Chlorine monoxide accumulates in the stratosphere above Antarctica each winter and plays a key role in the formation of the ozone hole above the South Pole each spring. Eventually, ClO decomposes according to the equation: 2C10(g) Cl, (g) + 0,(g) The second-order rate constant for the decomposition of CIO is 7.38×10° M-1s-1 at a particular temperature. Determine the half-life of CIO when its initial concentration is 1.16x10-8 M.

Chemistry: The Molecular Science
5th Edition
ISBN:9781285199047
Author:John W. Moore, Conrad L. Stanitski
Publisher:John W. Moore, Conrad L. Stanitski
Chapter11: Chemical Kinetics: Rates Of Reactions
Section11.5: Temperature And Reaction Rate: The Arrhenius Equation
Problem 11.9E: The frequency factor A is 6.31 108 L mol1 s1 and the activation energy is 10. kJ/mol for the...
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Chlorine monoxide accumulates in the stratosphere above Antarctica each winter and plays a key role in the formation of the ozone
hole above the South Pole each spring. Eventually, CIO decomposes according to the equation:
2C10(g) -
→ Cl, (g) + 0, (g)
The second-order rate constant for the decomposition of CIO is 7.38×10°M-1s-1 at a particular temperature. Determine the half-life of
CIO when its initial concentration is 1.16x10-8 M.
S
Transcribed Image Text:Chlorine monoxide accumulates in the stratosphere above Antarctica each winter and plays a key role in the formation of the ozone hole above the South Pole each spring. Eventually, CIO decomposes according to the equation: 2C10(g) - → Cl, (g) + 0, (g) The second-order rate constant for the decomposition of CIO is 7.38×10°M-1s-1 at a particular temperature. Determine the half-life of CIO when its initial concentration is 1.16x10-8 M. S
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