Student’s name: DO THI KIM HUE
Class: K52 Advanced Chemistry
**********
Home work II
Problem 7.1
a.
SSA states that d[O]/dt = 0 => r
1
= r
2
r =
3
[]dO
dt
3
[]dO
dt
= r = 2r
1
=2k
1
[O
3
][M] or
2
[]dO
dt
= 3k
1
[O
3
][M]
b.
Cannot assume Quasi-Equilibrated Adsorption (No Langmuir isotherm)
r =
2
d CO
dt
; at steady state, so r
1
= r
2
, Site Balance: L =
SO
+ [S]
1
1 2 2 2
2
[]
k N O S k CO S O S O N O
[]
k
S
k CO
1 2 2
2
1 2 2
Lk k CO N O
r k CO S O
k N O k CO
c.
Step 1 is a quasi equilibrated, but step 2 and 3 isn’t, so no Langmuir isotherm, then
we use SSA to determine surface concentration. We also assume single-site adsorption
and C
2
H
2(ad)
is MARI.
We assume: d[CH
2(ad)
]/dt = 0 → d[CH
2
]/dt = 2k
1
[C
2
H
2
][H
2
] - k
2
[CH
2(ad)
][H
2
] = 0
→ [CH
2(ad)
] = 2k
1
[C
2
H
2
] /k
2
→ 2k
1
= k
2
(1)
r = d[CH
4
]/dt = k
2
[CH
2(ad)
][H
2
] (2)
Site balance for C
2
H
2(ad)
is MARI: L = [C
2
H
2(ad)
] + [S] or 1 = θ
C2H2
+ θ
v
→ [S] = L - [C
2
H
2(ad)
] (3)
From eq. QE 1: K =
[CH 2(ad )][H2]2
[C2H6][S]
→ [C
2
H
2(ad)
] =
C2H6][S]
[H2]2
(4)
Replace (3) into (4), we obtain: [C
2
H
2(ad)
] =
[C2H6]
[H2]2
( L - [C
2
H
2(ad)
])
→ [C
2
H
2(ad)
] =
[C2H6]
(1+[26/[2]2])
H2
2
(5)
Replace (5) into (2), we have the rate:
r = d[CH
4
]/dt = k
2
[CH
2(ad)
][H
2
] =
k2 [C2H6]
26
2
+
H2
Problem 7.2
3
[ ] [ ]
r k B S
d A d B
dt dt
12
[ ] [ ]
K , K
[ ][ ] [ ]
A S B S
A S A S
Site balance:
L=[S] +[A-S] + [B-S]
a) If [B-S] is the MARI, then L= [s] + [B-S] and
2 1 2
12
L S K A S S K K A S S
1 K K A
L
r= k
3
K
2
[A-S]= [K
1
K
2
k
3
[A][S] =
3 1 2
12
Lk K K A
1 K K A
b) If [A-S] is the MARI, then L= [s] + [A-S] and
L= [S] + K
1
[A][S] ] =>
1
S
1 K A
L
r= k
3
K
2
[A-S]= [K
1
K
2
k
3
[A][S] =
3 1 2
1
Lk K K A
1 K A
the mathematical forms are identical.
Problem 7.4
r = -
2 2 2
d H O d H d CO
dt dt dt
r = k
3
[H
2
O*] = k
4
[O*][CO*] and K
1
=
co
CO*
P*
L = [*] + [CO*] + [H
2
O] + [O*] (from site balance)
Steady – state approximations:
On H
2
O* : k
2
P
H2O
[*]= k
3
[H
2
O*]
On O* : k
3
[H
2
O] = k
4
[O*][CO+]
2
3
2
22
34
H O* ( )P & O* H O* / CO*
k
HO
k
k
k
3
2
1 CO H2O 2
34
L K P * P * * H O / CO*
k
k
kk
the last term can be negligible, so
2
2
1 CO H O
3
L K P P 1 *
k
k
22
2
3 2 2 H O
32
3
1 CO H O
. Lk P
r k H O* *
1 K P k'P
HO
k k P
k
Problem 7.5
a. A + S
1
1
k
k
A S reversible RDS (For an ideal gas)
B + S
2
K
B S
A S + B S
3
K
C S + D S
C S
4
K
C + S
5
K
D S D S
A + B
C + D
The rate of reaction r = k
1
P
A
[S] – k
-1
[A S]
From site balance: L = [S] + [A S] + [B S] + [C S] + [D S]
Moreover
2
4
5
[ ] [ ]
[]
[]
B
C
D
B S K P S
PS
CS
K
PS
DS
K
and
3
C S D S
AS
K B S
K =
CD
AB
PP
PP
= K
1
K
2
K
3
K
4
K
5
[A S] =
CD
5 4 3 2 B
P P S
K K K- K P
So we can obtain:
L = [S]
CD
2 3 4 5 B 2 B C D
45
1 P P
11
K K K K P K P P P
KK
Thus r =
1 C D
1A
2 3 4 5 B
Lk P P
Lk P
K K K K P
S
=
1 C D
1A
2 3 4 5 B
CD
2 3 4 5 B 2 B C D
45
Lk P P
Lk P
K K K K P
1 P P
11
K K K K P K P P P
KK
b.
