Week 3 Flashcards

(50 cards)

1
Q

What does the box represent in a box model?

A

Small parcel of air or the entire globe

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2
Q

What do we assume within a box model?

A

That the box is well mixed

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3
Q

What is another way of thinking of the lifetime t of X in the box?

A

The average time that a molecule of X remains in the box

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4
Q

Equation to workout lifetime t of X in the box

A

t= m/Fout+L+D

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5
Q

What does P represent in atmospheric box?

A

Chemical production

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6
Q

What does L represent in box model?

A

Chemical loss

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7
Q

What does E represent in box model?

A

Emission

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8
Q

What does D represent in box model?

A

Deposition

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9
Q

What is lifetime?

A

The average/median time that a molecule of X remains in the box

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10
Q

Residence time

A

When the loss terms are physical loss e.g. Fout or D

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11
Q

Generalised chemical rate constant is chemical loss rate is:

A

Fout+ L +D=(kout+kL+kD)=km

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12
Q

Chemical rate constant equation:

A

kout=1/tout

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13
Q

What is the concept of mass balance?

A

Mass is conserved- what is produced in one place must be lost elsewhere

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14
Q

Sources in a box model

A

Inflow (Fin), Emission and Chemical production

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15
Q

Sinks within box model:

A

Chemical loss, deposition and Outflow (Fout)

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16
Q

Overall Source rate Equation:

A

S = Fin+E+P

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17
Q

The cycling of what compounds are central to the production of O3

A

NOx and HOx and VOCs

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18
Q

Expression describing the steady state concentration of CO from the oxidation background CH4 if the mean rate constants for CH4 and CO by OH in the atmosphere are K1 and K2 respectively

A

K1[CH4][OH]=K[CO][OH]

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19
Q

What are initiation reactions?(HOx)

A

Reactions producing HOx (OH and HO2) from non HOx species introducing new radicals to system

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20
Q

What are propagation reactions?(HOx)

A

Reactions that inter convert OH and HO2 maintaining HOx pool without net production loss

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21
Q

What are termination reactions? (HOx)

A

Reactions removing HOx radicals from system forming stable products

22
Q

Low NOx termination

A

Dominated by HOx self reactions or reactions with peroxides

23
Q

High NOx termination

A

Terminsation involving NOx species e.g. nitric acid formation

24
Q

Equation- Initiation for HOx

A

O(1D)+H2O –> 2OH

25
Equation Low NOx termination
HO2 + HO2 --> H2O2 + O2
26
Equation High NOx termination
NO2 + OH + M --> HNO3
27
Equation propogation examples HOx
CO + OH --> HO2 + CO2 HO2 + NO --> OH + NO2 NO2 +OH + M --> HNO3
28
Which compounds work together to oxidise CO and CH4 leading to ozone production (O3)
HOx and NOx
29
Propagation steps without NOx-
CO + OH* → CO₂ + H* H* + O₂ + M → HO₂* + M
30
Rate law - first order reaction
Rate= k[A] in s^-1
31
Rate law - second order reaction
Rate= k[A]^2 or k[A][B]
32
Lifetime- first order reaction
t=1/k
33
Lifetime - second order reaction
t=1/k[A]o
34
Sources of NOx
* Fossil Fuel Combustion * Transport from stratosphere * Biomass burning * NH3 oxidation * Lightning * Aircrafts
35
Production of Thermal NOx via Zeldovich mechanism
O2 <--> O +O O+N2 <--> NO + N N + O2 <--> NO + O
36
Why are NO and NO2 part of the NOx family?
Because they cycle rapidly between each other
37
Equations - cycling of NO and NO2
NO + O3 --> NO2 + O2 NO2 + hv --> NO + O --> O + O2 --> O3
38
Daytime sink of NOx- main loss path
NO2 + OH + M --> HNO3 + M
39
Why is HNO3 lost by precipitation
It is soluble
40
Levels of OH at nightime
Low- other oxidants dominate
41
Storage of NOx- PAN
PAN acts as a reservoir = temporary transport
42
How to HOx and NOX work together to produce ozone?
HOX- initiates oxidation of VOCs or CO and peroxy radicals react with NO converting it to NO2 which then undergoes photolysis to form O3
43
Net effect of VOCs+NOx to form O3
VOCs (or CO) + NOₓ + sunlight → O₃ + other oxidized products
44
Levels of O3 at nightime
O3 is Scarce meaning other oxidants dominate
45
Difference between PAN and HNO3 for NOx transport
PAN is a reservoir - temporary storage whereas HNO3 is more of a permanent sink
46
How is PAN formed
From the oxidation of carbonyl compounds in the presence of NOX
47
Stability of PAN vs HNO3
PAN is stable at colder temperatures- upper troposphere HNO3 is not stable at altitude
48
Transport role of PAN vs HNO3 for O3
PAN is a major carrier of NOx over distance HNO3 transport of NOx is minimal
49
How can temperature effect PAN?
PAN can thermally decompose- at 295k lifetime= 1 hour and at 250K lifetime is several months
50