PlanetPhysics/Penny Falling From Empire State Building

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A Penny's Journey

As an example of constant [[../Acceleration/|acceleration]], we will analyze a penny falling from the roof of the Empire State Building. Hopefully, any worries one might have of being killed by a falling penny as they stroll by tall buildings in New York will be quelled. After all, people are usually not injured by hail falling from the clouds.

We will apply [[../NewtonsLaws/|Newton's laws of motion]] to two cases. At first we will neglect air [[../Conduction/|resistance]] (drag) so we can solve the problem analytically. Then we will use a simple model of drag to show how the penny reaches a terminal [[../Velocity/|velocity]] and how this dramatically affects the impact velocity of the penny on the ground.

Free Fall Acceleration

When the only force acting on a body as it falls toward another body, similar to an apple falling to the Earth, is gravity then we say the body is in free fall. The only way we can do this is if we neglet things like drag caused by the atmosphere, wind or variations in [[../GravitationalField/|The Gravitational Field]]. This situation is depicted in Figure 1, where the force due to gravity is

F=mg

\includegraphics[scale=1]{FreeFallAcceleration.eps}

{\mathbf Figure 1:} Penny falling from Empire State Building

The two things we want to calculate is the velocity of the penny when it impacts the ground and the time it takes the penny to fall. Applying Newton's second law to the penny

F=ma

yields the acceleration of the penny in the y direction

a(t)=Fm=mgm=g.

Notice that the minus sign comes from the coordinate [[../SimilarityAndAnalogousSystemsDynamicAdjointnessAndTopologicalEquivalence/|system]] choice with the y axis pointing up. Next, integrate the acceleration equation to get the velocity of the penny at a given time. Remember that the acceleration is defined as

a=dvdt.

This leads to the integration setup of

dv=gdt.

Integrate to get

v(t)=gt+C.

The constant is found using initial conditions, so at t=0, the velocity of the penny is zero

v(0)=0=g(0)+C.

This is only true if C is also zero, therefore the velocity equation is

v(t)=gt

Well, this is great, we can find the velocity at any given time. However, we do not know the time of the impact. For this we must integrate (1) to get the [[../Position/|position]] of the penny. Remember, that velocity is defined as

v=dxdt

This leads to the integration setup of

dx=gtdt.

Integrate to get

x(t)=12gt2+C.

Once again, the constant is found from the initial condition, at t=0, x(0)=h. Therefore, the position equation is

x(t)=12gt2+h

What we want is the time of impact. This happens when x=0. So solve (2) for t.

0=12gtf2+h.

Rearrange to get

tf=2hg

Evaluate (3), using the value g=9.8, to get

tf=(2)*(381)9.8 tf=8.82[s].

Finally, we get the velocity at impact by substituting (3) into (1)

v(tf)=g2hg.

Bringing g under the [[../PiecewiseLinear/|square]] root to get

v(tf)=2hg.

This evaluates to

v(tf)=2*381*9.8=86.42[m/s].

In english units, the velocity is

v(tf)=193.3[mi/hr].

This is fairly fast for a penny, however this does not come very close to the actual [[../Velocity/|speed]] because for such a large height, air resistance will become a big factor. In the next [[../IsomorphicObjectsUnderAnIsomorphism/|section]] we will model air resistance to capture this effect.

Resist the Penny

Since the penny is traveling through the atmosphere (a fluid), we need to use some basic results from fluid [[../Mechanics/|mechanics]] to model the [[../CoriolisEffect/|drag force]] acting on the penny. A simple model combined with experimental data results in the drag expression

Fd=12CdρAv2

where Cd is the drag coefficient of the penny. It is an experimantly derived value and here we will use the value given by [1],

Cd=1.17.

The drag force is in the opposite direction of the velocity [[../Vectors/|vector]] as shown in the free body [[../Commutativity/|diagram]] in Figure 2.

\includegraphics[scale=1]{FreeBodyDiagram.eps}

{\mathbf Figure 2:} Free Body Diagram

The density we will use is the standard day value at sea level given in the tables from [2],

ρ=1.225[kg/m2]

Next A, is the effective cross-sectional area of the penny, From Wikipedia [3], the diameter of the US penny is

D=19.05[mm]=1.905×102[m]

So the cross-sectional area is then

A=πr2=πD24=0.000286m2

Combining all these constants gives us the drag force that is proportional to the square of the velocity

Fd=0.0002v2.

Now we have 2 forces to use with Newton's second law, this gives the acceleration equation as

a(t)=0.0002v2mg

The integral setup is then

dv=0.0002v2mdtgdt.

Unlike the free fall example, the analytical solution is a litte more difficult. However, all is not lost. We will first turn to numerical methods such as Euler's method or numerical [[../SupercomputerArchitercture/|programs]] such as Matlab, Octave or Maple and then later compare with analytical solution (coming soon). Here we will solve the [[../DifferentialEquations/|differential equation]] using Octave [4]. First a little setup must be done to use Octave's lsode solver. The differential equation of [[../CosmologicalConstant2/|motion]] that we will solve with the [[../Mass/|mass]] of the penny, m=2.5×103[kg] [3]

d2xdt2=0.0817(dxdt)29.8

We cannot use a 2nd order differential equation in lsode, so we must use two 1st order equations. This is done by using two states, one for position and another for velocity. Then our equations of motion become

y˙=y˙ y¨=0.0817y˙29.8

The commands in octave are

t = linespace(0, 100, 10000);

y = lsode("penny", [381 0], t);

The [[../Bijective/|function]] "penny" passed to lsode is here. The results are displayed in Figure 3, Figure 4 and Figure 5.

\includegraphics[scale=1]{figure1.eps}

{\mathbf Figure 3:} Penny's Velocity

Note how the max velocity is now a measly 10.952[m/s] and that it stays constant for quite awhile up until impact. This is because the penny reaches what is called terminal velocity where the upward drag force at the terminal velocity cancels out the gravitational force,

0.0817vt2=g vt=g0.0817=10.952[m/s].

Figure 2 is a plot of the position and upon further inspection we see impact occurs at

tf=35.36[s]

and the impact velocity is the terminal velocity

v(tf)=10.952[m/s].

\includegraphics[scale=1]{figure2.eps}

{\mathbf Figure 4:} Penny's Position

Finally, we will zoom in on the first few seconds of the fall to see the position before terminal velocity is reached.

\includegraphics[scale=1]{figure3.eps}

{\mathbf Figure 5:} First Few Seconds

So to wrap things up, we see that air resistance makes a dramatic difference in the maximum velocity of the penny and the time of impact. In reality, the motion is a little more complicated due to winds and the fact that the penny will tumble, but understanding how a falling [[../TrivialGroupoid/|object]] reaches terminal velocity is something to take away. For a more detailed analysis of chaotic [[../MathematicalFoundationsOfQuantumTheories/|dynamics]] of disks, see [6]

All Sources

[1] [2] [3] [4] [5] [6]

References

  1. Yoon, Joe, Scott, Jeff, Gravity, Acceleration \& Speed . Aerisoaceweb
  2. Andersonn, John, Fundamentals of Aerodynamics . 4th Edition. McGraw-Hill, New York, 2007.
  3. Wikipedia, Cent
  4. Octave, [ http://www.gnu.org/software/octave/ GNU Octave]
  5. Halliday, D., Resnick, R., Walker, J. Fundamentals of Physics . 5th Edition. John Wiley \& Sons, New York, 1997.
  6. Stuart B. Field, M. Klaus, M. G. Moore, Franco Nori Chaotic dynamics of falling disks . Nature 388, 252-254, 17 July 1997.

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