Over the past several years, the atmospheric ozone concentration over Antarctica has decreased during the winter. The reaction that causes this is shown below: NO(g)+O3(g)⟶NO2(g)+O2(g) Using the data obtained at 100 degree Celsius, determine the rate law for this process: Trial [NONO] [O3O3 ] Rate 1 1.00x10−61.00x10^-6 3.00x10−63.00x10^-6 6.60x10−56.60x10^-5 2 1.00x10−61.00x10^-6 6.00x10−66.00x10^-6 1.32x10−41.32x10^-4 3 1.00x10−61.00x10^-6 9.00x10−69.00x10^-6 1.98x10−41.98x10^-4 4 3.00x10−63.00x10^-6 9.00x10−69.00x10^-6 1.78x10−31.78x10^-3 None of these. rate=k[NO] rate=k[NO][O3] rate=k[NO]^2[O3] rate=k[NO][O3]^2
Over the past several years, the atmospheric ozone concentration over Antarctica has decreased during the winter. The reaction that causes this is shown below: NO(g)+O3(g)⟶NO2(g)+O2(g) Using the data obtained at 100 degree Celsius, determine the rate law for this process: Trial [NONO] [O3O3 ] Rate 1 1.00x10−61.00x10^-6 3.00x10−63.00x10^-6 6.60x10−56.60x10^-5 2 1.00x10−61.00x10^-6 6.00x10−66.00x10^-6 1.32x10−41.32x10^-4 3 1.00x10−61.00x10^-6 9.00x10−69.00x10^-6 1.98x10−41.98x10^-4 4 3.00x10−63.00x10^-6 9.00x10−69.00x10^-6 1.78x10−31.78x10^-3 None of these. rate=k[NO] rate=k[NO][O3] rate=k[NO]^2[O3] rate=k[NO][O3]^2
Introduction to Chemical Engineering Thermodynamics
8th Edition
ISBN:9781259696527
Author:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Publisher:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Chapter1: Introduction
Section: Chapter Questions
Problem 1.1P
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Over the past several years, the atmospheric ozone concentration over Antarctica has decreased during the winter. The reaction that causes this is shown below:
NO(g)+O3(g)⟶NO2(g)+O2(g)
Using the data obtained at 100 degree Celsius, determine the rate law for this process:
Trial | [NONO] | [O3O3 ] | Rate |
1 | 1.00x10−61.00x10^-6 | 3.00x10−63.00x10^-6 | 6.60x10−56.60x10^-5 |
2 | 1.00x10−61.00x10^-6 | 6.00x10−66.00x10^-6 | 1.32x10−41.32x10^-4 |
3 | 1.00x10−61.00x10^-6 | 9.00x10−69.00x10^-6 | 1.98x10−41.98x10^-4 |
4 | 3.00x10−63.00x10^-6 | 9.00x10−69.00x10^-6 | 1.78x10−31.78x10^-3 |
- None of these.
- rate=k[NO]
- rate=k[NO][O3]
- rate=k[NO]^2[O3]
- rate=k[NO][O3]^2
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