For a brief time in the early universe, the temperature was hot enough to produce large numbers of electron-positron pairs. These pairs then constituted a third type of "background radiation," in addition to the photons and neutrinos (see Figure 7.21). Like neutrinos, electrons and positrons are fermions. Unlike neutrinos, electrons and positrons are known to be massive (ea.ch with the same mass), and each has two independent polarization states. During the time period of interest, the densities of electrons and positrons were approximately equal, so it is a good approximation to set the chemical potentials equal to zero as in Figure 7.21. When the temperature was greater than the electron mass times c2k, the universe was filled with three types of radiation: electrons and positrons (solid arrows); neutrinos (dashed); and photons (wavy). Bathed in this radiation were a few protons and neutrons, roughly one for every billion radiation particles. the previous problem. Recall from special relativity that the energy of a massive particle is ϵ=(pc)2+mc22.

(a) Show that the energy density of electrons and positrons at temperature Tis given by

u(T)=0x2x2+mc2/kT2ex2+mc2/kT2+1dx;whereu(T)=0x2x2+mc2/kT2ex2+mc2/kT2+1dx

(b) Show that u(T)goes to zero when kTmc2, and explain why this is a

reasonable result.

( c) Evaluate u(T)in the limit kTmc2, and compare to the result of the

the previous problem for the neutrino radiation.

(d) Use a computer to calculate and plot u(T)at intermediate temperatures.

(e) Use the method of Problem 7.46, part (d), to show that the free energy

density of the electron-positron radiation is

FV=-16π(kT)4(hc)3f(T);wheref(T)=0x2ln1+e-x2+mc2/kT2dx

Evaluate f(T)in both limits, and use a computer to calculate and plot f(T)at intermediate

temperatures.

(f) Write the entropy of the electron-positron radiation in terms of the functions

uTand f(T). Evaluate the entropy explicitly in the high-T limit.

Short Answer

Expert verified

(a). The energy density of electrons is U=16π(kT)4V(hc)3u(T)

(b). By observing the graph, it can be concluded that the result is reasonable.

(c). The result of the neutrino radiation

U=14π5V(kT)415(hc)3

(d). The plot at intermediate temperatures is

(e). Since, FV=-16π(kT)4(hc)3f(T). Hence, Proved.

(f). The entropy of the electron-positron radiation F=-16πV(kT)4(hc)3f(T).

Step by step solution

01

Part(a) Step 1: Given information

We have to prove that energy density of electron and positrons is given byu(T)=0x2x2+mc2/kT2ex2+mc2/kT2+1dx

02

Part(a) Step 2: Solution

Probability of any single state state to be occupiedn¯FD=1eϵ/kT+1

Total energy equalsU=2·2nxnynzϵn¯FD

Energy of massive particleϵ=(pc)2+mc22

U=4nx,ny,nz(pc)2+mc22e(pc)2+mc22/kT+1

Changing sum to integral U=40π/2dΦ0π/2sin(θ)dθ0n2(pc)2+mc22e(pc)2+mc22/kT+1dn

U=2π0n2(hcn/2L)2+mc22e(hcn/2L)2+mc22/kT+1dn

U=2π2LkThc30x2(xkT)2+mc22e(xkT)2+mc22/kT+1dx

U=16π(kT)4V(hc)3u(T)whereu(T)=0x2x2+mc2/kT2ex2+mc2/kT2+1dx

03

Part(b) Step 1: Given information:

We have to Evaluate :u(T0)=0

04

Part(b)  Step 2: Simplify

u(T)=0x3ex+1dx

0x3ex+1dx=7π4120

U=14π5V(kT)415(hc)3

05

Part(c) Step 1: Given information

We have been given that u(T)=0x2x2+(1/t)2ex2+(1/t)2+1dx

06

Part(c) Step 2:Simplify

To plot the function,we get graph

07

Part(d) Step 1: given information

we have been given thatF=-kTln(Z)

08

Part(d) Step 2: Simplify

F=-4nxnynzkTln1+e-ϵ/kT=-4nx,ny,nzkTln1+e-ϵ/kT

ϵ=(pc)2+mc22

F=-16πV(kT)4(hc)3f(T)

09

Part(e) Step 1:Given information

Se have been given thatF=-kTln1+e-ϵ/kT

10

Part(e) Step 2:Simplify

The spherical coordinator is

F=-4kT0π/2dΦ0π/2sin(θ)dθ0n2ln1+e-ϵ/kTdn

ϵ=(pc)2+mc22

11

Prt(f) Step 1:Given information

We have been thatF=-16πV(kT)4(hc)3f(T)

12

Part(f) Step 2:Simplify

The Helmotz free energy us

S=16πV(kT)3(hc)3(u(T)+f(T))k

S=56π5V(kT)345(hc)3k

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Most popular questions from this chapter

In the text I claimed that the universe was filled with ionised gas until its temperature cooled to about 3000 K. To see why, assume that the universe contains only photons and hydrogen atoms, with a constant ratio of 109 photons per hydrogen atom. Calculate and plot the fraction of atoms that were ionised as a function of temperature, for temperatures between 0 and 6000 K. How does the result change if the ratio of photons to atoms is 108 or 1010? (Hint: Write everything in terms of dimensionless variables such as t = kT/I, where I is the ionisation energy of hydrogen.)

