Tuesday 1 May 2012

Natural Cleaning Process of Atmosphere






 


Residence Time for Different Contaminants in Air

Type
Contaminants Approximate Residence Time

Major species 
N2 106 yr
O2 10 yr

Tracer species 
CO2 15 yr
CH4 10 yr
H2 10 yr
N2O 150 yr
CO 65 days
NH3 20 days
NO/NO2  1 day
O3(troposphere) < 1 yr
HNO3 1 day
CFC 11 65 yr

Sulfur Compounds 
SO2 40 days
COS > 0.3 * 105 hrs
CS2 > 1.8 * 105 hrs
CH3CH 3 - 13 hrs
(CH3)S 31 hrs
H2S 53 hrs
  The residence time gives us an idea of how long it takes for an air contaminant to be removed from the atmosphere. For example, the residence times of carbon dioxide and carbon mono-oxide are 15 years and 65 days respectively. Carbon monoxide is quite reactive, while CO is much more stable.
There are two methods involved in the cleansing of the atmosphere:


bullet Deposition of the pollutants, and
bullet Conversion of pollutants to other forms ( due to oxidation, absorption etc.)
In the atmosphere, rain, snow, and dew tend to wash smoke, dust, pollen, and gaseous waste products. Particles less than 2 microns in diameter are not washed by rain and tend to remain suspended. These particles slowly settle down and are then removed by impaction with trees, rocks, or other surface obstacles. The particles may travel for many miles without regard to national boundaries. Pollutants are deposited on the earth surface due to dry deposition and wet deposition. The dry deposition rate can be computed using the following formula:
Dry deposition rate = Deposition velocity * Pollution concentration
The deposition velocity is generally determined by performing experiments. The deposition velocity generally increases with
(a)    solubility of pollutant
(b)     particle diameter and density
(c)    wetness and roughness of surface
(d)    wind speed and turbulence
Typical values of deposition velocity under experimental conditions are given below:




Species Deposition velocity(cm/s)
O3 0.2 to 0.7
NO 0.01 to 0.1
NO2 0.1 to 0.8
MNO3 0.5 to 5.0
NH3 0.2 to 0.6
PAN 0.1 to 0.6
SO2 0.2 to 3.0
H2S 0.2 to 0.4

In the following sections a discussion is given on cleaning processes involved with various contaminants.
 
Cleansing of SO2
The total world emissions are about 100 million tons/year. SO2 is removed from the atmosphere in about 40 days. The two theories for removal are mentioned below:

1.   SO2  +  O2         >  SO3     + H2O > H2 SO   + NH3, Lime    > Ammonia Sulfate, Calcium Sulfate. 2.   SO2    + NH3, directly calcite of lime  > Sulfites    oxidation >  Sulfate (Precipitate)
    Ammonia Sulfate is a good fertilizer.
Cleansing of H2S
The total world emissions is about 300 million tons/year. Major sources are volcanoes and biological decay. There is no evidence of accumulation.
    H2S      Chemically React - PbO, FeO (metal oxides)   > Insoluble metal sulfides.
In the laboratory odor can be removed by the addition of a few tenths of nitrogen oxides, which act as a catalyst to form H2SO4.  
Cleansing of Ammonia
Ammonia is removed from the atmosphere by reaction with acids or acid forming oxides.
 
Cleansing of Fluorides
Hydrogen fluoride and SiF4 (Silica Fluoride) readily attack a variety of materials (carbonates, silicates, and organic compounds), and are readily removed from the atmosphere.
 
Cleansing of CO bullet    Reaction with the hydroxyl radical. bullet   Oxidized in the upper atmosphere by atomic oxygen to yield CO2. bullet    No evidence of accumulation.


  •  


  • Cleansing of CO2    Consumption in photosynthesis
  • bullet   Removed slowly                 >  silicate rocks                 >  limestone and dolomite.
    bullet    The concentration of CO2 began increasing in the 18th century. Data reported in literature indicate that the increase has          accelerated.
    Cleansing of NOx
    Nitric Acid formed   reacts with ammonia or lime > Ammonia nitrate or Calcium nitrate.
    Cleansing of Smoke
     


    1. Can be removed at source
    2. Smoke particles slowly settle as a result of gravitational effects, agglomeration, or rain.
     
    Cleansing of Hydrocarbons
    Reactive hydrocarbons are removed by a series of photochemical reactions.
     
    A summary of major known sinks for different air contaminants is given in the following table.
     
     

    Major Sinks For Common Air Contaminants
    Contaminants Major known sinks
    SO2 Scavenging, chemical reactions, soil and surface water absorption, dry deposition
    H2S Oxidation to SO2
    N2O Photodissocation in stratosphere, surface water and soil absorption
    NO Oxidation to NO2
    NO2 Photochemical reactions, oxidation to nitrate, scavenging
    NH3 Reaction with SO2 , oxidation to nitrate, scavenging
    CO Soil absorption, chemical oxidation
    O3 Photochemical reactions, absorption by surfaces (soil and vegetation) and surface water
    Non reactive Hydrocarbons Biological action
    Reactive Hydrocarbons Photochemical oxidation
    CO2 Biogenic
    HCl , Cl2  Precipitation

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