The rms speed of molecules in a gas is given by vrms=√3RT/M, where T is the temperature and M is the molar mass of the gas. The speed required for escape from Earth's gravitational pull is v=√2gre, where g is the acceleration due to gravity at Earth's surface and re(=6.37×106 m) is the radius of Earth. To derive this expression, take the zero of gravitational potential energy to be at infinity. Then, the gravitational potential energy of a particle with mass m at Earth's surface is
U=−GMm/r2e=−mgre,
where g=GM/r2e was used. If v is the speed of the particle, then its original energy is E=−mgre+12mv2. If the particle is just able to travel far away, its kinetic energy must tend toward zero as its distance from Earth becomes large without bound. This means E=0 and v=√2gre. We equate the expressions for the speeds to obtain √3RT/M=√2gre.
The solution for T is T=2greM/3R.
(a)The molar mass of hydrogen is 2.02×10−3 kg/mol, so for that gas
T=2(9.8 m/s2)(6.37×106 m)(2.02×10−3 kg/mol)3(8.31 J/mol.K)=1.0×104 K.
The solution for T is T=2greM/3R.
(b) The molar mass of oxygen is 32.0×10−3 kg/mol, so for that gas
T=2(9.8 m/s2)(6.37×106 m)(3.20×10−3 kg/mol)3(8.31 J/mol.K)=1.6×105 K.
(c) Now, T=2gmrmM/3R, where rm=1.74×106 m is the radius of the Moon and gm=0.16 g is the acceleration due to gravity at the Moon's surface. For hydrogen, the temperature is
T=2(0.16)(9.8 m/s2)(1.74×106 m)(2.02×10−3 kg/mol)3(8.31 J/mol.K)=4.4×102 K.
(d) For oxygen, the temperature is
T=2(0.16)(9.8 m/s2)(1.74×106 m)(32.0×10−3 kg/mol)3(8.31 J/mol.K)=7.0×103 K.
(e) The temperature high in Earth's atmosphere is great enough for a significant number of hydrogen atoms in the tail of the Maxwellian distribution to escape. As a result, the atmosphere is depleted of hydrogen.
(f) On the other hand, very few oxygen atoms escape. So there should be much oxygen high in Earth's upper atmosphere.