F=1.01325×105 N
= Mg = M×9.80665 m s-2 (where N = J/m = kg m s-2)
M = 1.033×104 kg (!)
n = M/MW = 1.033×104 kg / 0.02898 kg mol-1
V = nRT/P
V = Ah = 1 m2 h = 7991 m3
|
MW = 0.01(39.95) + 0.05(18.016) + 0.20(32.00) + 0.74(28.02)
= 28.44 g/mol vHe / vair = [ MWair / MWHe ]½ = [28.44/4.003]½ = 2.665 Since vHe > vair by a long shot, the He effuses into the bubble 2.7× faster than the air effuses out. So the bubble initially inflates. |
THe = (98.6-32)×(5/9)
+ 273.16 = 310 K
r = m/V = (n/V)MW = (P/RT)MW = (P/R)(MW/T)
(MWair / MWHe) = 28.44/4.003 = 7.1 so
Tair = 7.1×310 K = 2200 K (!) The bubble can't survive. |
[Bonus: at that new T for the super-bubble, what would the new effusion rate ratio (warm He vs. hot air) become?]
½mv2 = KE = (3/2)RT
v = [(3R/2)(T/m)]½ (vHe / vair) = [(THe/Tair)×(MWair/MWHe)]½ But the ratio of T's is the same as the ratio of MW's. So (vHe/vair)=1. |
Because if you don't breathe, your lungs will rupture just after your eardrums do. At 100 feet down, there's not 1 atm of air in your lungs but rather four atmospheres, the extra 3 due to 3×33 feet, each one the equivalent of an atmosphere since 33 feet of 1 g/cc density is equivalent in mass to 760 mm of 13.6 g/cc (Hg) density. So as you ascend, your lungs will expand under the reducing pressure, and you must let that extra air out to keep your lungs at their same volume! |
rmossy Al
= 0.8×2.702 = 2.16 g/cc = m/V = MW/Vmolar nAl=1
Vmolar = MW/r = 26.98 g/mol / 2.16 g/cc = 12.48 cc/mol = 1.248×10-2 L
nH2 = ½ nAl = ½
|
nO2 = ½ nMg = ½ mMg/MWMg
VO2 = nRT/P
Vair = VO2 / XO2 = 4610 L / 0.21 = 21,950 L |
Comments to Chris Parr | Return to CHM 1316 HomePage | Last modified 15 February 1999. |