Open in App Suggest Corrections 2 By the end of this section, you will be able to:
We have examined pressure and temperature based on their macroscopic definitions. Pressure is the force divided by the area on which the force is exerted, and temperature is measured with a thermometer. We can gain a better understanding of pressure and temperature from the kinetic theory of gases, the theory that relates the macroscopic properties of gases to the motion of the molecules they consist of. First, we make two assumptions about molecules in an ideal gas.
To derive the ideal gas law and the connection between microscopic quantities such as the energy of a typical molecule and macroscopic quantities such as temperature, we analyze a sample of an ideal gas in a rigid container, about which we make two further assumptions:
The collisions between molecules do not appear in the derivation of the ideal gas law. They do not disturb the derivation either, since collisions between molecules moving with random velocities give new random velocities. Furthermore, if the velocities of gas molecules in a container are initially not random and isotropic, molecular collisions are what make them random and isotropic. We make still further assumptions that simplify the calculations but do not affect the result. First, we let the container be a rectangular box. Second, we begin by considering monatomic gases, those whose molecules consist of single atoms, such as helium. Then, we can assume that the atoms have no energy except their translational kinetic energy; for instance, they have neither rotational nor vibrational energy. (Later, we discuss the validity of this assumption for real monatomic gases and dispense with it to consider diatomic and polyatomic gases.) Figure 2.9 shows a collision of a gas molecule with the wall of a container, so that it exerts a force on the wall (by Newton’s third law). These collisions are the source of pressure in a gas. As the number of molecules increases, the number of collisions, and thus the pressure, increases. Similarly, if the average velocity of the molecules is higher, the gas pressure is higher.
In a sample of gas in a container, the randomness of the molecular motion causes the number of collisions of molecules with any part of the wall in a given time to fluctuate. However, because a huge number of molecules collide with the wall in a short time, the number of collisions on the scales of time and space we measure fluctuates by only a tiny, usually unobservable fraction from the average. We can compare this situation to that of a casino, where the outcomes of the bets are random and the casino’s takings fluctuate by the minute and the hour. However, over long times such as a year, the casino’s takings are very close to the averages expected from the odds. A tank of gas has enormously more molecules than a casino has bettors in a year, and the molecules make enormously more collisions in a second than a casino has bets. A calculation of the average force exerted by molecules on the walls of the box leads us to the ideal gas law and to the connection between temperature and molecular kinetic energy. (In fact, we will take two averages: one over time to get the average force exerted by one molecule with a given velocity, and then another average over molecules with different velocities.) This approach was developed by Daniel Bernoulli (1700–1782), who is best known in physics for his work on fluid flow (hydrodynamics). Remarkably, Bernoulli did this work before Dalton established the view of matter as consisting of atoms. Figure 2.10 shows a container full of gas and an expanded view of an elastic collision of a gas molecule with a wall of the container, broken down into components. We have assumed that a molecule is small compared with the separation of molecules in the gas, and that its interaction with other molecules can be ignored. Under these conditions, the ideal gas law is experimentally valid. Because we have also assumed the wall is rigid and the particles are points, the collision is elastic (by conservation of energy—there’s nowhere for a particle’s kinetic energy to go). Therefore, the molecule’s kinetic energy remains constant, and hence, its speed and the magnitude of its momentum remain constant as well. This assumption is not always valid, but the results in the rest of this module are also obtained in models that let the molecules exchange energy and momentum with the wall.
