course Phy 202 `q001. If the mass of the ball is m, the before-collision speed of the ball is v and the after-collision speed is v ', then What is the before-collision momentum, and what is the after-collision momentum of the ball? (Be sure to pick a positive direction and use the correct signs in your quantities.)
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We'll worry about the energy questions and the optics this weekend. You have plenty to do right now.
Impulse-Momentum:
The impulse of a force F acting during time interval `dt is F * `dt.
The impulse of the net force F_net acting on a system during time interval `dt is F_net * `dt, and this impulse is equal to the change in momentum m * v of the system. This is the impulse-momentum theorem:
Today's Class:
If you bounce a ball off an analog bathroom scale you can see the scale register several pounds, for a short time. If you were to bounce, say, ten balls off the scale every second (think of 10 people throwing balls at the scale, each with a large supply of balls, with an average of 10 balls being thrown every second), you would be exerting a certain average force on the scale. If people start throwing the balls harder, they will exert a greater average force. A greater number of balls per unit of time will also exert a greater average force. This situation can be analyzed using the impulse-momentum theorem.
We bounced a ball off the scale.
`dp = p_f - p_0 = +.5 kg m/s - (-1.0 kg m/s) = +1.5 kg m/s.
If we had 10 people each throwing one ball downward at the scale every second, the 1-second momentum change would be +15 kg m/s, and the average force (from the impulse-momentum theorem F_ave * `dt = `d(m v) or `dp), we get F_ave = `dp / `dt = +15 kg m/s / (1 s) = +15 kg m/s^2 = +15 N. The scale would be exerting an average force of +15 N on the ball, a bit more than 3 lbs.
When the scale is struck once with the ball its reading can be observed to oscillate between about +20 lb and - 20 lb.
If we were to continue bombarding the scale with 10 impacts every second, each equal to that of the ball used in this model, the scale reading would still oscillate, but it would oscillate about a new 'equilibrium position' corresponding to about 3 lbs of force (3 lbs being the average force exerted by the balls, according to our model).
`q001. If the mass of the ball is m, the before-collision speed of the ball is v and the after-collision speed is v ', then
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We need to begin by choosing a positive direction. Let the positive direction be that of the ball after collision.
Then the before-collision momentum is -m v and the after-collision momentum is + m v '.
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The change in the ball's momentum is
`dp = p_f - p_0 = m v ' - (-m v) = m ( v ' + v ).
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The average force on the ball, by the impulse-momentum theorem, is
F_ave = `dp / `dt = m ( v ' + v ) / `dt.
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We need just divide the average force by the area:
- F_ave / A = (m ( v ' + v) / `dt) / A.
Force / area is average pressure, so we can say that
- P_ave = F_ave / A = (m ( v ' + v) / `dt) / A.
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F_ave = 50 grams * (10 m/s + 20 m/s) / (.1 sec) = .050 kg * 30 m/s / (.1 s) = 15 kg m / s^2 = 15 N.
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P_ave = F_ave / A = (m ( v ' + v) / `dt ) / A = (.050 kg * (10 m/s + 20 m/s) / (.1 s) ) / (.07 m^2) = 15 N / (.07 m^2) = 214 N / m^2, approx.
This can also be expressed as 214 Pa.
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Molecules in a gas, striking a surface, behave in a manner similar to the balls striking the scale. Their velocities are randomly distributed in 3 dimensions so you get 1/3 the force that would be exerted if all were oriented perpendicular to the surface (as was the case for the balls thrown downward at the scale). Because of the randomness of their direction they exert the same pressure on any surface.
`q002. If the directions of the balls striking the scale were random, rather than all being directed downward, what would be the expression for the average force exerted on the scale, in terms of m, v, v ' and `dt? (this question actually neglects some of the finer points of the analysis, but for now we're going to neglect those points)
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P_ave = F_ave / A = (m ( v ' + v) / `dt) / A.
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Consider the piece of tubing, containing some water, passed around the room. You noted that the water level in both sides of the tube remained the same no matter how you changed the positions of the ends of the tube (provided you didn't let water spill, and that you didn't block either end). If you use the tubing like a straw, though, you can easily pull water up toward your mouth, and the levels will no longer be equal. Also, if you were to block one end of the tube with your thumb, you could then achieve different levels by moving one end up or down.
