understanding 8.5 acid deposition

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Acid deposition

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Page 1: Understanding 8.5 Acid deposition

Acid deposition

Page 2: Understanding 8.5 Acid deposition

• Oxides of non-metals are acidic and, if soluble in water, dissolve to produce acidic solutions.

• Rain is naturally acidic because of dissolved carbon dioxide :

•H2O (l) + CO2 (g) H2CO3 (aq)

Carbonic acid

Page 3: Understanding 8.5 Acid deposition

• H2CO3 (aq) is a weak acid and dissociates partially according to the equation :

H2CO3 (aq) H+ (aq) + HCO3- (aq)

Page 4: Understanding 8.5 Acid deposition

• Because of these reaction, the pH of rain water is about 5.6.

• This is a natural phenomenon- rain with a pH between 5.6 and 7 is not considered to be ‘acid rain’.

Page 5: Understanding 8.5 Acid deposition

• Acid rain is considered to be rain with a pH lower than 5.6.

• The average pH of rain in some areas can be as low as 4.

Page 6: Understanding 8.5 Acid deposition

• Acidic pollutants include the oxides of sulphur and nitrogen.

• Sulphur dioxide (sulfur(IV) oxide) can be formed by various natural and anthropogenic process – such as the burning of sulfur-containing fuels :

S(s) + O2(g) SO2(g)

Page 7: Understanding 8.5 Acid deposition

• The process by which SO2 is converted into SO3 and H2SO4 in the atmosphere is complex and does not involve simple oxidation by atmospheric oxygen – interactions with hydroxyl radicals, ozone or hydrogen peroxide are involved.

Page 8: Understanding 8.5 Acid deposition

• However, the reactions can be summarised :

2SO2(g) + O2(g) 2SO3 (g)

2SO3(g) + H2O (l) H2SO4 (aq)

Page 9: Understanding 8.5 Acid deposition

• SO2 can also dissolve in water to produce sulfuric acid (IV) (sulfurous acid) :

SO2 (g) + H2O (l) H2SO3 (aq)

Page 10: Understanding 8.5 Acid deposition

• The main anthropogenic sources of nitrogen oxides are the internal combustion engine, coal, gas, oil-fuelled power stations and heavy industry power generation.

Page 11: Understanding 8.5 Acid deposition

• The combustion temperatures of fuels in these process are very high and oxidation of atmospheric nitrogen occurs forming NO (nitrogen monoxide, nitric oxide or nitrogen(II) oxide) :

N2(g) + O2 (g) 2NO (g)

Page 12: Understanding 8.5 Acid deposition

• NO can be oxidised in the atmosphere to NO2.• Again, the exact nature of the process is

complex but the reaction can be summarised as :

2NO (g) + O2 (g) 2NO2 (g)

Page 13: Understanding 8.5 Acid deposition

• The NO2 can then react with a hydroxyl free radical (HO.) to form nitric (V) acid :

NO2 (g) + HO. (g) HNO3 (g)

Page 14: Understanding 8.5 Acid deposition

• Other reactions can occur and the formation of nitric acid can also be shown as :

4NO2 (g) + O2 (g) + 2H2O (l) 4HNO3 (aq)

Or 2NO2 (g) + H2O (l) HNO2 (aq) + HNO3(aq)