Monitoring The Environment (1) Flashcards
Topic 1
What are erratic weather patterns?
Climate changes may lead to more erratic weather patterns, increasing the severity and frequency of natural phenomena.
Bushfires, cyclones, droughts and floods
Climate change may affect patterns of cropping in agriculture. Droughts, flooding, unusual weather patterns
What is permafrost?
Permafrost is made of a combination of soil, rocks and sand that are held together by ice.
The soil and ice in permafrost stay frozen all year long.
Some building are built on top of permafrost.
Permafrost contains frozen organic materials.
What are the 3 types of solar radiation?
Solar radiation entering Earth’s atmosphere consists of:
- Infrared radiation (IR)
- Visible light (ROYGBIV)
- Ultraviolet radiation (UV)
What is the greenhouse effect?
The Earth’s surface absorbs short-wave radiation (UV and visible light) from the sun and re-emits it as longer wavelength (and lower energy) infrared radiation (IR).
Why is the greenhouse effect needed?
Radiation (visible and ultraviolet) from the sun passes through the atmosphere and heats the earths surface.
The radiation is then re-emitted as longer wavelength infrared radiation.
Greenhouse gases in the lower atmosphere absorb some of this re-radiated energy.
The absorbed energy is reradiated to other molecules in the atmosphere, out to space and back to the surface of the Earth.
This creates a thermal balance with the amount of thermal radiation entering the atmosphere in equilibrium with the amount of thermal radiation emitted back into space.
This is a natural process, called the natural greenhouse effect, which keeps the troposphere (the lowest layer of Earth’s atmosphere) warm enough for our survival
What molecules can absorb infrared radiation?
Only molecules with polar bonds can absorb IR.
Polar bonds can stretch or bend asymmetrically, absorbing and re-radiating thermal radiation.
Name the different greenhouse gases.
CO2, N2O, H2O vapour and CH4 have polar covalent bonds which stretch and bend to absorb the IR.
These are greenhouse gases
N2 and O2 do not contribute to greenhouse effect.
H2O absorbs more energy per molecule than any other greenhouse gas!
What are polar bonds?
Polar bonds are covalent bonds between atoms with different electronegativities, leading to unequal sharing of valence electrons. This leads to the formation of a positive and negative dipole.
Explain why CO2 molecules are nonpolar, even though it has polar bonds.
CO2 is a linear molecule. There are no 2 distinct regions of charge as the dipoles cancel each other out to yield a molecule with no net dipole.
What is causing the increase in greenhouse gases?
- Carbon dioxide (CO2): Burning of fossil fuels, clearing of rainforests. Carbon dioxide makes a 50% contribution to global warming. Fossil fuels are made of long hydrocarbon chains.
- Methane (CH4): Agricultural activity and landfill.
- Nitrous oxide. Fertilizer use and internal combustion engines.
- Chlorofluorocarbons (CFCs): Are very efficient greenhouse gases. CFCs were previously used in everyday products like aerosols, packaging and refrigerators. They are now banned in 197 countries because of the damage they can do to the ozone layer.
What does anthropogenic mean?
Anthropogenic: changes in nature caused by human activity.
How does ocean acidification occur?
Human activities contribute to rising CO2 emissions. e.g. transportation, industry, use of electricity.
The ocean absorbs CO2 from the atmosphere.
Too much dissolved CO2 can harm marine organisms and ecosystems.
When carbon dioxide is absorbed by the ocean:
Carbon dioxide + Water → Carbonic Acid
CO2(g) + H2O(l) → H2CO3(aq)
Acids are proton donors
∴ H2CO3(aq) + H2O(l) → HCO3- + H3O+
Then: HCO3-(aq) + H2O(l) → CO32- + H3O+
H3O+ = Hydronium ions are formed —> pH decreases (acidic)
What is the impact of ocean acidification?
What happens to the pH as more carbon dioxide is released into the water?
The release of hydronium ions increases the acidity/decreases the pH of the ocean.
Over the past 250 years (since the industrial revolution) the pH of the ocean has dropped from 8.2 to 8.1.
This is a significant change since the pH scale is logarithmic (around 25 – 30% increase in H+ concentration).
This acidic environment can disintegrate shells.
Calcium carbonate, CaCO3, is the main building block of sea shells, coral, molluscs and crabs
Organisms such as coral, shells and crabs build their shells and skeletons from the calcium ions and carbonate ions in the ocean.
Ca2+(aq) + CO32-(aq) → CaCO3 (s)
As the pH of the ocean decreases (H+ concentration increases), the additional protons cause the dissolution of the solid calcium carbonate, weakening the shells and skeletons and also making it harder for them to build shells and skeletons.
What is photochemical smog?
Is a type of air pollution formed during the day over large cities with polluted air
Its characteristic brown haze is due to the presence of nitrogen dioxide within the air.
Typically, common in larger cities with warmer weather.
Gaseous Nitrogen (𝑁_2) is required to produce the nitrogen dioxide in photochemical smog.
78% of the air within the troposphere contains 𝑁2.
The triple bond leads to an incredibly stable structure. Can be broken when subjected to high energy.
Once a high enough energy source has been supplied (either natural or anthropogenic), Nitrogen reacts with atmospheric oxygen to produce nitric oxide (𝑁𝑂)
N2 (g) + O2 (g) → 2NO(g)
This can undergo further reaction with atmospheric oxygen to form nitrogen dioxide (𝑁𝑂_2)
2NO + O2 (g) → 2NO2 (g)
NO2 can undergo a further photochemical (a chemical reaction initiated by light) decomposition reaction.
𝑁𝑂2 (𝑔) → (UV light) –> NO(𝑔) + 𝑂^.
Highly reactive oxygen radicals 𝑂^. (oxygen with one unpaired electron) can then undergo further reactions with atmospheric oxygen gas to produce ozone:
𝑂^. + 𝑂2 (𝑔) → 𝑂3(𝑔)
Ozone and nitrogen oxides act as pollutants within the atmosphere
What conditions are required for photochemical smog?
To produce photochemical smog a few conditions are required:
- High concentration of pollutants (large cities with lots of motor transport, industrial area or high population density)
- Sunlight (for photochemical reactions)
- Still conditions (wind may disperse pollutants)
- Temperature inversion (Cool at the surface and hot air further up) (stops reactants from dispersing)