
Anthony P. answered 12/18/23
PhD in Physical Chemistry
The volume of the atmospheric layer is the volume of a sphere with radius from the earth center to the outer fringes of atmospheric gases, minus the the volume of the earth.
Let Ve = volume of the earth, Re = radius of the earth
Va = volume of the air layer, Da = thickness of the air layer
Vt = volume to the outer fringes Rt = radius of the outer fringes
Then Va = Vt - Ve (1)
Note that the volume of a sphere is (4/3)*pi* R3
Also note that Rt = Re + Da (2)
Thhen from equ(1), Va = (4/3)*pi*Rt3 - (4/3)*pi*Re3
Substituting equ(2) we get Va = (4/3)*pi* (Rt3 - Re3) = (4/3)*pi* [ (Re+Da)3 - Re3 ]
Rather than expanding the sum-cubed, let's put in the numbers.
Va = (4/3)*pi* [ (6400+50)3 - (6400)3 ]
= 1.33*3.14* [ 268.336E9 - 262.144E9 ]
= 1.33*3.14* 6.19E9
Va = 25.9E9 = 25.9 billion km3 (about 6.3 billion cubic miles!)
For the total number of gas molecules in the atmosphere, we start with the Ideal Gas Law:
PV = nRT
n = PV/RT = (0.20 atm)*(25.9E9 km3)*(103 m/km)3 *(102 cm/m)3 *(10-3 L/cm3)
(0.08205 L*atm/degK*mole * 288.15 degK)
(note the change to Kelvin temperature: 15 C = 288.15K)
Doing the arithmetic gives n = 2.19E20 moles
Converting the moles to molecules requires Avogadro's Number:
N = n * NA = 2.19E20 moles * 6.023E23 molecules/mole
N = 13.2 E43 = 1.32 E44 molecules
Calculating the number of gas molecules in Caesar\'s last breath
Again using PV=nRT ,
n(Clb) = PV/RT = (1 atm)*(500 ml)*(10-3 L/ml) / [ (0.08205 L*atm/degK/mole)*(300.15 degK) ]
n(Clb) = 0.0203 moles
N(Clb) = 0.0203 * 6.023E23 = 0.122E23 = 1.22 E22 molecules
The fraction of all air molecules from Caesar's last breath is
F = N(Clb) / N(atm) = 1.22E22 / 1.32E44
F = 0.924 E-22 = 9.24 E-23
About how many molecules from Caesar\'s last breath do you inhale?
Assuming the 500ml breath volume from the Caesar calculation,
N(breath) = 1.22 E22 molecules
N(Caesar in modern breath) = N(C) * F = 1.22 E22 * 9.24 E-23 = 11.3 E-1 = 1.13
= about 1 molecule per breath (weird, huh?)