Atmospheric Chemistry Flashcards

1
Q

how far is the atmosphere

A

extends about 100km

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2
Q

how far is thin air

A

6 km up the air is too thin to breath

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3
Q

what does the atmosphere consist of

A

mixture of gases
similar all over the earth due to mixing
1. caused by rotation of earth
2. heating of earth by sun

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4
Q

composition of earth

A
nitrogen 
oxygen
carbon dioxide 
noble gases
water 
pollutants
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5
Q

production of oxygen

A
  1. natural production
    made by green plants using photosynthesis
    6CO2 + 6H2O = C6H12O6 + 6O2
  2. industrial production
    fractional distillation of liquid air
    a) scrub air - remove water and dust
    b) liquefy - compressing then cooling then releasing
    c) separate - let liquid warm up gases will boil of when their boiling point is reached
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6
Q

boiling points

A

Bigger atoms (molecules) have higher boiling points due to bigger attraction between molecules caused by Van der Waal’s Forces

0C = K - 273
K = oC + 273
[ -273 0C = Absolute Zero]

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7
Q

uses of oxygen

A
  1. oxygen in hospitals
  2. cellular respiration
  3. combustion
  4. steel making
  5. in rockets
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8
Q

nitrogen

A

unreactive
needs lots of energy to break n triple bond n

lightning can provide this forming NO2
N2 + 2O2 = 2NO2

NO2 dissolves in rain to form nitrites and nitrates
H2O + 2NO2 = HNO2 + HNO3

HNO2 = nitrites
HNO3 = nitrates
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9
Q

uses of nitrogen

A
  1. Haber process - making ammonia
  2. liquid nitrogen to freeze pizzas
  3. filling crisp packets - prevent crushing
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10
Q

nitrogen cycle

A
atmospheric nitrogen 78 %
nitrification 
denitrifying bacteria 
nitrates in soil 
death and decay 
absorbed by plants
plants 
death and decay
animals 
eaten as food
death and decay and excretion
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11
Q

noble gases

A

He - filing airships
Ar - filing light bulbs
Ne - neon light

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12
Q

inorganic carbon compound

A

co produced by incomplete combustion
co is a neutral oxide
no effect on universal indicator

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13
Q

types of oxide

A

Acidic
neutral
basic

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14
Q

types of oxide

A

Acidic
neutral
basic

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15
Q

CO2
PRODUCED
USED

A

produced - respiration, burning, rotting, fermentation
used in - photosynthesis, fire extinguishers, fizzy drinks

carbon dioxide is an acidic oxide
CO2 + H2O -> H2CO3
carbonic acid is a weak acid - it turns Universal Indicator yellow

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16
Q

carbon cycle

A
atmospheric CO2 0.03%
plants 
photosynthesis 
animals 
eaten 
respiration 
respiration 
solution 
oceans
death and decay 
fossil fuels 
carbonate rocks
roasting limestone
17
Q

greenhouse gases

A

CO2
CH4
CFCs
H2O

levels of CO2 are getting too high
due to increase in use of fossil fuels, rainforest burning, deforestation
CH4 from oil fields, rubbish dumps and cattle belching

more violent weather
rising sea levels

18
Q

pollution

A

Addition of any damaging substance to the environment

19
Q

atmospheric pollution example

Acid rain formation and effect

A
SULPHUR DIOXIDE S02
from- volcanoes 
fossil fuel combustion 
industry 
S + O2 = SO2

Acid rain has a pH of less than 4.5
SO2 dissolves in rainwater to form H2SO3 [sulphurous acid]
SO2(g) + H2O(l) = H2SO3(aq)

Sulphurous acid then reacts with O2 in air
H2SO3(aq) + ½ O2(g) = H2SO4(aq)
[sulphuric acid]

causes

  1. corrosion
  2. health effects
  3. death of animals
  4. death of plants
20
Q

Nitrogen Dioxide NO2

A

N2 generally unreactive

N2(g) + O2(g) = 2 NO(g)
[nitrogen monoxide - colourless gas]
NO(g) + 1/2 O2(g) = NO2(g)
[nitrogen dioxide - brown gas]
2 NO2(g) + H2O(l) = HNO2(aq) + HNO3(aq)

Nitrous acid Nitric acid

21
Q

Other Pollutants

A

Lead and lead compounds (Pb)
Replaced by Volatile Organic Chemicals [VOC’s] e.g. benzene
VOC + O2 + UV => O3 (poisonous)

22
Q

CFCs

HCFCs

A

If we change a Cl in CCl4 for a F then we get CFCl3 a ChloroFluoroCarbon a CFC

HCFCs = HydroChloroFluoroCarbons

23
Q

ozone layer

A
O3
formed in stratosphere
25 - 50 km up
Absorbs harmful UV radiation from sun
UV burns and causes cancer.
24
Q

Formation of Ozone

A

O2 = (UV) O radical + O radical
oxygen splitting called photodissociation {breaking of a bond using light}

O radical + O2 = O3
Most of the oxygen radicals [atoms] formed in this way react with oxygen molecules to form ozone again.
In this way even more harmful UV is absorbed and ozone is not depleted

some ozone lost due to oxygen radicals react with ozone form oxygen
O radical + O3 = 2O2

25
Q

CFC’s

A

Chlorine radicals are produced by CFCs (ChloroFluoroCarbons)
Contain Chlorine, Fluorine and Carbon
Used as aerosol propellants, fire extinguishers
residence time of 100 years

26
Q

CFCs and UV

A

CCl3F => UV CCL2F radical + CL radical
O3 + CL radical => O2 + CLO radical
CLO radical + O radical => Cl radical + O2

One Cl atom can destroy tens of thousands of O3 (by a chain reaction)

27
Q

Other Ozone Destroyers

A

Nitrogen monoxide [NO]

O3 + NO = O2 + NO2

28
Q

Helpers

A

Methane (CH4) a serious greenhouse gas helps use up chlorine atoms

Cl radical + CH4 => CH3 radical + HCL
Gets rid of chlorine atoms [radicals]