This can be explained by a model similar to that of the balls hitting the scale. The molecules in the air are striking the water surface in each side of the tube. As long as both sides are open to the atmosphere, then during any given time interval (as long as the interval is long enough to ensure a large number of strikes) there will be very nearly equal numbers of strikes, each with the same average momentum change, on both sides. So the average force exerted by the air molecules on the water surface is the same on both sides. (Again we have ignored some details; e.g., air is made up of molecules of different substances, which therefore have different masses. This complicates the analysis a bit, but won't change the conclusions drawn from this simplified model.)
However if you use your mouth to 'pull' water up, as in a straw, you are in fact increasing the volume occupied by the air on one side (you do this using the muscles in your mouth, or your diaphragm, expanding the air cavity in your head and/or lungs).
`q003. If you were to block one end of the tube with your thumb, then raise that end, the net gravitational force on the water in the tube will tend to keep the levels in the two tubes the same. However to keep the water in the raised side at the same level as the water on the other side, the air column trapped inside the tube, between your thumb and the water surface, will have to get longer, increasing the volume of the trapped air.
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The side which remains open to the atmosphere will experience the same force as before.
However if the length of the air column trapped between thumb and water surface increases (which increases the volume of the air), the molecules will have to travel further between collisions with the water surface and the average force they exert will decrease.
More correctly we can say that since the volume increases, fewer molecules are available to hit the water surface within a given time interval `dt, which reduces the force they exert.
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The water in the tube is in equilibrium. More force is exerted on it by the pressure on the open side than on the closed side. To remain in equilibrium, gravity must therefore exert more force on the closed side. So the water level on the closed side will be higher than the level on the open side.
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Suppose you have a long tube, open to the atmosphere, with cross-sectional area 5 cm^2, filled with water. Consider the top 10 cm of water in the tube.
Pressure is force / area. So we see that the pressure required to support our 10-cm column of water is 1000 N / m^2 = 1000 Pa. This result doesn't depend on the cross-sectional area of the tube.
`q004. We generalize the above results, using symbols. We will perform the same operations with the symbols we did in the numerical example above.
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The volume of a column with uniform cross-sectional area A and altitude h is the product of the cross-sectional area and the height:
V = A * h.
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The mass is the product of the volume and the density:
m = rho * V = rho * A * h.
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The weight of mass m is just m g, where g is the acceleration of gravity.
So the weight of the mass m = rho * A * h is
wt = rho * g * A * h.#$&*
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The bottom of the column must exert an upward force equal to the weight of the column, which is rho g A h.
The pressure is the force divided by the area over which that force is applied.
Thus the pressure is
P = rho g A h / A = rho g h.
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When we brought the bottle in from the cold, we estimated that its temperature must have been about 45 Fahrenheit, and we brought it into a room whose temperature was around 68 Fahrenheit.
You are expected to be able to convert Fahrenheit to Celsius, and to know that the freezing point of water at atmospheric pressure is about 272 Celsius degrees above absolute zero. The F to C conversion requires that you know only two things: Water freezes at 0 Celsius and 32 Fahrenheit, and a Celsius degree is 9/5 of a Fahrenheit degree.
For example, 45 Fahrenheit is 13 F above freezing, so it's 5/9 * 13 = 7 Celsius degrees above freezing, which is 7 Celsius. Similarly, 68 F is 36 F above freezing so its 5/9 * 36 = 20 Celsius degrees above freezing. Thus the air inside the bottle warmed from 7 C to 20 C, an increase of about 13 Celsius degrees.
Applying the gas law P V = n R T to this situation:
Rearranging the equation so that the constant terms are all on one side we get P / T = n R / V. Since n, R and V are constant (or nearly so), P / T is constant (or nearly so).
We estimated that this resulted in a water column in the vertical tube, about 30 cm high.
In fact, atmospheric pressure is about 70% higher than this, about 100 000 Pa, but our calculations haven't taken account of all possible factors (for example, the bottle did expand a bit so V didn't really remain constant; and the cool water in the bottle might have kept the temperature of the air a little cooler than that of the room. The 5% figure is rounded off to one significant figure, and is in fact rounded a little high. Our temperature estimates were just that, estimates; we didn't really measure the temperatures).
`q005. In a careful experiment we determine that a water column 50 cm high is supported by a bottle pressure of 1.06 atmosphere--i.e., by a pressure which exceeds atmospheric pressure by about 6%.