A + S
1
K
A S
B + S
2
K
B S
A S + B S
3
K
C S + D S
C S
4
K
C + S
5
5
k
k
D S D S
Reversible RDS
A + B
C + D
The rate of the reaction:
r = k
5
[D S] – k
-5
P
D
[S]
Using site balance: L = [A S] + [B S] + [C S] + [D S] + [S], we also have
some relations:
2
1
4
[ ] [ ]
[]
[]
B
A
D
B S K P S
A S K P S
PS
DS
K
and
3
C S D S
K
A S B S
So [D S] =
3
1 2 3 4 A B
C
K K K K P P
S
P
K A S B S
CS
L =
C 1 2 3 4 A B
1 A 2 B
4C
P K K K K P P
1 K P K P
KP
S
Thus r =
5 1 2 3 4 A B
5D
C
C 1 2 3 4 A B
1 A 2 B
4C
Lk- K K K K P P
– Lk P
P
P K K K K P P
1 K P K P
KP
In this case, K = K
1
K
2
K
3
K
4
K
5
and K
1
= K
A
, K
2
= K
B
,
4
1
K
= K
C
,
5
1
K
= K
D
=
5
5
k
k
, K
1
K
2
K
3
K
4
=
5
55
kK
K
Kk
Substituting on the rate equation, we get:
r =
5 A B
5D
C
AB
1 A 2 B
C
Lk- KP P
– Lk P
P
KK P P
1 K P K P P K
P
D
CC
c.
A
2
+ 2S
1
1
k
k
2A S reversible RDS
2[B + S
2
K
B S]
2[A S + B S
3
K
C S + D S]
2[ C S
4
K
C + S]
A
2
+ 2B
2C
The rate equation is: r = k
1
P
A2
[S]
2
– k
-1
[A S]
2
,
Applying site balance: L = [A S] + [B S] + [C S] + [S]
2
4
[ ] [ ]
[]
B
C
B S K P S
PS
CS
K
and
3
C S S
K
A S B S
[A S] =
3
*
*
*
C S S
AS
K B S
, K = K
1
K
2
2
K
3
2
K
4
2
or K
1/2
= K
1
1/2
K
2
K
3
K
4
Then, [A S] =
2 3 4 B
K K K P
C
PS
. And L =
2
2 3 4 4
1
CC
B
B
PP
S K P
K K K P K
So we can calculate that:
r =
2
2
22
11
2 3 4 B
2
2
2 3 4 4
22
K K K P
1
C
A
CC
B
B
PS
ZZ
L k P L k
LL
PP
KP
K K K P K
with
2
Z
L
= site-pair probability and Z = coordination number
Moreover, K
2
K
3
K
4
= K
1/2
/K
1
1/2
then:
r =
2
2
'
2
1
2
2
2 3 4 4
1
C
A
B
CC
B
B
P
Lk P
KP
PP
KP
K K K P K
d.
