted here for the year 2000 data.
Seeing this form allows one to swiftly plug in values of \( t \) and generate corresponding \( O(t) \). For students, it’s like having a formula you can feed numbers into to see what's happening over time.
This method is particularly helpful not only in mathematics but also in fields like environmental research, where accurately modeling trends helps in taking informed decisions.
Environmental Mathematics
Environmental mathematics involves using mathematical techniques to tackle problems related to the environment. It connects theoretical math with practical environmental issues, like the depletion of the ozone layer.
The case of chlorofluorocarbons (CFCs) and their impact on the ozone layer is a classic example of how environmental policies (like the Montreal Protocol) are governed by mathematical modeling. By modeling the ODGI as a linear function, we can assess how changes in production limits impact ozone recovery.

Some key benefits of using mathematics in environmental science include:
  • Predicting outcomes based on data trends, like when the ozone layer might recover.
  • Simulating scenarios to understand potential impacts of environmental policies.
  • Visualizing complex data in simpler, understandable forms.
Thus, environmental mathematics isn't just about crunching numbers—it's about applying these numbers to predict, prevent, and plan better for environmental and public welfare.

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