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As we saw previously the pressure required to support a column of height h is
P = rho g h.
The density of water is 1000 kg / m^3, so the required pressure is
P = 1000 kg / m^3 * 9.8 m/s^2 *.50 m = 4900 N / m^2 = 4900 Pa.
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If 4900 Pa is .06 of the atmospheric pressure, then using P_atm for atmospheric pressure we have
.06 * P_atm = 4900 Pa so that
P_atm = 4900 Pa / (.06) = 82 000 Pa, approx..
This isn't a bad estimate of the accepted value, which is about 100 000 Pa.
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`q006. If the pressure of a gas is 100 000 Pa, temperature 273 Kelvin and n = 1 mole, then what is the volume of the gas? Note that R = 8.31 Joules / (mole K).
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P V = n R T, so
V = n R T / P = 1 moles * 8.31 Joules / (mol Kelvin) * 273 Kelvin / (100 000 N / m^2) = .022 m^3,
which is equal to about 22 liters.
This is the volume of a mole of gas at STP (standard temperature and pressure), to two significant figures.
Using a more accurate expression for atmospheric pressure we find that the 3-significant-figure volume of a mole at STP is 22.4 liters.
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The same calculation as before, but with the 293 K temperature, would give us a volume of about 23 liters.
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Room temperature was around 290 Kelvin, pressure was about 100 000 Pa. .5 liters is .5 * .001 m^3 = .0005 m^3. So the number of moles would have been
n = P V / (R T) = 100 000 Pa * .0005 m^3 / (8.31 J / (mol K * 290 K) = .02 moles, approximately.
NOTE COMMON ERROR:
100 000 Pa (.5 liters) = n (8.31 J/mole*K) (293K)
20.5353 moles = n
INSTRUCTOR COMMENT: Good solution, but this last calculation doesn't come out in moles.
The units of the given calculation are N / m^2 * liters / ( J / (mole Kelvin) * Kelvin).
The unit 'liter' isn't directly compatible with the SI units of the other quantities:A liter is .001 m^3, and a Joule is a N * m. So our units are
N / m^2 * (.001 m^3) / ( N * m / (mole Kelvin) * Kelvin) =
N / m^2 * (.001 m^3) / ( N * m / mole) =
.001 N * m^3 / (N * m * m^2 * mole) =
.001 mole so your result would be
20.5353 (.001 mole) = .0205 mole.It would probably have been easier to express the liters in moles in the first place, using 10^-3 m^3 instead of liters:
- 100 000 Pa (.5 * 10^-3 m^3) = n (8.31 J/mole*K) (293K)
The numbers and the units would then have worked out as they did in the given solution.
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`q007. A mole of a diatomic gas has a specific heat of 5/2 R = 5/2 * 8.31 Joules / (mole K) = 31 J / (mol K), approximately, when it is heated at constant volume (i.e., in such a way that it can't expand). This means that a mole of gas requires 31 J of energy to raise its temperature by 1 Kelvin degree.
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With .02 moles of gas in the bottle, the energy required to raise temperature of the gas, per degree, is (.02 moles * 31 J / (mole Kelvin) ) = 0.62 J / Kelvin.
Thus the system requires .62 Joules for every Kelvin degree increase in temperature.
To raise the temperature of the system by 13 Kelvin degrees requires energy (0.62 J / Kelvin) * 13 Kelvin = 8 Joules, approx. .
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`q008. A gram of water requires about 4 Joules of energy to raise its temperature 1 degree Celsius.
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The original water has mass 200 grams. So the energy to raise this water, per Celsius degree, is 200 grams * 4 Joules / (gram Celsius) = 800 Joules / Celsius.
The temperature of the original water decreased by 15 Celsius, so the energy change of the water is -15 Celsius * 800 J / Celsius = -12 000 J.
The original water therefore lost about -12 000 J of energy.
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If the system was indeed isolated so that no energy could be exchanged with the surroundings, the loss of 12 000 J by one part of the system is balanced by a gain of 12 000 J by the other part of the system.
So the snow gained 12 000 Joules of energy.
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After melting the snow will be in the form of water, and every gram will gain 4 Joules for every Celsius degree change in temperature.
The temperature of the melted snow increased from 0 C to 10 C, a change of +10 C.