A
2
+ 2S
1
K
2A S
2[B + S
2
K
B S]
2[A S + B S
3
K
C S + D S]
4
4
2
k
k
C S C S
reversible RDS
A
2
+ 2B 2C
The rate equation is:
r = k
4
[C S] – k
-4
P
C
[S]
Also we have: [A S]
2
=
2
2
1A
K P S
; [B S] = K
2
P
B
[S], and
3
C S S
K
A S B S
[C S] =
2
11
22
3 1 2 3
[A ]
K
AB
S B S
K K K P P S
S
From site balance: L = [S] + [A S] + [B S] + [C S]
=
1/2 1/2 1/2 1/2
1 A2 2 B 1 2 3 A2 B
1 K P K P K K K P PS
Moreover, we also have: K = K
1
K
2
2
K
3
2
K
4
2
K
1
1/2
2
1 2 3
4
K
K K K
K
So
2 1/2 1/2 2
4 2 3 A B 4 C
1/2 1/2 1/2 1/2
1 A2 2 B 1 2 3 A2 B
L k K K K P P L k P
22
1 K P K P K K K P P
ZZ
LL
r
With K
1
= K
A2
, K
2
= K
B
,
4
1
K
= K
C
K = K
A
K
B
2
K
3
2
K
4
2
So
1/2 1/2
4 A2 B C
1/2 1/2 1/2
A2 A2 B B C A2 B
L k K P P – P
2
1 K P K P KK P P
Z
r
Problem 7.6
a. The rate equation is: r =
2 4 2
26
3
[]
C H H
d C H
Lk P
dt
2 4 2
25
C H H
2
C H H
P
P
k
Applying steady-state approximation on total surface carbon atoms, we obtain
another equation for
25
CH
, dθ
C(total)
/dt
= 0. Additionally, because steps 2 and 4 are very
rapid:
2 6 2 5 2 4 2
C(total)
1 C H 1 C H 3 C H H
d
k P – Lk – Lk P 0
dt
2 6 2 4 2 5
1 C H 3 C H H2 1 C H H
k P – Lk P Lk
2 5 2 4
25
1 C H 3 C H H2
C H
1
k P – Lk P
Lk
H
2 6 2 4 2
24
2
1 C H 3 C H
2
CH
1
H
H
H
H
k P Lk P
K
P
Lk
=
2 6 2 2 4
2 1 C H 1 H 2 3 C H 1
K k P / Lk P – LK k / Lk
26
24
2
1 2 C H
23
CH
1 1 H
k K P
Kk
1
k Lk P
2 6 2
24
12
C H H
1
CH
2 3 1
kK
P / P
Lk
1 K k k
and
2 2 6
2
26
3 H 1 2 C H
1H
1 2 3 C H
C2H6
2 3 2 3
11
Lk P k K P
Lk P
k K k P
r k’P
K k K k
1 1
kk
but θ
C2H4
can be rewritten to give:
2 6 2
25
1
C H H
3
C H
1 2 3
k
P / P
k
L 1 k / K k
so that
26
1 C H
1
23
k P
r
k
1
Kk
b.
C
2
H
6
+ 2S
1
1
k
k
C
2
H
5
S + H S
C
2
H
5
S + H S
2
K
C
2
H
4
S + S + H
2
C
2
H
4
S + H
2
+ S
3
k
2CH
3
S
4
3 2 4
2 2 2
K
CH S H CH S
C
2
H
6
+ H
2
2CH
4
The rate of reaction can be defined as:
r =
26
d C H
dt
= k
3
[C
2
H
4
S][S]
2
H
P
K
2
= [C
2
H
4
S][S]
2
H
P
/ [C
2
H
5
S][H S]
Steady-state approximation on all surface C atoms gives:
k
1
26
CH
P
[S]
2
– k
-1
[C
2
H
5
S][H S] – k
3
[C
2
H
4
S][S]
2
H
P
= 0
k
1
P
C2H6
[S]
2
– k
3
[C
2
H
4
S][S]
2
H
P
= k
-1
[C
2
H
5
S][H S] and
[C
2
H
5
S] =
26
2
2
1 C H
3 2 4
11
k P S
k [H ]
H
k C H S S P
S k H S
[C
2
H
4
S] =
26
2
2
1 3 2 4
2
1
CH
H
k P S k C H S
K H S
S P k H S
26
2
1 2 C H
23
24
1
1H
k K P
Kk
[C H ] 1
k
kP
S
2 6 2
12
C H H
1
24
23
1
kK
( )P / P
k
[C H ]
Kk
1
k
S
Now, site balance to get [S] is:
L = [S] + [H S] +[C
2
H
5
S] + [C
2
H
4
S] + [CH
3
S]
(a) is obtained only if [S]~ L, it means the surface is essentially free of all adsorbed
species or θ
H
, θ
C2H5
, θ
C2H4
, θ
CH3
<< 1. This is a questionable assumption.