A black hole is a blackbody if ever there was one, so it should emit blackbody radiation, called Hawking radiation. A black hole of mass M has a total energy of Mc2, a surface area of 16πG2M2/c4, and a temperature ofhc3/16π2kGM(as shown in Problem 3.7).

(a) Estimate the typical wavelength of the Hawking radiation emitted by a one-solar-mass (2 x 1030 kg) black hole. Compare your answer to the size of the black hole.

(b) Calculate the total power radiated by a one-solar-mass black hole.

(c) Imagine a black hole in empty space, where it emits radiation but absorbs nothing. As it loses energy, its mass must decrease; one could say it "evaporates." Derive a differential equation for the mass as a function of time, and solve this equation to obtain an expression for the lifetime of a black hole in terms of its initial mass.

(d) Calculate the lifetime of a one-solar-mass black hole, and compare to the estimated age of the known universe (1010 years).

(e) Suppose that a black hole that was created early in the history of the universe finishes evaporating today. What was its initial mass? In what part of the electromagnetic spectrum would most of its radiation have been emitted?

The argument given above for why CvTdoes not depend on the details of the energy levels available to the fermions, so it should also apply to the model considered in Problem 7.16: a gas of fermions trapped in such a way that the energy levels are evenly spaced and non-degenerate.

(a) Show that, in this model, the number of possible system states for a given value of q is equal to the number of distinct ways of writing q as a sum of positive integers. (For example, there are three system states for q = 3, corresponding to the sums 3, 2 + 1, and 1 + 1 + 1. Note that 2 + 1 and 1 + 2 are not counted separately.) This combinatorial function is called the number of unrestricted partitions of q, denoted p(q). For example, p(3) = 3.

(b) By enumerating the partitions explicitly, compute p(7) and p(8).

(c) Make a table of p(q) for values of q up to 100, by either looking up the values in a mathematical reference book, or using a software package that can compute them, or writing your own program to compute them. From this table, compute the entropy, temperature, and heat capacity of this system, using the same methods as in Section 3.3. Plot the heat capacity as a function of temperature, and note that it is approximately linear.

(d) Ramanujan and Hardy (two famous mathematicians) have shown that when q is large, the number of unrestricted partitions of q is given approximately by

p(q)eπ2q343q

Check the accuracy of this formula for q = 10 and for q = 100. Working in this approximation, calculate the entropy, temperature, and heat capacity of this system. Express the heat. capacity as a series in decreasing powers of kT/η, assuming that this ratio is large and keeping the two largest terms. Compare to the numerical results you obtained in part (c). Why is the heat capacity of this system independent of N, unlike that of the three dimensional box of fermions discussed in the text?

The planet Venus is different from the earth in several respects. First, it is only 70% as far from the sun. Second, its thick clouds reflect 77%of all incident sunlight. Finally, its atmosphere is much more opaque to infrared light.

(a) Calculate the solar constant at the location of Venus, and estimate what the average surface temperature of Venus would be if it had no atmosphere and did not reflect any sunlight.

(b) Estimate the surface temperature again, taking the reflectivity of the clouds into account.

(c) The opaqueness of Venus's atmosphere at infrared wavelengths is roughly 70times that of earth's atmosphere. You can therefore model the atmosphere of Venus as 70successive "blankets" of the type considered in the text, with each blanket at a different equilibrium temperature. Use this model to estimate the surface temperature of Venus. (Hint: The temperature of the top layer is what you found in part (b). The next layer down is warmer by a factor of 21/4. The next layer down is warmer by a smaller factor. Keep working your way down until you see the pattern.)

Most spin-1/2 fermions, including electrons and helium-3 atoms, have nonzero magnetic moments. A gas of such particles is therefore paramagnetic. Consider, for example, a gas of free electrons, confined inside a three-dimensional box. The z component of the magnetic moment of each electron is ±µa. In the presence of a magnetic field B pointing in the z direction, each "up" state acquires an additional energy of -μBB, while each "down" state acquires an additional energy of +μBB

(a) Explain why you would expect the magnetization of a degenerate electron gas to be substantially less than that of the electronic paramagnets studied in Chapters 3 and 6, for a given number of particles at a given field strength.

(b) Write down a formula for the density of states of this system in the presence of a magnetic field B, and interpret your formula graphically.

(c) The magnetization of this system is μBN-N, where Nr and N1 are the numbers of electrons with up and down magnetic moments, respectively. Find a formula for the magnetization of this system at T=0, in terms of N, µa, B, and the Fermi energy.

(d) Find the first temperature-dependent correction to your answer to part (c), in the limit TTF. You may assume that μBBkT; this implies that the presence of the magnetic field has negligible effect on the chemical potential μ. (To avoid confusing µB with µ, I suggest using an abbreviation such as o for the quantity µaB.)

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