40 grams of water will require 40 grams * 4 J / (gram * C) = 160 J / C, i.e., 160 Joules for every Celsius degree increase in temperature. The 10 C increase will therefore require ( 160 J / C ) * 10 C = 1600 Joules of energy.
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The snow gained 12 000 J of energy, only 1600 J after melting. So it gained the difference 12 000 J - 1600 J = 10 400 J in the melting process.
This is the energy gained by 40 grams of snow. We conclude that the energy per gram is 10 400 J / (40 grams) = 260 J / gram.
This differs by about 25% from the accepted value, which is about 330 J / gram.
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You observed in class the effect of snow melted in water. Give your data, and repeat the analysis outlined in the preceding questions for your data.
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Your reasoning should be equivalent to that in the above series of questions.
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`q009. The bottle you observed contained
about 500 cm^3 of air. The water in the tube extended about 30 cm higher than the water in the bottle. The tube has an inner diameter of 3/16 inch, which is close to 4.5 millimeters.****
A cross section of the water in the tube is a circle whose diameter is 4.5 millimeters.
The cross-sectional area of the tube is pi r^2 = pi * (4.5 mm / 2) ^ 2 = 16 mm^2, approx.. Since there are 10 mm in a cm, a mm^2 is .01 cm^2, so our result is equivalent to .16 cm^2.
A 20 cm section of tubing therefore contains volume 20 cm * .16 cm^2 = 3.2 cm^3 of water.
The air in the bottle has a volume of about 500 cm^3. The 3.2 cm^3 of water in the bottle is 3/500 = .006 as great as the volume of air in the bottle. So the water in the tube has 0.6% (a little more than half of 1%) as much volume as the air in the bottle.
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`q010. When the bottle was brought in from
the cold, the air in the bottle expanded as it warmed up. The bottle also expanded, but by much less than the air, so let's ignore the expansion of the bottle, at least for now. The air wasn't free to expand much, so the pressure in the bottle increased.****
The air expanded by an amount equal to the volume of water in the tube, about 3 cm^3. This is less than a 1% expansion.
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We estimated that the temperature in the bottle increased from about 273 K to about 293 K.
The of the air volume increased from about 500 cm^3 to about 503 cm^3.
The original pressure of the air was about 1 atmosphere.
So in its original state we had
- P_1 V_1 / T_1 = 1 atmosphere * 500 cm^3 / (273 K).= 1.82 atm cm^3 / K.
If P_2, V_2 and T_2 denote the final values of pressure, volume and temperature then, since P V / T is constant, we have
P_2 * V_2 / T_2 = 1.82 atm cm^3 / K. We easily conclude that
- P_2 = 1.82 atm cm^3 / K * (T_2 / V_2) = 1.82 atm cm^3 / K * (293 K) / (503 cm^3) = 1.067 atm.
This means that the pressure inside the bottle exceeded that of the atmosphere by a factor of .067.
Compare this to the result we obtain if we assume volume to be constant. If V and n are constant we conclude that P / T is constant, so
P_2 / T_2 = P_1 / T_1 so that
P_2 = P_1 * T_2 / T_1 = 1 atm * (293 K) / (273 K) = 1 atm * 1.073 = 1.073 atm.
By ignoring the volume change we would estimate the pressure to change by a factor of .073, rather than .067. So considering the volume change due to water entering the tube did make a difference, but not a great difference, in our result.
We can independently determine the pressure change:
A 20 cm column of water requires excess pressure equal to (1000 kg / m^3) * 9.8 m/s^2 * 0.20 m = 2000 N / m^2, or 2000 Pa of excess pressure.
From this we would conclude that the .067 atmosphere increase in pressure was equivalent to a 2000 Pa increase in pressure, so that 1 atmosphere would be about 2000 Pa / (.067 atm) = 300 000 Pa.
Since the accepted value of atmospheric pressure is about 100 000 Pa, we are led to suspect either the accuracy of our data or our ability to control extraneous variables in our setup.
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`q011. Assume that a domino is 1 cm thick and
has mass 20 grams. We start with 10 dominoes, each lying flat on the tabletop, and construct a stack of 10 dominoes on the tabletop.****
One domino has mass 20 grams = .020 kg, so its weight is .020 kg * 9.8 m/s^2 = .2 N, approx..
