Using data from Appendix 4, calculate ∆H°, ∆G°, and K (at 298 K) for the production of ozone from oxygen: 3 O 2 ( g ) ⇌ 2 O 3 ( g ) At 30 km above the surface of the earth, the temperature is about 230. K and the partial pressure of oxygen is about 1.0 × 10 −3 atm. Estimate the partial pressure of ozone in equilibrium with oxygen at 30 km above the earth's surface. Is it reasonable to assume that the equilibrium between oxygen and ozone is maintained under these conditions? Explain.
Using data from Appendix 4, calculate ∆H°, ∆G°, and K (at 298 K) for the production of ozone from oxygen: 3 O 2 ( g ) ⇌ 2 O 3 ( g ) At 30 km above the surface of the earth, the temperature is about 230. K and the partial pressure of oxygen is about 1.0 × 10 −3 atm. Estimate the partial pressure of ozone in equilibrium with oxygen at 30 km above the earth's surface. Is it reasonable to assume that the equilibrium between oxygen and ozone is maintained under these conditions? Explain.
Solution Summary: The author explains that the partial pressure of ozone is estimated to be in equilibrium with oxygen at 30 km above the Earth's surface.
Using data from Appendix 4, calculate ∆H°, ∆G°, and K (at 298 K) for the production of ozone from oxygen:
3
O
2
(
g
)
⇌
2
O
3
(
g
)
At 30 km above the surface of the earth, the temperature is about 230. K and the partial pressure of oxygen is about 1.0 × 10−3 atm. Estimate the partial pressure of ozone in equilibrium with oxygen at 30 km above the earth's surface. Is it reasonable to assume that the equilibrium between oxygen and ozone is maintained under these conditions? Explain.
The table includes macrostates characterized by 4 energy levels (&) that are
equally spaced but with different degrees of occupation.
a) Calculate the energy of all the macrostates (in joules). See if they all have
the same energy and number of particles.
b) Calculate the macrostate that is most likely to exist. For this macrostate,
show that the population of the levels is consistent with the Boltzmann
distribution.
macrostate 1 macrostate 2 macrostate 3
ε/k (K) Populations
Populations
Populations
300
5
3
4
200
7
9
8
100
15
17
16
0
33
31
32
DATO: k = 1,38×10-23 J K-1
Don't used Ai solution
In an experiment, the viscosity of water was measured at different
temperatures and the table was constructed from the data obtained.
a) Calculate the activation energy of viscous flow (kJ/mol).
b) Calculate the viscosity at 30°C.
T/°C
0
20
40
60
80
η/cpoise 1,972 1,005 0,656 0,469 0,356
Applications and Investigations in Earth Science (9th Edition)
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