An experimental study of the kinetics of this reaction was undertaken in 0.2 mol L¹ hydrochloric acid (HCI) at 298 K. The initial concentration of GHBA was 18.23 x 10³ mol L¹. The concentration of GBL in solution was followed as a function of time (t), as indicated in Table B.3. Time/min GBL concentration /10³ mol L¹ 0 0 21 2.41 36 3.73 50 4.96 65 6.10 80 7.08 100 8.11 Table B.3: Experimental data corresponding to the GHBA to GBL conversion. 13.28 Use the data in Table B.3 to determine the equilibrium constant and the first-order rate constants for both forward and reverse reactions.

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Question B2: Kinetics of a reversible, first-order reaction
The acid-catalysed conversion of y-hydroxybutyric acid (GHBA) into its lactone, y-butyrolactone (GBL) is a
reversible reaction. The GHBA to GBL forward reaction is first-order with respect to the GHBA
concentration; the GBL to GHBA reverse reaction is first-order with respect to the GBL concentration.
Time/min
GBL
An experimental study of the kinetics of this reaction was undertaken in 0.2 mol L¹ hydrochloric acid (HCI) at
298 K. The initial concentration of GHBA was 18.23 x 10³ mol L¹. The concentration of GBL in solution was
followed as a function of time (t), as indicated in Table B.3.
concentration
/10³ mol L¹
0
0
21
2.41
36
3.73
50
4.96
65
6.10
80
7.08
100
8.11
Table B.3: Experimental data corresponding to the GHBA to GBL conversion.
LC
13.28
5
Use the data in Table B.3 to determine the equilibrium constant and the first-order rate constants for both
forward and reverse reactions.
Transcribed Image Text:Question B2: Kinetics of a reversible, first-order reaction The acid-catalysed conversion of y-hydroxybutyric acid (GHBA) into its lactone, y-butyrolactone (GBL) is a reversible reaction. The GHBA to GBL forward reaction is first-order with respect to the GHBA concentration; the GBL to GHBA reverse reaction is first-order with respect to the GBL concentration. Time/min GBL An experimental study of the kinetics of this reaction was undertaken in 0.2 mol L¹ hydrochloric acid (HCI) at 298 K. The initial concentration of GHBA was 18.23 x 10³ mol L¹. The concentration of GBL in solution was followed as a function of time (t), as indicated in Table B.3. concentration /10³ mol L¹ 0 0 21 2.41 36 3.73 50 4.96 65 6.10 80 7.08 100 8.11 Table B.3: Experimental data corresponding to the GHBA to GBL conversion. LC 13.28 5 Use the data in Table B.3 to determine the equilibrium constant and the first-order rate constants for both forward and reverse reactions.
15:44
But how good is this approximation for reactive intermediates in the Earth's atmosphere?
Let us consider the Earth's atmosphere at an altitude of 80 km above the Earth's surface, where the
temperature is "200 K.
Here the combined concentration, [M], of nitrogen gas (N₂) and molecular oxygen (0₂) is
3 x 10¹ molecules cm³, with [M] = [N₂] + [0₂]: molecular oxygen comprises around 20% of this.
Molecular oxygen (O₂) at these altitudes can be photochemically decomposed to excited oxygen atoms, o
(often reported as O('D) and ground-state oxygen atoms,O (often reported as O(³P):
O₂+ hv0+0
(A.1)
In this reaction hv represents a photon of light of sufficient energy to cause the decomposition of O₂. The
rate of this reaction can be represented as labs
The major loss processes for these atoms are:
and
X
0'+M²0+M
(A.2)
k₂= 1.4x10-33 cm molecule-2 s-1
0+0₂ + M²0₂ + M
(A.3)
In reactions (A.2) and (A.3), M = N₂ or O₂, with k, being the second-order rate constant for reaction (A.2),
and k, being the third-order rate constant for equation (A.3). At the altitude and temperature considered,
these composite rate constants have the following values.
kg = 3x10-11 cm³ molecule-1 s-1
Transcribed Image Text:15:44 But how good is this approximation for reactive intermediates in the Earth's atmosphere? Let us consider the Earth's atmosphere at an altitude of 80 km above the Earth's surface, where the temperature is "200 K. Here the combined concentration, [M], of nitrogen gas (N₂) and molecular oxygen (0₂) is 3 x 10¹ molecules cm³, with [M] = [N₂] + [0₂]: molecular oxygen comprises around 20% of this. Molecular oxygen (O₂) at these altitudes can be photochemically decomposed to excited oxygen atoms, o (often reported as O('D) and ground-state oxygen atoms,O (often reported as O(³P): O₂+ hv0+0 (A.1) In this reaction hv represents a photon of light of sufficient energy to cause the decomposition of O₂. The rate of this reaction can be represented as labs The major loss processes for these atoms are: and X 0'+M²0+M (A.2) k₂= 1.4x10-33 cm molecule-2 s-1 0+0₂ + M²0₂ + M (A.3) In reactions (A.2) and (A.3), M = N₂ or O₂, with k, being the second-order rate constant for reaction (A.2), and k, being the third-order rate constant for equation (A.3). At the altitude and temperature considered, these composite rate constants have the following values. kg = 3x10-11 cm³ molecule-1 s-1
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