16.12* The dimerization of CIO in the Antarctic winter stratosphere is believed to play an important part in that region's severe seasonal depletion of ozone. The following equilibrium constants are based on measurements on the reaction 2 CIO(g) →(CIO),(g). 268| 4.13 x 10° 5.00 × 10 1.45 x 107 5.37 x 10° 3.20 x 10° 9.62 x 105 T/K 233 248 258 273 280 K T/K 288 295 303 K 4.28 x 10 1.67 x 10° 6.02 x 10° (a) Derive the values of A,H and A,S° for this reaction. (b) Compute the standard enthalpy of formation and the standard molar entropy of (CIO), given AH°(CIO,g) = +101.8 kJ mol¯and S(CIO,g) = 226.6 J K' mol"'.

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16.12* The dimerization of CIO in the Antarctic winter stratosphere is believed
to play an important part in that region's severe seasonal depletion of ozone.
The following equilibrium constants are based on measurements on the
reaction 2 CIO(g) →(CIO),(g).
268|
4.13 x 10° 5.00 × 10 1.45 x 107 5.37 x 10° 3.20 x 10° 9.62 x 105
T/K 233
248
258
273
280
K
T/K 288
295
303
K
4.28 x 10 1.67 x 10° 6.02 x 10°
(a) Derive the values of A,H and A,S° for this reaction. (b) Compute the
standard enthalpy of formation and the standard molar entropy of (CIO),
given AH°(CIO,g) = +101.8 kJ mol¯and S(CIO,g) = 226.6 J K' mol"'.
Transcribed Image Text:16.12* The dimerization of CIO in the Antarctic winter stratosphere is believed to play an important part in that region's severe seasonal depletion of ozone. The following equilibrium constants are based on measurements on the reaction 2 CIO(g) →(CIO),(g). 268| 4.13 x 10° 5.00 × 10 1.45 x 107 5.37 x 10° 3.20 x 10° 9.62 x 105 T/K 233 248 258 273 280 K T/K 288 295 303 K 4.28 x 10 1.67 x 10° 6.02 x 10° (a) Derive the values of A,H and A,S° for this reaction. (b) Compute the standard enthalpy of formation and the standard molar entropy of (CIO), given AH°(CIO,g) = +101.8 kJ mol¯and S(CIO,g) = 226.6 J K' mol"'.
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