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- Distribution & concentration (1)
- Distribution & concentration (2)
     
 

Lower Atmosphere

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Distribution & concentration (2)

If we would like to know about concentrations of less stable compounds in the atmosphere, we cannot just give a number. They depend very much on the chemistry going on in the air.

 

 

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Vertical profile

Not only the horizontal distribution can vary depending on sources, sinks and different physical parameters (hours of sunshine, temperature, precipitation, wind). Most gases have also a vertical profile and often show slightly decreasing mixing ratios with increasing altitudes, in particular above the tropopause and in the first two kilometres from the planetary boundary layer (influenced by the Earth surface) to the free troposphere. An exception is ozone, which has the highest mixing ratio and concentration in the ozone layer in the stratosphere. But we need not to go that high. Most of the chemistry is taking place in the boundary layer next to the ground, where the chemical compounds are emitted.

In the graphs below you see vertical tropospheric profiles of several organic and inorganic trace gases measured by a research plane. Apart from carbon dioxide, ozone and methane typical values for mixing ratios are a few hundred ppt or a few ppb. But the ones observed here are only the more important trace gases. There are hundreds of other organic gases which have lower mixing ratios of only a few ppt.

 

modelled PBL concentrations

1. Mixing ratios of different compounds changing during the night next to the ground. The ratios are not measured but the result of a chemical model. This allows also to consider the changes in time which are shown in different colours.
Authors: Andreas Geyer, Shuihui Wang and Jochen Stutz

 

vertical profile 1

Measured compounds:

CH4 = methane
CO = carbon monoxide
CH3OH = methanol
CH3COCH3 = acetone
HCHO = formaldehyde

 

vertical profile 2

O3 = ozone
NO = nitrogen oxide
NOy = oxidised nitrogen compounds without NO, NO2
PAN = peroxiacetylnitrate
CN = condensation nuclei (particles)

 

vertical profile 3

2. a-c) Vertical profiles of various organic and a few inorganic gases
The values have been measured in a research plane over the Mediterranean sea during the MINOS field campaign in august 2001. The strong black lines show the median vertical profiles, the thinner black lines the standard deviation. Grey squares show values from canister samples. Red dashed lines and red squares are from another flight and give you an idea of how the values may vary within a few days.
Each larger view of the graphs has 16 K. Click on the image!
Data and illustration from: J. Lelieveld and co-authors

 

C2H6 = ethane
C2H2 = acetylene = ethyne
C3H8 = propane
C6H6 = benzene
CH3Cl = methyl chloride

 

Gases in the troposphere

To give an overview of trace gases in the troposphere and their concentrations is hardly possible. The same compound can be present in extremely low concentrations for example over the ocean and in very high concentrations in the urban environment. Also, a few dozens of gases could be regarded as important. Therefore the following table can only be a compilation of examples, which gives a reasonable range of mixing ratios (usually near the ground) for often measured compounds.

 

Overview of important gases in the free atmosphere:

name

formula

mixing ratio

nitrogen
N2
78.08 %
oxygen
O2
20.95 %
argon
Ar
0.93 %
water vapour
H2O
0.1 - 4 %
= 1,000 - 40,000 ppm
carbon dioxide
CO2
372 ppm*
carbon monoxide
CO
50 - 200 ppb
methane
CH4
1.7-1.8 ppm*
hydrogen
H2
0.5 ppm
(480 - 540 ppb)
ozone
O3
10 -100 ppb
troposph. average: 34* ppb
hydroxi radical
OH
< 0.01 - 1 ppt
nitrogen dioxide
NO2
1 - 10 ppb
nitrogen oxide
NO
0.1 - 2 ppb
nitrous oxide
N2O
320 ppb*
nitrate radical
NO3
5 - 450 ppt
nitric acid
HNO3
0.1-50 ppb
ammonia
NH3
< 0.02 - 100 ppb
sulfur dioxide
SO2
1 ppb (background)
1 ppm (polluted air)
formaldehyde
HCHO
0.5 - 75 ppb
formic acid
HCOOH
< 20 ppb
acetone
CH3COCH3
0.1 - 5 ppb
isoprene
C5H8
< 1 - 50 ppb
monoterpenes
-
< 100 ppt
carbonyl sulfide
COS
500 +/- 50 ppt
CFC11
CCl3F
258*
CFC12
CCl2F2
546*
*Gases with increasing concentration due to human influence which are relatively well mixed over the globe. Data from 2001-2003.

 

Mixing ratios, concentrations and different units:

Amounts of gases are often given in different units:

concentrations: molecules/cm3 or µg/m3
or mixing ratios: ppt (pmol/mol), ppb (nmol/mol), ppm (µmol/mol), % (10 mmol/mol)

Mixing ratios are often more helpful for scientist, because if air rises and expands the volume grows and therefore the concentration change, but the mixing ratio (relation of the gases) remains the same.
The conversion from one unit into the other depends on the pressure (= the altitude) and molecular weight. If we do the calculation for the Earth surface for normal pressure of about 1 bar we can express the total molecules per air volume in the following way:

1 mol = 22.4 L = 6x1023 molecules =>
1 cm3 = 2.7x1019 molecules
1 dm3 = 1 L = 2.7x1022 molecules
1 m3 = 2.7x1025 molecules

Example for a rough estimate:

2 µg/m3 = 2x10-6 g/m3 NO2 is a typical value for nitrogen dioxide in a non-urban area.
molecular weight M(NO2) = 46 g/mol
This means: 2x10-6 g/m3 = 4.3x10-8 mol/m3 = 2.6x1016 molec/m3

So the mixing ratio is about 2.7x1016 / 2.7x1025 = 10-9 = 1 ppb

Since ozone has a similar molecular weight, M(O3) = 48 g/mol, we can also roughly say
2 µg/m3 of ozone = 1 ppb
This calculation is valid only for the Earth surface, where we live. So, for ozone smog events in urban areas we can now calculate:
120 µg/m3 = 60 ppb -> high level
240 µg/m3 = 120 ppb -> very high level, no sports, risk for health
360 µg/m3 = 180 ppb -> extremely high level, very unhealthy for the lung, stay at home!

 

Related pages

You will find more explanations about concentrations and mixing ratios in
Higher atmosphere - Basics - Unit 1 - composition

 

About this page:
author: Dr. Elmar Uherek - Max Planck Institute for Chemistry Mainz
scientific reviewer: Dr. Rolf Sander - Max Planck Institute for Chemistry, Mainz - 2004-05-18
last published: 2004-04-06

 

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last updated 11.07.2006 09:36:28 | © ESPERE-ENC 2003 - 2013