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Subsections
The purpose of this lab is to use Maple to study applications of
exponential and logarithmic functions. These are used to model many
types of growth and decay, as
well as in many scales, such as the Richter and decibel scales.
The simplest model for growth is
exponential, where
it is assumed that
y'(t) is proportional to y. That is,

Separating the variables and integrating (see section 4.4 of the text),
we have

so that

(If y is a positive quantity, we may drop the absolute value signs
around y.) Solving for y
y = ekt + C
which we may write in the form y = Aekt, where A is an arbitrary
positive constant.
In a sample of a radioactive material, the
rate at which atoms decay is proportional to the amount of material present.
That is,

where k>0 is a constant. This is the same equation as in exponential growth,
except that -k replaces k. The solution is
A(t) = A0 e-kt
where A0 is a positive constant. Physically, A0 is the amount of
material present at t=0.
Radioactivity is often expressed in terms of an element's half-life.
For example, the half-life of carbon-14 is 5730 years. This statement means
that for any given sample of
, after 5730 years, half of it
will have undergone decay.
So, if the half-life is of an element Z is c years, it must be
that
, so that
and
.
What is usually called Newton's law of cooling is a simple model for
the change in temperature of an object that is in contact with an
environment at a different temperature. It says that the rate of
change of the temperature of an object is proportional to the
difference between the object's temperature and the temperature of the
environment. Mathematically, this can be expressed as the differential
equation

where k is the constant of proportionality and
is
the temperature of the environment. Using a technique called
separation of variables it isn't hard to derive the solution

where T0 is the temperature of the object at t=0.
The main functions you need are the natural exponential and
natural logarithm. The Maple commands for these functions are
exp and ln. Here are a few examples.
> f := x -> exp(-2*x);
> simplify(ln(3)+ln(9));
> ln(exp(x));
> simplify(ln(exp(x)));
> solve(exp(-3*x)=0.5,x);
> plot(log[10](x),x=0..100);
- 1.
- Exponential growth can be used to model the growth of certain
kind of investments. Suppose that the value I of an investment
satisfies the differential equation

where r is the interest rate. If
and
you start with an
investment of $10,000 dollars, how many years does it take for the
value to double? How many years does it take to quadruple? Is there an
easy way to answer the second part of this question? Explain.
- 2.
- In 1935 Charles F. Richter of Cal Tech developed a scale for
measuring the magnitude of earthquakes. The Richter Scale formula is
given by

where M is the magnitude of the earthquake, x is the amplitude of
the largest seismic wave as measured on a standard seismograph 100
kilometers from the epicenter
and c is the amplitude of a reference earthquake of amplitude 1
micron ( 1 micron is 0.001 mm) on a standard seismograph at the same
distance from the epicenter.
- (a)
- When the amplitude of an earthquake is doubled, by how much does
the magnitude increase?
- (b)
- The largest earthquake magnitude ever measured was 8.9 for an
earthquake in Japan in 1933. Determine the ratio of the amplitude of
this earthquake to that of the 1906 San Francisco earthquake, which
measured 8.3.
- 3.
- Suppose that the last bit of ice in a picnic cooler has
melted. How long will it take for the temperature inside to reach
? Use Newton's law of cooling to model this, using
,
and
.
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Up: Labs and Projects for
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Jane E Bouchard
11/30/1999