Problem 7.7
Plotting ln rate vs. lnP
i
using a power rate law gives the following reaction orders:
T(K)
Reaction Order
N
2
O
O
2
N
2
623
0.08
-0.31
0
653
0.24
-0.12
0
673
0.31
-0.07
0
The simplest L-H model would be for unimolecular decomposition:
(1) 2[N
2
O + *
2
NO
K
N
2
O *]
(2) 2[N
2
O*
k
N
2
+ O*]
(3) 2O*
2
1/
O
K
O
2
+2*
2N
2
O ==> 2N
2
+ O
2
r
m
=
1
m
dN
N
2
dt
=
1
m
2
= k[N
2
O*]
From(1) : K
N2O
=
[N
2
O
]
2
[]
, so [N
2
O*] = K
N2O
P
N2O
[*]
From(3) : K
O2
=
[]
2
2
[]
2
, so [O*] = K
O2
1/2
P
O2
1/2
[*]
Site balance gives: L=[*] +[N
2
O*] +[O*] thus
L =[*] +
2
2
[*] +
2
1/2
2
1/2
[*] , and [*] =
(1 +
2
2
+
2
1/2
2
1/2
)
,
consequently,
r = k K
N2O
P
N2O
[*] =
2
2
1+
2
2
+
2
1/2
2
1/2
Arrhenius plots of the fitting parameters listed in Table 2 provide the following
values :
For K
N2O
:∆H
ad
o
= -17 kcal mole
-1
and ∆S
ad
o
- 21 cal mole
-1
K
-1
(e.u.)
For K
O2
:∆H
ad
o
= -25 kcal
1
and ∆S
ad
o
- 35 e.u.
For k : E
RDS
= 57 kcal mole
-1
The enthalpy and entropy values for adsorption fulfill all the guidelines in Table 6.9,
thus they are consistent.
From either a linear extrapolation of the high-P portions of the two isotherms in
Figure 1 or using the difference between the two at 100 Torr CO pressure, the irreversible
uptake is 580 µmole CO g
cat
-1
. The dispersion of Cu is : D
Cu
= Cu
s
/ Cu
tot
, and with CO
ad
/Cu
s
= 1,
D
Cu
=
580 µmole Cu
s
g
cat
1
0.0456 g Cu g
cat
1
mole Cu
63.55 g Cu
(10
6
µmole
mole
= 0.81
Under differential reaction conditions, P
O2
O and can be ignored; therefore, an
easy way is to choose a known differential rate and correct for temperature , for example
:
823
673
=
823
673
=
36200 cal /mole /(1.987cal /mole .K )(823K )
36200 cal /mole /(1.987cal /mole .K)(673K )
= 139
thus
TOF
823K
=
823
=
(12.6 µmole /s.g) (13 atm 1)(0.0666 atm )(139)
[1+ (13 atm 1)(0.0666 atm )](580 µmole Cu s/g)
= 1.4 s
-
Problem 7.8
Step 2 defines the rate:
r
m
=
1
m
d
N
2
dt
=
1
m
(-
d
N
2
dt
) = k[N
2
O*]
Step 1 gives : K
N2O
=
[N2O]
PN2O []
, so [N
2
O*] = K
N2O
P
N2O
[*]
Assuming all surface species are included, a site balance gives
L =[*] +[N
2
O*] + [O*]
To remove the unknown [O*], the SSA must be used:
d
[O ]
dt
= k[N
2
O*] + k
-1
P
O2
[*]
2
– k
1
[O*]
2
= 0
And [O*] =(
k[N2O] + k
1
PO2 []
2
k1
)
1
2
Then L = [*] + K
N2O
P
N2O
[*] +
k[N2O] + k
1
PO2 []
2
k1
)
1
2
= z[*] + (x[*] + y[*])
1/2
Where z = 1 + K
N2O
P
N2O
x = k K
N2O
P
N2O
/ k
1
y = k
-1
P
O2
/ k
1
Rearranging and squaring each side gives :
x[*] + y[*]
2
= (L-z[*])
2
= L
2
– 2Lz[*] + z
2
[*]
2
and (y-z
2
) [*]
2
+ (x +2Lz) [*] – L
2
= 0
The solution for this quadratic expression is
[*] =
(x + 2Lz ) ± (x2 + 4Lxz + 4yL2)
1
2
2(yz
2
)
Substituting back and using the positive root gives :
[*] =
kK
N 2O
P
N 2O
/ k
1
+ 2L(1 + K
N 2O
P
N 2O
)
2[k
1
P
O
2
/k
1
(1 + K
N 2O
P
N 2O
)
2
+
+
(
2
2
1
)
2
+
4
2
2
(1+
2
2
)
1
+
4
2
1
2
1
)
1
2
2[k
1
P
O
2
/k
1
(1 + K
N 2O
P
N 2O
)
2
Because the rate is: r
m
= k[N
2
O*] = K
N2O
P
N2O
[*] , the final rate expression is :
r
m
=
2
(1+(+)
2
+[
2
+ (
2
+)
2
+
2
]
1
2
)
(1+
2
)
2
2
Where a = kK
N2O
/ k
1
b = k
1
/k
-1
c = K
N2O
d = LkK
N2O
These four parameters can be combined in various ways to give the values in Table
1.
