Mathematical Modelling - What is it?
People study mathematics for many reasons. There are those, like Dr Gavin
Hitchcock, the editor of Zimaths, who believe that mathematics is worth
studying just for its own sake. Generally, this is what most pure
mathematicians believe - that there is a certain beauty about mathematics,
enough reason to spend hours, days, or a life-time, doing mathematics
just for the sake of maths.
My own ideas about mathematics closely resemble those of Richard
Haberman, who is, in my opinion, one of the greatest mathematicians of this
century. For me, the primary reason for studying
mathematics lies in its applications. We study mathematics in order to
apply it. Good mathematics is always applicable, even if we haven't yet
found how it can be applied! Mathematics has been applied to virtually
all facets of life.
The process of applying mathematics to a real life situation is often
referred to as mathematical modelling. A model in this
sense is a simplified, mathematical concept that represents a real life
situation. Mathematical models are developed to help in the understanding
of physical phenomena. Formulating a model usually involves making
observations, collecting data or carrying out an experiment. The
observations made, or the
results of our experiment, are then put in a
mathematical form, together with some assumptions. Often this means
representing our observations or
experimental results by an equation or set of equations involving some
derivatives of one or more unknown functions. Such equations are
called differential equations, and these constitute our
mathematical model. However,
before we can say anything to our friends about our model, we need to
validate the model. To do this usually means solving
the differential equations (it may sometimes be necessary to invent new
mathematics to do this), then interpreting the solution and
testing the predictions of the mathematical model against real-life
situations. In most cases, it is then necessary to modify the initial
model, possibly by removing some of the assumptions made in the
formulation of the initial
model, or applying different mathematical techniques to solve the set of
differential equations that constitute the model.
Mathematical modelling is widely used in industry, commerce and government.
Perhaps what most people might relate to, and what comes readily to mind
when we speak of mathematical modelling, is the process of predicting the
weather in meteorology. In an over-simplified way, this consists of
collecting data on ocean currents, wind directions and speeds, cloud
formations, etc., and putting together a mathematical model to predict
future weather patterns.
Some areas in which mathematical modelling has been successfully
used are: population dynamics (this includes predictions of population
growths and the spread of epidemics, such as the AIDS virus), financial
mathematics (for example, trading in stocks and derivatives),
modelling traffic flow, modelling conflicts (such as political unrests
and wars), etc. (See page 17, where the challenge is to model the
degeneration of roads by potholes.)
Obviously, mathematical modelling is a vast subject. Looking at all the
areas in which it has been applied might require more than the 32 volumes
of the Encyclopedia Brittanica! We will look at two examples of
mathematical models in our attempt to introduce some of the fundamental
concepts to the reader.
The first we will give now, and the second (modelling conflict situations)
we will give in the next issue.
Example: Free fall
Let us consider the case of an object dropped from a
certain height above
the ground and falling under gravity. Newton's second law states that the
acceleration of a particle times its mass equals the total force
acting on it. And Newton's Law of Gravitation states that the force
exerted on a particle of mass m by another particle of mass M is
proportional (by a universal gravitational constant g) to the
product of the masses divided by the square of the distance between
them. These two mathematical equations together constitute a mathematical
model
of the way matter and space are related - and allow us to explain and
predict, to a high degree of accuracy, the behaviour
of both terrestrial projectiles and celestial planets. This grand and
yet stunningly simple synthesis was arrived at by Isaac Newton in the
seventeenth century, ``standing on the
shoulders'' of others before him (like Kepler and Galileo), and based upon
centuries of careful
observation and measurement. How can we use these two laws to arrive at a
reasonable mathematical model
of our falling object?
A non-trivial piece of integration tells us that the attractive force
exerted on a particle by a uniformly dense spherical object is the same as
would be exerted on it were the whole mass of the sphere concentrated at
its centre. Therefore, we assume that both our falling object and
the earth are uniformly dense spheres of masses m and M, with the
former small enough to behave like a particle, and R the radius of the
earth.