If the molecule’s velocity changes in the x-direction, its momentum changes from −mvx−mvx to +mvx.+mvx. Thus, its change in momentum is Δmv=+mvx−(−mvx)=2mvx.Δmv=+mvx−(−mvx)=2mvx. According to the impulse-momentum theorem given in the chapter on linear momentum and collisions, the force exerted on the ith molecule, where i labels the molecules from 1 to N, is given by Fi=ΔpiΔt=2mvixΔt.Fi=ΔpiΔt=2mvixΔt. (In this equation alone, p represents momentum, not pressure.) There is no force between the wall and the molecule except while the molecule is touching the wall. During the short time of the collision, the force between the molecule and wall is relatively large, but that is not the force we are looking for. We are looking for the average force, so we take ΔtΔt to be the average time between collisions of the given molecule with this wall, which is the time in which we expect to find one collision. Let l represent the length of the box in the x-direction. Then ΔtΔt is the time the molecule would take to go across the box and back, a distance 2l, at a speed of vx.vx. Thus Δt=2l/vx,Δt=2l/vx, and the expression for the force becomes Fi=2mvix2l/vix=mvix2l.Fi=2mvix2l/vix=mvix2l. This force is due to one molecule. To find the total force on the wall, F, we need to add the contributions of all N molecules: F=∑i=1NFi=∑i=1Nmvix2l=ml∑i=1Nvix2.F=∑i=1NFi=∑i=1Nmvix2l=ml∑i=1Nvix2. We now use the definition of the average, which we denote with a bar, to find the force: F=Nml(1N∑i=1Nvix2)=Nmvx2–l.F=Nml(1N∑i=1Nvix2)=Nmvx2–l. We want the force in terms of the speed v, rather than the x-component of the velocity. Note that the total velocity squared is the sum of the squares of its components, so that v2–=vx2–+vy2–+vz2–.v2–=vx2–+vy2–+vz2–. With the assumption of isotropy, the three averages on the right side are equal, so v2–=3vix2–.v2–=3vix2–. Substituting this into the expression for F gives F=Nmv2–3l.F=Nmv2–3l. The pressure is F/A, so we obtain p=FA=Nmv2–3Al=Nmv2–3V,p=FA=Nmv2–3Al=Nmv2–3V, where we used V=AlV=Al for the volume. This gives the important result pV=13Nmv2–.pV=13Nmv2–. Combining this equation with pV=NkBTpV=NkBT gives 13Nmv2–=NkBT.13Nmv2–=NkBT. We can get the average kinetic energy of a molecule, 12mv2–12mv2–, from the left-hand side of the equation by dividing out N and multiplying by 3/2.
The average kinetic energy of a molecule is directly proportional to its absolute temperature: K–=12mv2–=32kBT.K–=12mv2–=32kBT. The equation K–=32kBTK–=32kBT is the average kinetic energy per molecule. Note in particular that nothing in this equation depends on the molecular mass (or any other property) of the gas, the pressure, or anything but the temperature. If samples of helium and xenon gas, with very different molecular masses, are at the same temperature, the molecules have the same average kinetic energy. The internal energy of a thermodynamic system is the sum of the mechanical energies of all of the molecules in it. We can now give an equation for the internal energy of a monatomic ideal gas. In such a gas, the molecules’ only energy is their translational kinetic energy. Therefore, denoting the internal energy by Eint,Eint, we simply have Eint=NK–,Eint=NK–, or Eint=32NkBT.Eint=32NkBT. Often we would like to use this equation in terms of moles: Eint=32nRT.Eint=32nRT. We can solve K–=12mv2–=32kBTK–=12mv2–=32kBT for a typical speed of a molecule in an ideal gas in terms of temperature to determine what is known as the root-mean-square (rms) speed of a molecule.
The root-mean-square (rms) speed of a molecule, or the square root of the average of the square of the speedv2–v2–, is vrms=v2–=3kBTm.vrms=v2–=3kBTm. The rms speed is not the average or the most likely speed of molecules, as we will see in Distribution of Molecular Speeds, but it provides an easily calculated estimate of the molecules’ speed that is related to their kinetic energy. Again we can write this equation in terms of the gas constant R and the molar mass M in kg/mol: We digress for a moment to answer a question that may have occurred to you: When we apply the model to atoms instead of theoretical point particles, does rotational kinetic energy change our results? To answer this question, we have to appeal to quantum mechanics. In quantum mechanics, rotational kinetic energy cannot take on just any value; it’s limited to a discrete set of values, and the smallest value is inversely proportional to the rotational inertia. The rotational inertia of an atom is tiny because almost all of its mass is in the nucleus, which typically has a radius less than 10−14m10−14m. Thus the minimum rotational energy of an atom is much more than 12kBT12kBT for any attainable temperature, and the energy available is not enough to make an atom rotate. We will return to this point when discussing diatomic and polyatomic gases in the next section.
