1 mae 5310: combustion fundamentals chemical kinetics: steady-state approximation and chain...
TRANSCRIPT
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MAE 5310: COMBUSTION FUNDAMENTALS
Chemical Kinetics:
Steady-State Approximation and Chain Reactions
October 1, 2012
Mechanical and Aerospace Engineering Department
Florida Institute of Technology
D. R. Kirk
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STEADY-STATE APPROXIMATION
• What are we talking about:
– In many chemical combustion systems, many highly reactive intermediate species (radicals) are formed
• Physical explanation:
– Rapid initial build-up of radical concentration
– Then radicals are destroyed as quickly as they are being created
• Implies that rate of radical formation = rate of radical destruction
– Situation typically occurs when the reaction forming the radicals is slow and the reaction destroying the radicals is fast
– This implies that the concentration of radicals is small in comparison with those of the reactants and products
• The radical species can thus be assumed to be at steady-state
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MECHANISM FOR UNIMOLECULAR REACTIONS
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1
*
*
***
*
*
*
Mkk
Mkk
productsA
Mkk
MAk
kMk
MAkkAk
dt
prodd
kMk
MAkA
AkMAkMAkdt
Ad
productsA
MAMA
MAMA
uni
de
eapp
k
uni
de
e
unide
euniuni
unide
e
unidee
k
k
k
app
uni
de
e
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CHAIN AND CHAIN-BRANCHING REACTIONS• Chain reactions involve production of a radical species that subsequently reacts to produce another
radical. This radical in turn, reacts to produce yet another radical
• Sequence of events, called chain reaction, continues until a reaction involving the formation of a stable species from two radicals breaks the chain
• Consider a hypothetical reaction, represented by a global mechanism:
MABMBA
AABAB
BABBA
MAAMA
ABBA
k
k
k
k
4
3
2
1
2
2
2
22 2
Chain-initiation reaction
Chain-propagating reactions
Chain-terminating reaction
Global model
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CHAIN AND CHAIN-BRANCHING REACTIONS: EXAMPLE
21
4
32121
22
21
22
41
322
12
21
42
31
21
2
22
1
22
41
32
2
2
2
1
42322
4232221
42322
222
23212
411
2
411
2
0
02
k
kkkBA
M
B
kk
kkAM
k
dt
Bd
kk
kk
B
A
M
B
kk
kk
B
AM
k
kA
MBAkABkBAk
MBAkABkBAkMAk
MBAkABkBAkdt
ABd
ABkdt
Bd
BAkMAkdt
Ad
Steady-state approximationfor radical concentration
In the early stages of reaction, the concentrationof the product AB is small, as are the concentrationsof A and B throughout the course of the reactiontherefore, reverse reactions may be neglected atthis reaction stage
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CONCLUSIONS
• Term in brackets [ ] >> 1 because the rate coefficients for the radical concentrations, k2 and k3 are much larger than k1 and k4
• Can write approximate expressions for [A] and d[B2]/dt
• Radical concentration depends on the square root ratio of k1 to k4
– The greater the initiation rate, the greater the radical concentration
– The greater the termination rate, the lesser the radical concentration
– Rate coefficients of chain-propagating steps are likely to have little effect upon radical concentration because k2 and k3 appear as a ratio, and their influence on the radical concentration would be small for rate coefficients of similar magnitude.
• Increasing k2 and k3 results in an increased disappearance of [B2]
• Note that these scalings break down at pressure sufficiently high to cause 4k2k3[B2]/(k1k4[M]2) >> 1
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COMMENTS ON CHAIN-BRANCHING
• Chain Branching
– Chain branching reactions involve formation of two radical species from a reaction that consumes only one radical
• Example: O + H2O → OH + OH
– Existence of a chain-branching step in a chain reaction mechanism can have an explosive effect
• Example: Explosions in H2 and O2 mixtures, that we will examine in our study of detailed mechanisms, are a direct result of chain-branching steps
• Example: Chain-branching reactions are responsible for a flame being self-propagating
– In systems with chain branching, it is possible for the concentration of a radical species to build up geometrically, causing the rapid formation of products
– Unlike the previous hypothetical example, the rate of chain-initiation step does not control the overall reaction rate
– With chain-branching, the rates of radical reactions dominate
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CONCLUSIONS AND COMMENTS ON CHAIN-BRANCHING• Conclusions:
– First term in both equations dominates at low pressures– Concentration of A depends directly on the ratio of the initiation-step rate coefficient, k1, to the
first propagation step, k2, rate coefficient– The rate at which B2 disappears is governed by the initiation step– Increasing k2 and k3 has virtually no effect on the production rates of the products– The termolecular rate coefficient, k4, has virtually no effect on either the radical concentration or
the overall reaction rate, however at higher pressures it does have an influence in the 2nd terms
• Chain Branching– Chain branching reactions involve formation of two radical species from a reaction that consumes
only one radical• Example: O + H2O → OH + OH
– Existence of a chain-branching step in a chain reaction mechanism can have an explosive effect• Example: Explosions in H2 and O2 mixtures, that we will examine in our study of detailed
mechanisms, are a direct result of chain-branching steps• Example: Chain-branching reactions are responsible for a flame being self-propagating
– In systems with chain branching, it is possible for the concentration of a radical species to build up geometrically, causing the rapid formation of products
– Unlike the previous hypothetical example, the rate of chain-initiation step does not control the overall reaction rate
– With chain-branching, the rates of radical reactions dominate
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EXAMPLE: ZELDOVICH MECHANISM FOR NO• A famous mechanism for the formation of nitric oxide from atmospheric nitrogen is called the
Zeldovich (thermal) mechanism, given by:
• Because the second reaction is much fast than the first, the steady-state approximation can be used to evaluate the N-atom concentration. Furthermore, in high-temperature systems, the NO formation reaction is typically much slower than other reactions involving O2 and O. This, the O2 and O can be assumed to be in equilibrium, i.e., O2 ↔ 2O.
• Construct a global mechanism:
• Determine kglobal, m, and n using the elementary rate coefficients, etc., from the detailed mechanism• Using these results and the heating of air to 2500 K and 3 atmospheres, determine:
1. The initial NO formation rate in ppm/s2. The amount of NO formed (in ppm) in the 0.25 ms– The rate coefficient, k1f, is k1f=1.82x1014exp(-38,370/T)
ONOON
NNOONf
f
k
k
2
1
2
2
nmglobal
k
ONkdt
NOd
NOONglobal
22
22 2