Now, let us take the origin O of our axis at the point where the object
is falling from. Let z(t) be the distance from the origin to the centre
of the object at time t, so that the acceleration (measured
downward) of the object is [(d2z)/(dt2)]. Then the
two
laws lead, on our assumptions above, to the two model equations:
|
m |
d2z dt2
|
= F, and F = g |
mM (R+h-z)2
|
|
| (1) |
yielding the single differential equation
In order to simplify the model still more we make one more assumption: that
the height h is very small in comparison with the radius R of the
earth, so that R+h-z » R; and so we obtain, finally, the differential equation we shall use to
model the behaviour of our falling object:
where g = g[mM/(R2)] is called the acceleration of gravity. It
is usually taken to be a constant, although in fact it varies from place to
place on the Earth's surface.
Having obtained the differential equation we now need to
solve it. Dividing by m and integrating with respect to time t leads
to an equation for the velocity v(t) of the object at time t:
You may have met this equation in the form v = u+at. A further integration
then gives an equation for the height of the object at time t:
Clearly, the constants of integration c1 and c2 are the initial
velocity and height of the object. You may have met this equation in
the form s = ut+[1/2]at2. By taking the origin of our axis at the
point where the object is dropped from, this means that c2 is zero.
Notice that you can use equation 5 to measure g in your
classroom. All you need is a stop watch
and a small object which you can drop from the top of a desk. Drop this
object from different heights z and measure the time in seconds it takes
to hit the floor. In each case the initial speed is zero and if you plot a
graph of z against t2, the slope should give you g/2. Compare your
value of g with that from the expression g = (9.80616-0.025928cos2b+0.000069cos22b-0.000003h) ms-2, where b is the latitude
and h is the height above sea-level measured in metres. What are the
values of b and h in Harare, say? If you get an accurate value
for g using this model, then it means that the model must be pretty good.
This in general is how you validate a model, by comparing its predictions
with reality.
However, thinking about the model just developed above, we realize that
there is another factor which is not `true to life'. We have assumed that
the only force acting on the object is that due to gravity. Surely, an
object moving through air (or any other medium for that matter) must be
subject to medium resistance - in this case, air resistance?
Unfortunately, there is no formula that
exactly determines the air resistance acting on the object. We suspect
that the air
resistance may depend on the air density, the velocity of the object and
perhaps even the shape of the object! At this stage in order to make
progress with our model we need to make another assumption. Let us assume
that air resistance is proportional to the velocity (which
means to the number of air particles the object bumps into each second). The
model now becomes:
where k is a positive constant that depends on air density and body
shape. Why have we put a negative sign? Because air resistance opposes the
motion of the object, so the force is upward, in the
opposite direction to the gravitational force and the direction in which
we have measured z, [dz/dt], [(d2z)/(dt2)].
The new model equation can now be solved using a technique called
ßeparation of variables" by first re-writing the equation in the form
and integrating once to obtain
where c is a constant of integration. Let us multiply the last equation by
-k to obtain
Now taking exponentials of both sides and keeping in mind that for any
arbitrary numbers x and y, elnx = x and ex+y = exey, we
obtain the general solution
Let me leave it as an small exercise to show that if we now assume that at
time t = 0, the speed of the particle is v0, equation 8 gives
the formula for the velocity at time t as
|
v = |
mg k
|
+(v0- |
mg k
|
)e-kt/m. |
| (9) |
Notice from equation 9 that when an object has been falling for
a long time (perhaps it is dropped from a high cliff and takes a long
time to reach the ground!), the exponential term e-kt/m becomes
small, in fact, when t® ¥ then e-kt/m® 0. In this case
v = mg/k. In other words when an object has been in free fall fall for a
long time, its velocity is approximately its weight mg divided by k.
This is a constant. This constant mg/k is called the limiting or
terminal velocity of the object.
So, what does our model tell us? It predicts that when dropped from the
same height a heavier object would fall faster than a lighter one (since
the velocity is directly proportional to the weight, mg). In addition,
if somehow we were to reduce air resistance (which is equivalent to
making k small), the model predicts that the object would fall faster.
These predictions are broadly in line with our everyday experiences.
This confirms the validity of our model.
- Dr Precious Sibanda. [Next Issue: Example 2 on modelling
conflict]
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