CSCI 1210

From the Earth to the Moon

(Lecture notes from  Sept 6-8, 2000)

We now leave the world of baseball and consider the problem of how to travel in space. This is represented as trivial in science fiction movies such as Star Wars and Star Trek, but in the real world it's quite a challenge.
To the best of my knowledge, the first person to propose a physically feasible method of travel to outer space was Jules Verne. In his 1865 novel From the Earth to the Moon, he proposed firing three astronauts and their two dogs from a giant cannon to the Moon.  Interestingly, Verne chose Cape Canaveral, Florida, as his lauch point.
Let's think about how we would model this scenario. It should be clear that this problem has many elements in common with the batted-ball model. There are also the following differences:

Here is how we will deal with these issues:

Gravitation:

Isaac Newton discovered that the strength of the gravitational pull between two objects is inversely proportional to the square of the distance between the centers of the two objects. In equation form  the acceleration of Earth's gravity pulling on an object is

        A = k/Distance^2

where A is the acceleration, Distance is the distance of the object from the center of the Earth, and k is some constant of proportionality. The "caret" operator ^ is used in Excel to represent raising a number to a power. We really don't care about the numerical value of k, but we will solve for it so we can find the acceleration of gravity at any distance above the Earth. We use the known facts that the radius of the Earth is 3960 miles and the acceleration of gravity at the Earth's surface is 32.2 feet per second per second. Thus

    32.2 = k/3960^2

Solving for k we get

    k = 3960^2/32.2

If our projectile is at a distance y miles above the surface of the Earth, then its distance from Earth center is 3960 + y. Putting this back into the equations above we get
 
    A = k/(3960+y)^2

plugging in the value we found for k and doing a little algebra we get

    A = 32.2 * (3960^2)/(3960+y)^2

If you look at this equation you should notice the following reassuring facts:

  1. When y is zero, A will be 32.2
  2. When y is more than zero, A will be less than 32.2.
These observations don't prove that the equation is correct, but if they were't so the equation would definitely be wrong. Note that y must be expressed in miles, since the Earth's radius 3960 is expressed in miles.

Air resistance:

Unlike the simple dependence of gravitation on distance, the air density decreases with altitude in a complex way. Numerous experients involving rockets and airplanes sampling the upper atmosphere have yielded tha following formula for the variation of air density with altitude:

   d = exp(-0.169y)        if y<6,
         1.6 exp (-0.252y) if  6<= y <= 40,
          0                         if y>40

Here the air density d is defined to be 1.00 at Earth's surface, and y is once again the altitude in miles. Exp is the exponential function from mathematics, which we will see in many different contexts during this course. We'll be learning more about the properties of this function shortly, but for now it's enough to know that Exp is one of Excel's many built-in functions.
Air resistance itself is now defined as

    Air resistance = k*d* v^2

where v is the velocity of the projectile, d is the air density as calculated above, and k is another constant of proportionality called the drag coefficient. You must get used to the fact that the symbol k is re-used to represent different constants of proportionality in various contexts. For the current context, we will use the drag coefficient of a typical artillery shell, which is 0.00012.

Implementation details:

How do these considerations affect the way in which we set up our Excel workbook? I have also introduced two more new features of Excel to deal with this model: Now you are in a position to study the  Moonshot workbook itself. Make sure you understand all the formulas in this workbootk!