Tropospheric Chemistry Flashcards

(32 cards)

1
Q

Why is O(1D) production slower in troposphere?

A

Narrower wavelength band that can photolyze to produce O(1D)

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2
Q

What do we use to measure [OH] in troposphere?

A

Methylchloroform, CH2CCl3- only produced anthropogenically, banned in Montreal protocol, lifetime = 1/k[OH]

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3
Q

Sinks of OH in troposphere

A

OH + X –> products

where X is non-radical reduced species

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4
Q

Source of OH in troposphere

A

O3 + hv –> O2 +O(1D)

O(1D) + H2O –> 2OH

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5
Q

Key difference between troposphere and stratosphere

A

lower O3 and O concentrations in troposphere, lower O(1D), lower energy photons

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6
Q

Principal sink of NOx in the atmosphere - daytime

A

NOx + OH –> HNO3

only occurs in the daytime , not much OH at night

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7
Q

Three NOx sinks at nighttime

A

NO2 + O3 → NO3 + O2;
NO3 + NO2 → N2O5;
N2O5+H2O → 2HNO3

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8
Q

Why is HNO3 not an effective reservoir for NOx

A

Precipiates out in wet deposition too quickly

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9
Q

Production of PAN

A

peroxyacytlnitrate
CH3CHO + OH → CH3CO + H2O
CH3CO + O2 + M → CH3C(O)OO + M
CH3C(O)OO+NO2 +M→PAN+M

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10
Q

How does PAN function as a reservoir for NOx

A

PAN can thermally decompose to produce NOx,
PAN –> CH3C(O)OO + NO2
This is very temperature sensitive. PAN can be transported out of an area to later on thermally decompose back into NOx, facilitating the transport of NOx
PAN is most important reservoir

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11
Q

Ozone production inside the troposphere

A

HO2 + NO –> NO2 + OH
CH3O2 + NO –> CH3O + NO2
NO2 + hv –> NO +O3 (in presence of O2)

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12
Q

Loss pathways of O3 in troposphere

A

dry deposition
in remote troposphere: reacting with OH and HO2
O3 –> O(1D) + O2
O(1D) + H2O –> 2OH

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13
Q

Increasing NOx or O3- impact on OH

A

Increases OH

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14
Q

Increasing CO or CH4- impact on OH

A

Decrease OH

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15
Q

O3 destruction that is HOx propogation

A

OH + O3 –> O2 + HO2
HO2 + O3 –> 2O2 + OH
net : 2O3 –> 2O2

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16
Q

HOx + O3 cycling stops with loss of HOx radicals. This happens two ways:

A

In low NOx: peroxyl radicals react with themselves
HO2 + HO2 –> H2O2 +O2

In High NOx: oxidation of NO2
NO2 + OH –> HNO3

17
Q

Why is isoprene the primary hydrocarbon that contributes to ozone production

A

abundant, has two C=C bonds that OH reacts with very quickly. lifetime of a few hours

18
Q

Ozone production efficiency

A

ε = PO3/LNOx. How many ozone molecules are produced per molecule NOx consumed.

19
Q

increasing hydrocarbon concentrations does what to ozone production efficiency?

A

Increases-

Increasing hydrocarbons will decrease OH and extend lifetime of NOx, more O3 per NOx

20
Q

increasing NOx concentrations does what to ozone production efficiency?

A

Decrease-

Increasing NOx causes OH to increase, decreases lifetime of NOx

21
Q

Typical values of Ozone production efficiency

22
Q

One reason O3 may be increasing despite air quality constraints

A

Decreasing particulate matter pollution- particles scavenge HO2 radicals that otherwise would go to ozone production. Less particulate matter- more HO2 forms more ozone.

23
Q

Sources of HO2 in troposphere

A

Photodissociation of CH2O
CH2O + hv –> H + HCO
H + O2 +M –> HO2 + M
HCO + O2 –> HO2 + CO

from alkoxy radical reactions
RCH2O + O2 –> RCHO + HO2

24
Q

HONO photolysis

A

HONO + hv –> OH + NO
builds up at night
important source at daybreak
very long wavelength

25
O3 source in troposphere
photodissociation of NO2 NO2 + hv --> NO + O O + O2 --> O3
26
Sources of NO3 in troposphere
Oxidation of NO2 NO2 + O3 --> NO3 + O2
27
Sources of chlorine in troposphere
Sea salt chemistry
28
Lifetimes
``` d[M]/dt = -k[X][M] lifetime = 1/k[X] ```
29
Primary nighttime oxidant
NO3
30
peroxy radicals NO oxidation
NO +HO2 --> OH +NO2 | NO + RO2 --> RO + NO2
31
Oxidation of NO2
Daytime- NO2 + OH --> HONO2 nighttime: NO2 + O3 --> NO2 + O2 NO2 + NO3 --> N2O5
32
Source of HONO
OH + NO --> HONO