If we raise a domino by 1 cm the gravitational force, which acts downward, does work `dW_dom_cm = -.2 N * .01 m = .002 Joules on it. So its gravitational PE increases by .002 Joules.
If we raise a domino by 2 cm it's easy to see that the gravitational force does twice as much work, .004 Joules.
To build the stack we have to raise the first domino 1 cm, the second 2 cm, the third 3 cm, etc.. It's easy to see, then, that the PE of the system must in the process of building the stack increase by
- `dPE = .002 J + .004 J + .006 J + .008 J + .010 J + .012 J + .014 J + .016 J + .018 J = .090 J.
A shorter and more efficient calculation is also possible.
The 10 dominoes lying on the tabletop all had centers of mass which were half their thickness, or .5 cm, above the tabletop. When stacked their center of mass was 5 cm above the tabletop. So the center of mass of the 10-domino system increased in vertical position from .5 cm to 5 cm, an increase of 4.5 cm.
The gravitational PE of the stack therefore increased by .2 N * .045 m = .090 J.
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We could calculate the PE increase in making the 3 stacks, then the increase when each stack is added to the preceding stack. The result would be the same.
Since gravity is a conservative force, it doesn't matter how we get from the initial system to the final, the PE will be the same in any case.
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The original stack had a PE relative to the original configuration of .090 J, and no KE. Its total mechanical energy was therefore KE + PE = .090 J.
A stack of 9 dominoes has PE of about .002 J + .004 J + ... + .016 J = .072 J. Alternative the center of mass is at 4.5 cm, which is 4.0 cm above that of the original configuration, from which we conclude that the PE relative to the original system is (9 * .020 kg) * (.040 m) * 9.8 m/s^2 = .072 J.
A single domino moving at 2 m/s has KE of (1/2 * .020 kg * (2 m/s)^2 ) = .040 Kg m^2 / s^2. If that domino is on the tabletop its PE relative to the original configuration is zero.
The total mechanical energy of the second configuration is therefore .072 J + .040 J = .112 J, which is greater than that of the 10 domino stack.
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The KE of the moving domino is (1/2 * .020 kg * (1 m/s)^2 ) = .010 J. The PE of this domino, relative to its original position on the tabletop, is easily found to be .012 J (it wasn't specified so we assume the 6 cm height is relative to its previous position on the tabletop).
So the system as currently configured has PE, relative to the original position, of .072 J + .012 J = .084 J. This is less than the .090 J potential energy of the 10-domino stack. However it also has KE of .010 J, raising its total mechanical energy to .094 J, greater than that of the original stack.
An alternative way to make the comparison:
The difference in PE is due to the change in vertical position #$&*
`q012. Now consider a cylinder with water to
a height of 30 cm, a hole in the side of the cylinder at height 5 cm. Assume that a 1 cm section of the cylinder contains 10 cm^3 of water. We can if we wish think of the water as a stack of 30 disks, each with mass 10 grams.****
The center of mass of the first system is higher than that of the second, so its PE is greater. Nothing is moving in either system so both have zero KE. The first system therefore has the greater mechanical energy.
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If 10 grams of water are removed at the 30 cm height and replaced by water at the 5 cm height, then we have a PE change of -(.010 kg) * ( 9.8 m/s^2) * (.25 m) = -.025 Joules.
A 10 gram mass of water moving at 2 m/s has KE = (1/2 * .010 kg * (2 m/s)^2 ) = .020 Joules.
Relative to the original system, we have a PE loss of -.025 J and a KE gain of .020 J. The total mechanical energy therefore has changed by `dKE + `dPE = .020 J + (-.025 J) = -.005 J.
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As we have seen the potential energy has decreased by .025 J. If the mechanical energy is to remain the same, then the PE loss must be matched by a KE gain of equal magnitude. Thus the 10 gram mass of water, which was originally at rest and therefore had zero KE, now has kinetic energy .025 J.
If we set KE = 1/2 m v^2 and solve for v we obtain v = +-sqrt( 2 KE / m) so to preserve total mechanical energy the water must have velocity
v = +-sqrt( 2 KE / m) = +- sqrt( 2 * .025 J / (.010 kg) ) = +- sqrt( 5 m^2 / s^2) = 2.2 m/s, approx..