Calculating Kinetic Energy and Speed of a Gas Molecule(a) What is the average kinetic energy of a gas molecule at 20.0ºC20.0ºC (room temperature)? (b) Find the rms speed of a nitrogen molecule (N2)(N2) at this temperature.Strategy(a) The known in the equation for the average kinetic energy is the temperature:K–=12mv2–=32kBT.K–=12mv2–=32kBT. Before substituting values into this equation, we must convert the given temperature into kelvin: T=(20.0+273)K=293K.T=(20.0+273)K=293K. We can find the rms speed of a nitrogen molecule by using the equation vrms=v2–=3kBTm,vrms=v2–=3kBTm, but we must first find the mass of a nitrogen molecule. Obtaining the molar mass of nitrogen N2N2 from the periodic table, we find m=MNA=2(14.0067)×10−3kg/mol)6.02×1023mol-1=4.65×10−26kg.m=MNA=2(14.0067)×10−3kg/mol)6.02×1023mol-1=4.65×10−26kg. Solution
SignificanceNote that the average kinetic energy of the molecule is independent of the type of molecule. The average translational kinetic energy depends only on absolute temperature. The kinetic energy is very small compared to macroscopic energies, so that we do not feel when an air molecule is hitting our skin. On the other hand, it is much greater than the typical difference in gravitational potential energy when a molecule moves from, say, the top to the bottom of a room, so our neglect of gravitation is justified in typical real-world situations. The rms speed of the nitrogen molecule is surprisingly large. These large molecular velocities do not yield macroscopic movement of air, since the molecules move in all directions with equal likelihood. The mean free path (the distance a molecule moves on average between collisions, discussed a bit later in this section) of molecules in air is very small, so the molecules move rapidly but do not get very far in a second. The high value for rms speed is reflected in the speed of sound, which is about 340 m/s at room temperature. The higher the rms speed of air molecules, the faster sound vibrations can be transferred through the air. The speed of sound increases with temperature and is greater in gases with small molecular masses, such as helium (see Figure 2.11).
Calculating Temperature: Escape Velocity of Helium AtomsTo escape Earth’s gravity, an object near the top of the atmosphere (at an altitude of 100 km) must travel away from Earth at 11.1 km/s. This speed is called the escape velocity. At what temperature would helium atoms have an rms speed equal to the escape velocity?StrategyIdentify the knowns and unknowns and determine which equations to use to solve the problem.Solution
SignificanceThis temperature is much higher than atmospheric temperature, which is approximately 250 K (−25°C or−10°F)(−25°C or−10°F) at high elevation. Very few helium atoms are left in the atmosphere, but many were present when the atmosphere was formed, and more are always being created by radioactive decay (see the chapter on nuclear physics). The reason for the loss of helium atoms is that a small number of helium atoms have speeds higher than Earth’s escape velocity even at normal temperatures. The speed of a helium atom changes from one collision to the next, so that at any instant, there is a small but nonzero chance that the atom’s speed is greater than the escape velocity. The chance is high enough that over the lifetime of Earth, almost all the helium atoms that have been in the atmosphere have reached escape velocity at high altitudes and escaped from Earth’s gravitational pull. Heavier molecules, such as oxygen, nitrogen, and water, have smaller rms speeds, and so it is much less likely that any of them will have speeds greater than the escape velocity. In fact, the likelihood is so small that billions of years are required to lose significant amounts of heavier molecules from the atmosphere. Figure 2.12 shows the effect of a lack of an atmosphere on the Moon. Because the gravitational pull of the Moon is much weaker, it has lost almost its entire atmosphere. The atmospheres of Earth and other bodies are compared in this chapter’s exercises.
Check Your Understanding If you consider a very small object, such as a grain of pollen, in a gas, then the number of molecules striking its surface would also be relatively small. Would you expect the grain of pollen to experience any fluctuations in pressure due to statistical fluctuations in the number of gas molecules striking it in a given amount of time? The pressure a gas would create if it occupied the total volume available is called the gas’s partial pressure. If two or more gases are mixed, they will come to thermal equilibrium as a result of collisions between molecules; the process is analogous to heat conduction as described in the chapter on temperature and heat. As we have seen from kinetic theory, when the gases have the same temperature, their molecules have the same average kinetic energy. Thus, each gas obeys the ideal gas law separately and exerts the same pressure on the walls of a container that it would if it were alone. Therefore, in a mixture of gases, the total pressure is the sum of partial pressures of the component gases, assuming ideal gas behavior and no chemical reactions between the components. This law is known as Dalton’s law of partial pressures, after the English scientist John Dalton (1766–1844) who proposed it. Dalton’s law is consistent with the fact that pressures add according to Pascal’s principle. In a mixture of ideal gases in thermal equilibrium, the number of molecules of each gas is proportional to its partial pressure. This result follows from applying the ideal gas law to each in the form p/n=RT/V.p/n=RT/V. Because the right-hand side is the same for any gas at a given temperature in a container of a given volume, the left-hand side is the same as well.
