Physics on the Back of an Envelope

Why you should take this course!


Physics 309 Spring 2003
Room 202 OCNPS, W 10-11
L. Weinstein
683 5803
Room 217 Oceanography and Physics Building
Room 104 Nuclear and Particle Research Facility, 1021 W 47th St, Norfolk, VA 23529
Office Hours: Wed 11-12 Learning Center and Friday 10-11, OCNPS 217
weinstei@physics.odu.edu

Physicists should be able to estimate the order-of-magnitude of anything. How many atoms of Julius Caesar do you
eat every day? How much waste does a nuclear power plant generate? This 1 credit course will develop concepts,
relations and numbers useful for estimation. We will discuss the concepts as a group and attack the problems as a
group. I intend to lecture as little as possible. The course will not cover new material but will make use of already
acquired (or at least already taught) knowledge. It will try to help students apply physics to real-life questions and
understand which physical effects are appropriate on which scales. The corequisite is Physics 232.

Here is the master list of questions

FINAL EXAM: MONDAY MAY 5, 8:30-11:30, OCNPS 202

Sample final available here

NEWS and Homework:

Midterm Wednesday March 5.

Sample midterms are here and hereThere will be no calculators or crib sheets or other external aids allowed on the test.

The antiwar protest in New York City on Feb 15 was estimated at between 1 and 4*10^5 people.  If the protests filled 1st Avenue for 20 blocks, how many people were there?  There are 20 NYC blocks per mile and 1st Avenue is about 6 lanes wide.  Some party-poopers actually counted the crowd in San Francisco:  see this link

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Homework due Jan 22:  #3 (popcorn), #8 (speed of hair), #13 (human crowding).  On #13, please compare the area you get to the total area of Virginia Beach.

Homework due Jan 29:  #6 (cells), 31 (portapotties), 32 (fuel cost)

Homework due Feb 5:  42 (mass of moon) and 53 (1 km asteroid)
Notes on homework: #42: We determined in class that the angular size of the moon is the same as your finger held out at arm's length (or about 1 cm at a distance of 1 m).  From this we know that the moon's diameter is 1 cm / 1m = 1% of the distance from here to the moon (which is 1/4 million miles or 400,000 km).  Please estimate the mass of the moon from its diameter.  The density of water is 1000 kg/m^3.

#53: We determined in class that a reasonable speed for an asteroid is a) the speed of a rock falling from infinity in the Earth's g field (where escape velocity is 11 km/s) or b) the speed of a rock falling from infinity in the Sun's g field (where escape velocity is sqrt(2) times larger than the Earth's orbital speed around the Sun.  Since (b) is larger, use that.   To get the insolation of the Earth, you need the solar constant (solar radiation flux) at Earth orbit which is about 1 kW/m^2. 1 megaton of TNT is about 10^15 J (we will derive that later).

Homework due Feb 12: #43, #48, #57

Homework due Feb 19:  #57, #61
For problem 57, "how big an impact is needed to break the moon in two? to break Phobos in
2?" has been better defined. Use the mass of Phobos = 1*10^16 kg. Assume
that Phobos consists of 2 touching spheres, each with half of the total
mass. Use the density of rock (rho_rock = 3*rho_water). Find the energy
needed to separate the two spheres to infinity (with zero kinetic energy).
Now find the size of asteroid that has that much kinetic energy.  Since we
determined in a previous problem that a 1 km^3 asteroid has a kinetic energy of
KE = 1/2 * 10^9 m^3 * 3000 kg/m^3 * (3*10^4 m/s)^2 = 1.5*10^21 J,
we can use 10^21 J/km^3 as the kinetic energy density of a typical
asteroid.  Make a reasonable assumption for the conversion
efficiency of asteroid kinetic energy to gravitational potential
energy (ie: to splitting the Moon or Phobos).  Therefore, to answer the
question "How large an impact", I want the answer in terms of the size of
the asteroid needed to hit it, ie: in km^3.  Then do the same thing for
the moon.

 For problem 61, you can use 1 cm/yr for your velocity.

Homework due Feb 26: 85, 96, 106

For #85, you can use the solar constant of 1000 W/m^2  at Earth orbit (ie: at 1.5*10^8 km from the sun).  Alternatively, you can use the Stephan-Boltzmann law with a surface temperature of about 5500 K.

For #96, you can use our total energy input from food or you can calculate our energy output from various forms of heat transfer.

For #106, use the energy output calculated in #96.  Assume that the only form of heat output you have is perspiration (since if the ambient temperature is 98.6 F, conduction, convection and radiation are all useless).

Note that there is a discussion of this at  http://quiz.thphy.uni-duesseldorf.de/98/A08.98.html
(This is a great physics problem web site:  http://quiz.thphy.uni-duesseldorf.de)

March 3: Midterm Exam.  No homework due.  Please let me know which homework problems you want for March 17.  If you don't choose some, I will.

Important numbers to be memorized for the exam:
R_earth = 6*10^6 m
d_earth-sun = 1.5*10^11 m
d_earth-moon = 4*10^8 m
G = 7*10^(-11) N-m^2/kg^2
density of water = 1000 kg/m^3
1 year = pi * 10^7 s
avogadro's number = N_A = 6*10^23
1 e = 1.6*10^(-19) Coulombs
molecular binding energy = 1.5 V
cell size = 5 * 10 ^(-6) m
atom size = 10^(-10) m

Note that the atom size can be derived from Avogadro's number and the density of water.

Your grade in the class will depend partially on homework and class participation.   Please do both!



Useful numbers:



Last modified: Wed Jan 7 13:23:49 EST 2003