An Arrhenius plot of the adsorption equilibrium constant, K
N2O
, gives :∆H
ad
o
= -
25.2 kcal mole
-1
and ∆S
ad
o
- 33 e.u. , which satisfy the guidelines in Table 6.9.
The rate constant Lk represents a unimolecular decomposition reaction on the
surface, so guideline 2 in Table 6.10 can be applied :
r
a
= r
m
/A
cu,g
1.1
. .
1
2
354
10
15
2
= 2x10
12
molecule/s.cm
2
or with correction for activation energy:
LA
d
e
-34400/1.987-843
= 2x10
12
= 1.2 x 10
-9
LA
d
and LA
d
= 2x 10
21
molecule/s.cm
s
Both values are below 10
28
.
2
.
Problem 7.10
a, The rate of the reaction as:
2
2
2
[]
1 [ ]
[ *]
2
dN
d NO
r k N
dt dt
Moreover, there are 3 quasi-equilibrated steps, so we have:
22
1
11
22
[ *] [*]
[ *][ *] [ *][*]
[ *] [*]
NO NO
OO
NO K P
N O K NO
O K P
So:
22
22
11
1
11
22
[*] [*]
[ *][*]
[ *]
[ *] [ *]
[*]
NO NO NO NO
OO
K K P K K P
K NO
N
OO
KP
Using the balance gives: L = [N*] + [O*] + [NO*] + [*] then:
22
22
22
22
11
1
22
11
22
11
1
22
11
22
[*] [*] [*] [*]
[*]
1
NO NO
NO NO O O
OO
NO NO
NO NO O O
OO
K K P
L K P K P
KP
L
K K P
K P K P
KP
But, for site pairs:
2
Z
L
is probability factor, thus:
22
2 2 2 2
22
2 2 2 2 2
2 2 2 2
' 2 2 2
21
21
11
22
1
11
22
2
2
1 1 1 1
2 2 2 2
21
[*]
2
(1 )
NO NO
NO NO
NO NO
OO
O O NO NO O O
OO
NO
O O O NO O NO O O NO NO
ZL
k K K P
Lk K K P
r
K K P
KP
K P K P K P
KP
kP
r
K P K K P P K P K K P
b, If [NO*] is assumed to be very lowed compared to the other surface
species, it means [NO*] ~ 0.
2 2 2
2
2
11
22
21
NO
O O O O NO NO
kP
r
K P K P K K P
c, If [NO*] is assumed to be the MARI
2 2 2 2
2
2
1 1 1 1
2 2 2 2
NO
O O O NO O NO
kP
r
K P K K P P
d, If [O*] is assumed to be very low compared to the other surface species or
[O*] ~ 0.
2 2 2 2
2
2
1 1 1 1
2 2 2 2
1
NO
O O O NO O NO NO NO
kP
r
K P K K P P K K P
e, If [O*] is assumed to be the MARI
2 2 2
2
2
11
22
2
NO
O O O O
kP
r
K P K P
f, If [N*] is assumed to be the MARI:
22
2
2
11
22
1
NO
O O NO NO
kP
r
K P K K P
g, If [N*] is not only the MARI, but the surface is also nearly saturated with
N atoms:
[N*] >> [*] and [N*] ~ L
So
2
22
2
Z
r k L ZLk
L
In this case, over a La
2
O
3
catalyst at 923K, this reaction exhibited a reaction order
on NO of about 1.2 with no O
2
in the feed and approximately 1.5 with O
2
, and the rate
decrease significantly with the present of O
2
. the calculation of e, and g, will be rejected
because:
- (e) Order of P
NO
2
- (g) The observed reaction order is not zero.