An important application of partial pressure is that, in chemistry, it functions as the concentration of a gas in determining the rate of a reaction. Here, we mention only that the partial pressure of oxygen in a person’s lungs is crucial to life and health. Breathing air that has a partial pressure of oxygen below 0.16 atm can impair coordination and judgment, particularly in people not acclimated to a high elevation. Lower partial pressures of O2O2 have more serious effects; partial pressures below 0.06 atm can be quickly fatal, and permanent damage is likely even if the person is rescued. However, the sensation of needing to breathe, as when holding one’s breath, is caused much more by high concentrations of carbon dioxide in the blood than by low concentrations of oxygen. Thus, if a small room or closet is filled with air having a low concentration of oxygen, perhaps because a leaking cylinder of some compressed gas is stored there, a person will not feel any “choking” sensation and may go into convulsions or lose consciousness without noticing anything wrong. Safety engineers give considerable attention to this danger. Another important application of partial pressure is vapor pressure, which is the partial pressure of a vapor at which it is in equilibrium with the liquid (or solid, in the case of sublimation) phase of the same substance. At any temperature, the partial pressure of the water in the air cannot exceed the vapor pressure of the water at that temperature, because whenever the partial pressure reaches the vapor pressure, water condenses out of the air. Dew is an example of this condensation. The temperature at which condensation occurs for a sample of air is called the dew point. It is easily measured by slowly cooling a metal ball; the dew point is the temperature at which condensation first appears on the ball. The vapor pressures of water at some temperatures of interest for meteorology are given in Table 2.2.
The relative humidity (R.H.) at a temperature T is defined by R.H.=Partial pressure of water vapor atTVapor pressure of water atT×100%.R.H.=Partial pressure of water vapor atTVapor pressure of water atT×100%. A relative humidity of 100%100% means that the partial pressure of water is equal to the vapor pressure; in other words, the air is saturated with water.
Calculating Relative HumidityWhat is the relative humidity when the air temperature is 25ºC25ºC and the dew point is 15ºC15ºC?StrategyWe simply look up the vapor pressure at the given temperature and that at the dew point and find the ratio.SolutionR.H.=Partial pressure of water vapor at15°CPartial pressure of water vapor at25°C×100%=1705Pa3167Pa×100%=53.8%.R.H.=Partial pressure of water vapor at15°CPartial pressure of water vapor at25°C×100%=1705Pa3167Pa×100%=53.8%. SignificanceR.H. is important to our comfort. The value of 53.8%53.8% is within the range of 40%to60%40%to60% recommended for comfort indoors.As noted in the chapter on temperature and heat, the temperature seldom falls below the dew point, because when it reaches the dew point or frost point, water condenses and releases a relatively large amount of latent heat of vaporization. We now consider collisions explicitly. The usual first step (which is all we’ll take) is to calculate the mean free path, λ,λ, the average distance a molecule travels between collisions with other molecules, and the mean free time ττ, the average time between the collisions of a molecule. If we assume all the molecules are spheres with a radius r, then a molecule will collide with another if their centers are within a distance 2r of each other. For a given particle, we say that the area of a circle with that radius, 4πr24πr2, is the “cross-section” for collisions. As the particle moves, it traces a cylinder with that cross-sectional area. The mean free path is the length λλ such that the expected number of other molecules in a cylinder of length λλ and cross-section 4πr24πr2 is 1. If we temporarily ignore the motion of the molecules other than the one we’re looking at, the expected number is the number density of molecules, N/V, times the volume, and the volume is 4πr2λ4πr2λ, so we have (N/V)4πr2λ=1,(N/V)4πr2λ=1, or λ=V4πr2N.λ=V4πr2N. Taking the motion of all the molecules into account makes the calculation much harder, but the only change is a factor of 2.2. The result is λ=V42πr2N.λ=V42πr2N. In an ideal gas, we can substitute V/N=kBT/pV/N=kBT/p to obtain λ=kBT42πr2p.λ=kBT42πr2p. The mean free time ττ is simply the mean free path divided by a typical speed, and the usual choice is the rms speed. Then τ=kBT42πr2pvrms.τ=kBT42πr2pvrms.
Calculating Mean Free TimeFind the mean free time for argon atoms (M=39.9g/mol)(M=39.9g/mol) at a temperature of 0°C0°C and a pressure of 1.00 atm. Take the radius of an argon atom to be 1.70×10−10m.1.70×10−10m.Solution
SignificanceWe can hardly compare this result with our intuition about gas molecules, but it gives us a picture of molecules colliding with extremely high frequency.
Check Your Understanding Which has a longer mean free path, liquid water or water vapor in the air? |