B4.2 - Troposphere

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Last updated 1:11 PM on 6/10/26
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21 Terms

1
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What is an aerosol

tiny solid or liquid particles suspended in air

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Natural sources of aerosols

sea spray (sea salt)
Dust storms (mineral dust)
volcanoes (sulfates)

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Anthropogenic sources of aerosols

fossil fuel combustion (sulfates, nitrates)
incomplete combustion (soot)
industrial processes (metals and complex particles)

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what is a primary aerosol

emitted directly from the source

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what is a secondary aerosol

formed in the atmosphere

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what controls aerosol residence time

particle size (larger ones affected by gravity)

removal processes (wet/dry deposition)

atmospheric conditions (vertical mixing, cloud formation)

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what is wet deposition

Removal through precitipation processes like clouds, rain, and snow

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what is dry deposition

removal through the Earth’s oceanic and terrestrial surfaces (water, soild and vegetation) in the absence of precipitation

9
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what kind of cycles should be considered in the troposphere

null cycles (not catalytic cycles)

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what is the only species H2O will react with

O (1D)

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What species are present in the day

HOx, NOx (polluted), O3

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What species are present at night

NO3 (polluted), O3

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What will RO2 react with

NO (forms NO2 + RO)

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what will RO react with

O2 (forms HO2 + carbonyl or smth)

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What will CO react with

HO2 (forms H which reacts with O2 to form another HO2)

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importance of VOCs, HOx and NOx in the production of ozone in the troposphere

  • NOx/O3 forms a null cycle (NO + O3 → NO2 + O2) when VOC = low (region B)

  • need HOx to break null cycle and use NO2

  • CO + HO + O2 → HO2 + CO2

  • need photolysis of NO2 to form O

  • when [NOx] is low, rate of HO2 + NO → NO2 + OH is small

<ul><li><p>NOx/O3 forms a null cycle (NO + O3 → NO2 + O2) when VOC = low (region B)</p></li><li><p>need HOx to break null cycle and use NO2</p></li><li><p>CO + HO + O2 → HO2 + CO2</p></li><li><p>need photolysis of NO2 to form O</p></li><li><p>when [NOx] is low, rate of HO2 + NO → NO2 + OH is small</p></li></ul><p></p>
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are atmospheric reactions main kinetic or thermodynamically driven

kinetic

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where will O3 likely attack if you have a hindered and non-hindered alkene

non-hindered (kinetic driven)

19
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why draw the squiggles in ozonolysis mechanism

shows different ways the ozonide can break, dar 2 in different colours to show the 2 potential FIRST GENERATION products

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Crigee intermediate

Ozonolysis product, the RO2 one

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in increasing rate coefficient, list the species that can oxidise NMVOCs

O3, NO3, OH, Cl
Only OH and Cl interact with 1 C species