Tropospheric Chemistry Flashcards
(32 cards)
Why is O(1D) production slower in troposphere?
Narrower wavelength band that can photolyze to produce O(1D)
What do we use to measure [OH] in troposphere?
Methylchloroform, CH2CCl3- only produced anthropogenically, banned in Montreal protocol, lifetime = 1/k[OH]
Sinks of OH in troposphere
OH + X –> products
where X is non-radical reduced species
Source of OH in troposphere
O3 + hv –> O2 +O(1D)
O(1D) + H2O –> 2OH
Key difference between troposphere and stratosphere
lower O3 and O concentrations in troposphere, lower O(1D), lower energy photons
Principal sink of NOx in the atmosphere - daytime
NOx + OH –> HNO3
only occurs in the daytime , not much OH at night
Three NOx sinks at nighttime
NO2 + O3 → NO3 + O2;
NO3 + NO2 → N2O5;
N2O5+H2O → 2HNO3
Why is HNO3 not an effective reservoir for NOx
Precipiates out in wet deposition too quickly
Production of PAN
peroxyacytlnitrate
CH3CHO + OH → CH3CO + H2O
CH3CO + O2 + M → CH3C(O)OO + M
CH3C(O)OO+NO2 +M→PAN+M
How does PAN function as a reservoir for NOx
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
Ozone production inside the troposphere
HO2 + NO –> NO2 + OH
CH3O2 + NO –> CH3O + NO2
NO2 + hv –> NO +O3 (in presence of O2)
Loss pathways of O3 in troposphere
dry deposition
in remote troposphere: reacting with OH and HO2
O3 –> O(1D) + O2
O(1D) + H2O –> 2OH
Increasing NOx or O3- impact on OH
Increases OH
Increasing CO or CH4- impact on OH
Decrease OH
O3 destruction that is HOx propogation
OH + O3 –> O2 + HO2
HO2 + O3 –> 2O2 + OH
net : 2O3 –> 2O2
HOx + O3 cycling stops with loss of HOx radicals. This happens two ways:
In low NOx: peroxyl radicals react with themselves
HO2 + HO2 –> H2O2 +O2
In High NOx: oxidation of NO2
NO2 + OH –> HNO3
Why is isoprene the primary hydrocarbon that contributes to ozone production
abundant, has two C=C bonds that OH reacts with very quickly. lifetime of a few hours
Ozone production efficiency
ε = PO3/LNOx. How many ozone molecules are produced per molecule NOx consumed.
increasing hydrocarbon concentrations does what to ozone production efficiency?
Increases-
Increasing hydrocarbons will decrease OH and extend lifetime of NOx, more O3 per NOx
increasing NOx concentrations does what to ozone production efficiency?
Decrease-
Increasing NOx causes OH to increase, decreases lifetime of NOx
Typical values of Ozone production efficiency
1-20 mol/mol
One reason O3 may be increasing despite air quality constraints
Decreasing particulate matter pollution- particles scavenge HO2 radicals that otherwise would go to ozone production. Less particulate matter- more HO2 forms more ozone.
Sources of HO2 in troposphere
Photodissociation of CH2O
CH2O + hv –> H + HCO
H + O2 +M –> HO2 + M
HCO + O2 –> HO2 + CO
from alkoxy radical reactions
RCH2O + O2 –> RCHO + HO2
HONO photolysis
HONO + hv –> OH + NO
builds up at night
important source at daybreak
very long wavelength