At a depth in Jupiter's atmosphere where the pressure is 1 bar, what is the mean free path for the molecules given that s = 0.266 nm2 is the composition-weighted average cross-section for H2 and He?
l = (½)½kT /
sp
s = 0.266×10-18 m2
l = 0.707 × 1.381×10-23
J K-1 × 160 K / [ 2.66×10-19 m2
× 105 J m-3 ]
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The standard expression is TV1/c = constant where c =
CV / R. Therefore TfVf1/c = TiVi1/c. DT = Tf - Ti = Ti(Vi / Vf)1/c - Ti = Ti [ (Vi / Vf)1/c - 1 ] |
Use a P,T form of the adiabatic expression or you'll drive yourself crazy.
If we want a p,T adiabatic expression, we can get it by substitution of the
ideal gas expression Vm = RT/p into TV1/c fixed.
TV1/c = T(RT/p)1/c = R1/c T1+(1/c) p-1/c = fixed Since R is fixed regardless, we can fold it into whatever constant "fixed" stands for. Likewise we can raise the entire expression to the cth power and the constant similarly. This means that the expression we seek is
Tc+1 / p = T(CV / R) + 1 / p = TCP
/ R / p = fixed
But it's temperature in which we're interested, so we should rearrange the expression by raising it to the R/CP power to get T p=R/CP is fixed, or Tf pf-R/CP = Ti pi-R/CP or Tf = Ti (pf / pi)R/CP
Tf = 298 K ( 5 bar / 1 bar)8.315 J mol-1 K-1
/ 29.17 J mol-1 K-1
In fact, there are devices made which use sudden adiabatic compression to generate heat high enough to light kindling. Compressional matches. J |
dT = (dT/dp)V dp
+ (dT/dV)p dV
(dT/dV)p
= 1 / (dV/dT)p
= 1 / (aV)
dT = (kT/a) dp + (1/aV) dV
a = (1/V)
(dV/dT)p
=° (1/V) (d[RT/p]/dT)p
= (1/V) R/p = R/pV = 1/T
dT =° (T/p) dp + (T/V) dV = T d(ln p) + T d(ln V)
Integrating either partial alone gives ln(Tf / Ti) = ln(pf / pi) or Tf / T i = pf / pi or T / p fixed at fixed V. ln(Tf / Ti) = ln(Vf / Vi) or Tf / Ti = Vf / Vi or T / V fixed at fixed p. |
Molecule | CH4(g) | O2(g) | CO2(g) | H2O(liq) |
DfHq, kJ/mol | - 74.81 | 0.00 | - 393.51 | - 285.83 |
nH2O = 1 kg × (1 mol H2O / 0.018 kg) = 55.5 mol
DH = nCPDT +
nDvapH
CH4 + 2 O2
CO2 + 2 H2O
Thus, we need nCH4 = 2570/890.36 = 2.886 mol
V = nRT/p
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(p + a/V2)(V - b) = RT if we interpret V as Vm.
Z = pV/RT at 1 atm and 373 K requires knowledge of V. V = b + RT/(p + a/V2) solve by successive approximations.
The first guess should be
V = 0.1154 L + 30.61 L atm / (1 + 18.24/V2) atm
Z = pV/RT = 1 atm (30.12 L) / 30.61 atm L = 0.984 |