Problem 7.11
The rate of the reaction can be defined as:
24
11
N CH
m
dN dN
r
m dt m dt
The general reaction can be written as:
CH
4
+ 2O
2
CO
2
+ 2 H
2
O
With dissociative oxygen adsorption, we can obtain the steps of the reaction as
below:
(1)
2
2
2* 2 *
O
K
OO
(2)
4
44
**
CH
K
CH CH
(3)
1
43
* * *
k
CH O CH OH
(4)
2
32
* * * *
K
CH O CH O H
(5)
3
2
* * * *
K
CH O O HCO H
(6)
4
* * * *
K
HCO O CO OH
(7)
5
2
* * * *
K
H OH H O
(8)
6
2
* * * *
K
CO O CO
(9)
2
1
22
**
CO
K
CO CO
(10)
7
2
2 * * *
K
OH H O O
(11)
2
1
22
2 * *
HO
K
H O H O
(12)
1
**
CO
K
CO CO
4 2 2 2
22CH O CO H O
The last step (12) shows the desorption of CO* to get the product of CO. It is easy
to see that the RDS of this sequence is step (3), thus:
14
**
m
r k CH O
However, using the steps (1) and (2), we have
From step (1):
22
11
22
**
OO
O K P
From step (2):
44
4
**
CH CH
CH K P
4 2 4 2
11
2
22
1
*
m CH O CH O
r k K K P P
Moreover, the site balance gives that:
4 2 2
* * * * * *L CH O CO H O CO
Continuously, using the information of steps (9), (11) and (12) we obtain:
22
22
2
2
* [*]
* [*]
* [*]
CO CO
H O H O
CO CO
CO K P
H O K P
CO K P
Then
4 4 2 2 2 2 2 2
11
22
[*]
1
CH CH CO CO O O CO CO H O H O
L
K P K P K P K P K P
4 2 4 2
4 4 2 2 2 2 2 2
11
22
1
11
22
'
1
CH O CH O
m
CH CH O O CO CO H O H O CO CO
Lk K K P P
r
K P K P K P K P K P
Using the data of table 1 and table 2 adding to Arrhenius relation, we can calculate
that:
For CH
4
:
1
20 . ; 13 .
oo
ad ad
H kcal mol S eu
For O
2
:
1
30 . ; 25 .
oo
ad ad
H kcal mol S eu
Problem 7.12
a, NO disappearance:
The rate of the reaction can be defined as:
11
2
NO
i NO
m
i
dN dN
r
m v dt m dt
And
* 0 * 1
NO
m s NO s NO HNO
r L L k L L k
in which L
*
and L
s
is the density of * and S
sites, respectively.
Applying SSA on HNO* gives:
* 0 * 1
*
0
s NO s NO HNO
d HNO
L L k L L k
dt
and r
3
= r
4
, then
*0
*
2
NO
m s NO H
d HNO
r L L k
dt
Site balance for [*] sites is: L
*
= [*] + [NO*] and
*
*
NO
NO
NO
K
P
We have:
*
*
*
[*]
1
*
1
*
1
NO NO
NO NO
NO NO
NO NO
NO
NO NO
L
KP
L K P
NO
KP
NO
KP
L K P
Site balance on S sites: L
s
= [S] + [H – S] and
2
2
2
2
H
H
HS
K
PS
22
22
22
22
11
22
11
22
11
22
11
22
1
1
S
HH
HH
H H H
S
HH
L
S
KP
KP
HS
KP
L
KP
when θ
H
<< 1
Thus:
22
11
22
*0
2
1
NO
S NO H H NO
m
NO NO
L L k K K P P
r
KP
b, N
2
formation:
The rate:
2
2
*2
1
NO
N
m N O
dN
r L k
m dt
Using SSA on N
2
O* site:
2 2 2
2
* 1 * 2 * 2 * 3 *
0
S HNO NO N O N O N O
d N O
L L k L k L k L k P
dt
Then
22
2 2 2 2
2
2 2 2
2
* 2 * 3 * 1 * 3 *
11
22
0 3 * 0 3
2 3 2 3 2 3
11
*2
22
03
23
11
1
N
N O S HNO NO N O
S NO H N O S NO H NO H N O
NO
NO NO NO NO
m S NO H NO H N O
NO NO
L k L k L L k L k P
L k k P L k K K P P k P
k k k k K P k k K P
Lk
r L k K K P P k P
k k K P
c, N
2
O formation:
Similarly a, b we have:
2
22
2
2 2 2 2
2 2 2 2
2
* 3 * 3 *
11
22
0 3 * 3
*3
23
11
22
0 3 3 3 3 3 2 3
*
23
1
03
*
23
1
11
1
NO
NO
m N O N O
S NO H NO H N O N O
NO NO NO NO
S NO H NO H N O N O
NO NO
S NO H
dN
r L k L k P
m dt
L k K K P P k P L k P
Lk
k k K P K P
L k k K K P P k k P k k k k P
L
k k K P
L k k K K
L
kk
22
1
22
3 2 3
1
NO H N O
NO NO
P P k k k P
KP
Problem 7.14
The specific rate is:
=
1
2
=
1
2
=
1
Ѳ
2
The steps 1and 2:
2
=
Ѳ
2
2
Ѳ
And
=
Ѳ
Ѳ
SSA on O*:
Ѳ
=
1
Ѳ
2
2
Ѳ
Ѳ
Ѳ
=
1
Ѳ
2
2
Ѳ
=
1
2
2
Ѳ
2
Ѳ
Site balance:
1 = Ѳ
+
2
2
Ѳ
+
Ѳ
+
1
2
2
2
1
1
2
2
2
= Ѳ
1 +
2
2
+
=
1
2
2
Ѳ
=
1
2
2
1
1
2
2
2
1 +
2
2
+
Or
=
µ
1
1
=
2
2
2
1+
2
2
+
where =
1
2
and =
1
2
2
2
2
An Arrhenius plot of LK
1
gives E
1
= 26kcalmole
-1
while similar plots for K
N2O
and
K
CO
give:
- For N
2
O:
= 13 kcalmole
-1
and
= 29 calmole
-1
K
-1
(e.u.)