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`q013. A plastic bead of mass .4 grams falls
to the floor, hitting the floor at a speed of 5 m/s, then rebounds upward with a speed of 4.5 m/s.****
Choosing up as the positive direction the momentum of the bead changes from .4 g * (-5 m/s) = -20 g m/s = -.020 kg m/s, to .4 g * 4.5 m/s = 18 g m/s = .018 kg m/s
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The momentum change is therefore
`dp = p_f - p_0 = .018 kg m/s - (-.020 kg m/s) = .038 kg m/s.
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`q014. If a particle of mass 3 milligrams
approaches the floor with a downward velocity of 200 m/s, and bounces upward at 200 m/s, then by how much does its momentum change during the collision with the floor?****
Choosing upward as the positive direction, the particles momentum changes from 3 mg * (-200 m/s) = -600 mg m/s = -.0006 kg m/s to 3 mc * 200 m/s = 600 mg m/s = +.0006 kg m/s.
The momentum change is therefore
`dp = p_f - p_0 = .0006 kg m/s - (-.0006 kg m/s) = .0012 kg m/s.
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`q015. A particle of mass 5 milligrams was
bouncing back and forth between two walls separated by 10 cm, moving at 300 m/s when it is between the walls (i.e., except during collisions with the walls).****
From the time the particle collides with the wall, until it again collides with the wall, it has to travel to the other wall and back. The distance is double the distance between the wall, or 20 cm.
At 300 m/s the time required to move 20 cm is `ds / `dt = .20 m / (300 m/s) = .0007 sec, approx..
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Let the direction toward the other wall be positive. Then the momentum of the particle approaching the wall is 5 milligrams * (-300 m/s) = -1500 milligram * m/s, or -.000 0015 kg m/s, or in scientific notation -1.5 * 10^-6 kg m/s. The momentum of the particle after bouncing off the wall is +1.5 * 10^-6 kg m/s.
The change in momentum is therefore
`dp = p_f - p_0 = 3 * 10^-6 kg m/s.
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The 3 * 10^-6 kg m/s momentum change takes place once every .0007 sec, approx., so by the impulse-momentum theorem the approximate average force is
F_ave = `dp / `dt = 3 * 10^-6 kg m/s / (.0007 s) = 4 * 10^-3 kg m^2 / s^2 = .004 Newtons.
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`q016. Using P V = n R T, rearrange the equation so that constant quantities are all on one side, for each of the following situations, and state also which quantities will vary:
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If V and T are constant then we rearrange the equation with V, T and R (the last always being constant) on one side:
P V = n R T. Divide both sides by V to get
P = n R T / V. All constant terms are now on the right-hand side, along with the non-constant quantity n. Dividing both sides by n we get
P / n = R T / V.
Thus the ratio P / n of pressure to number of moles is constant. If one quantity goes up or down, the other must go up or down, respectively, by the same proportion.
This makes sense. If you keep volume and temperature constant and pump in more gas, the pressure should go up in the same proportion as the amount of gas.
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If P and V are constant then we rearrange the equation with P, V and R (the last always being constant) on one side:
P V = n R T. Divide both sides by R to get
P V / R = n * T. All constant terms are now on the left-hand side.
Thus the product n * T of temperature and number of moles is constant. If one of these quantities goes up, the other goes down and vice versa.
This makes sense. If you add gas to a constant-volume container, the only way you can keep pressure constant is to decrease the temperature.
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If P and n are constant then we rearrange the equation with P, n and R (the last always being constant) on one side:
P V = n R T. Divide both sides by P to get
V = n R T / P. All constant terms are now on the right-hand side, along with the non-constant quantity T. Dividing both sides by T we get
V / T = n R / P.
Thus the ratio V / T of volume to temperature is constant. If one quantity goes up or down, the other must go up or down, respectively, by the same proportion.
This makes sense. The only way to increase the temperature while keeping the pressure and number of moles constant is to increase the volume.
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If V and n are constant then we rearrange the equation with V, n and R (the last always being constant) on one side:
P V = n R T. Divide both sides by V to get
P = n R T / V. All constant terms are now on the right-hand side, along with the non-constant quantity T. Dividing both sides by T we get
P / T = n R / V.
Thus the ratio P / T of pressure to temperature is constant. If one quantity goes up or down, the other must go up or down, respectively, by the same proportion.
This makes sense. If we increase the temperature of a fixed quantity of gas, while keeping the volume of the container the same, the pressure goes up.
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