- For CO:
= 10 kcalmole
-1
and
= 23e.u.
All these thermodynamic values satisfy the criteria in Table 6.9. The TOF at 573K =
2100µ2
1
1
769µ
1
0.91
= 3.0
1
. Thus the pre-exponential factor per site is 3.0
1
=
0
26000
1.987
(573)
0
= 2.4 x 10
10
s
-1
which is less than 10
13
s
-1
and satisfies criterion 2
in table 6.10 for a unimolecular reaction. Also, the heat of adsorption of 10kcalmole
-1
for
CO on Cu is consistent with value of 7-10 kcalmole
-1
reported in the literature.
Problem 7.15
=
4
=
1
4
1
2
2
=
7
[2]
From step (6): [
2
O*] =
6
2
/[]
From step (4): [OH*] =
4
2
/[]
From step (2): [
2
*] =
2
2
[]
From step (8): [CO*] =
8
[]
Therefore:
=
7
6
2
/[] =
7
6
4
[
2
][
2
]/[]
=
7
6
4
2
2
[
2
][
2
]/
8
[]
SSA from surface CH
2
* (and CH
2
O*) species:
[
2
···]
=
1
4
1
2
2
7
2
= 0
2
=
1
4
1
2
2
7
From step (6):
2
=
2
[]
6
[]
=
2
[]
6
4
[
2
]
=
8
2
[]
2
4
6
2
[]
=
8
2
4
6
2
[
2
]
From SSA:
1
4
[] = (
7
+
1
8
2
2
4
6
2
)
2
Hence,
2
=
1
7
4
[]
1 +
1
8
2
7
6
4
2
Site balance with [CH
2
O*] as MARI: =
+[CH
2
O*]=
1 +
1
4
7
1 +
1
8
2
7
6
4
2
2
=
1 +
1
8
2
7
6
4
2
2
+
1
4
7
1 +
1
8
2
7
6
4
2
2
=
1+
1
8
2
7
6
4
2
2
1+
1
8
2
7
6
4
2
2
+
1
4
7
=
7
2
=
7
1
7
4
1 +
1
8
2
7
6
4
2
=
1
4
1 +
1
8
2
7
6
4
2
2
+
1
4
7
=
1
4
2
2
+
1
8
2
7
6
4
2
+
1
4
2
7
The TOF for step 7 is
5.35 µ
1
1
2.4µ
2
1
2µ
µ
2
= 1.1
1
Rate per site: TOF=1.1
s-1
=Ae
-E/RT
=Ae
-38000/1.987 (723)
=A( 3.25x10
-12
). Therefore,
A= 1.1/3.25x10
-12
= 3.4x10
11
s
-1
, which is less than 10
13
(Criterion 2 in Table 6.10)
Problem 7.16
2 2
1 1 1 1 1
22
N
i NO NO
m
i
dN
dN dN dN
dN
d
r
m dt m dt m dt m dt dt dt
2
1
2 [ *]
NO
dN
k NO
dt
,
[ *]
[ *] [*]
[*]
NO NO NO
NO
NO
K NO K P
P
L= [*] + 2[*(NO
2
)*] + [N
2
O*] + [O*] + [NO*] = [NO*]+ [O*]
2 2 2
2
2
1/2 1/2
[ *]
[ *] [*]
[*]
O O O
O
O
K O K P
P
22
1/2 1/2
[*](1 )
NO NO O O
L K P K P
and
22
1/2 1/2
[*] / (1
NO NO O O
L K P K P
So
22
22
2 2 2 2
1
1
21
1/2 1/2 2
2
[ *] [*]
2 (1 )
NO NO
N NO NO
NO NO O O
Lk K P
k
r NO k K P
K P K P
Or
2
32
[ *]
N
r k N O
and SSA on N
2
O* gives k
2
[*(NO
2
)
2
*]=k
3
[N
2
O*]
So
2
22
[* *]
N
r k N O
and SSA on[* N
2
O*] gives k
1
(NO
*
)
2
=k
2
[*(NO)
2
*]
So
2 2 2
2 2 2 1/2 1/2 2
11
[ *] / (1 )
N NO NO NO NO O O
r k NO Lk K P K P K P
b) From the site balance
k
3
[N
2
O*]=k
1
[NO
*]
2
and [N
2
O*]=(k
1
/k
3
)K
NO
P
NO
[*]
2
and k
2
[*(NO)
2
*]=k
1
[NO*]
2
and [*(NO)
2
*] = (k
1
/k
2
)K
NO
P
NO
[*]
2
then
4
3 2 4
2 2 2
K
CH S H CH S
Consequently, a quadractic expression for [*] is obtained and the solution for such
an equation is so complicated.
Problem 7.17
The series of elementary steps is:
(1) MCH + * MCH*
(2) MCH* MCX* +H
2
(3) MCX* MCD* +H
2
(4) MCD* TOL* + H
2
(5) TOL* TOL + * (RDS)
MCH TOL
Or
MCH + * TOL* + 3H2 where K’=K
1
K
2
K
3
K
4
TOL* TOL + *
Step 5 is RDS, so r = k
5
[TOL*]
L = [*] + [MCH*] + [MCX*] + [MCD*] + [TOL*]
If [TOL*] is MARI, then L = [*] + [TOL*] = [*](1+
2
3
) and [*] =
1+
2
3
Then, r = k
5
[TOL*]=k
5
2
3
=
5
(1+
2
3
)
2
3
or, r =
5
(
2
3
+
)
This is not consistent with the behavior because it contains
a
2
3
term.
Problem 7.18
22
22
2( )
1 3 2
2
g
OO
dO
r k P S k HCO S O S kP S
dt
2
L S HCO S O S
(1)
2
2
2
2
H CO
K P O S
HCO S
OH S
(2)
22
1/2 1/2
1/2 1/2
H O H O
OH S K P O S S
(3)
22
22
22
2 1/2 1/2
22
2
1/2 1/2
1/2 1/2
1/2 1/2
H CO H CO
H O H O
H O H O
K P O S K P O S S
HCO S
KP
K P O S S
(4) At steady-state:
2
2
1
32
O
k P S
OS
k HCO S
(Balance on O-S species)
(5) Substitute (4) in (3):
22
22
3/2 3/2 5/2
21
2
3/2
3/2 1/2 1/2
32
O
H CO O
H O H
K P k P S
HCO S
k HCO S K P
, then
(6)
22
22
2/5 2/5 3/5 3/5
21
2
3/5 1/5 1/5
3
H CO O
H O H O
K P k P S
HCO S
k K P
(7)
2 2 2
2
2/5 1/5 1/5
1
2/5 2/5 3/5 2/5
3 2 1
O H O H O
H CO
k P S K P
OS
k K k P
(8)
2 2 2 2 2
2 2 2
2/5 3/5 2/5 3/5 2/5 2/5 1/5 1/5
2 1 1
3/5 1/5 1/5 2/5 2/5 2/5
3 3 2
H CO O O H O H O
H O H O H CO
K k P P S k P K P S
LS
k K P k K P
(9)
2 2 2 2 2 2
2/5 3/5 1/5 2/5 2/5 1/5
1 ' ''
H CO O H O O H CO H O
L
S
K P P P K P P P
Assume P
H2O
is approximately constant and power of 0.2 is low. Then,
2
2 2 2 2
1
2
0.4 0.6 0.4 0.4
1 "' ''''
O
H CO O O H CO
Lk P
r
K P P K P P
If θ
HCO2
<<1 and θ
O
<<1, then r = kP
O2
If θ
O
is MASI, i.e., θ
O
>> θ
HCO2
then
2 2 2
2 2 2 2
0.8
1
22
0.4 0.4 0.4 0.4
'
1 '''' / ''''
O O H CO
O H CO H CO O
Lk P k P P
r
K P P P K P