composition of clean air: 78% nitrogen, 21% oxygen, 0.96% noblegases mainly argon, water vapour and other gases, 0.04% carbondioxide
uses of gases: (1) nitrogen: boiling point (-196 °c) - considered as an inert gas as its triple bond is relativelystrong and hard to break - reactions involving nitrogen as a reactant have relativelyhighactivation energies
uses of gases:
(2) oxygen: boiling point (-183 °c)
essential for combustion
used to support patients with breathingdifficulties
used as oxidiser in welding that joinspieces of metals together strongly
uses of gases:
(3) argon: boiling point (-186 °c)
provide inertenvironment for hightemperature processes (e.g. in lightbulbs and thermalpurification of copper and steel) - separation of liquid air: fractionaldistillation, since nitrogen has the lowestboiling point, it is boiled off and collected first
air pollution is the introduction of unwanted and harmfulchemicals into the atmosphere
cause: combustion of fossilfuels and volcaniceruptions 2. nitrogen oxide: NO- colourless and odourless, NO2- redbrown, pungentsmell
cause: vehicle combustionengines and lighting
effect: SO2 causes breathing difficulties in humans and animals, sulfurdioxide and nitrogenoxides react with oxygen to form acidic compounds which dissolves in rain water to form acid rain. --> it kills plants and aquatic life, corrodes building and structures made from limestone, marble and metal
(air pollutants & harmful effects) 3. carbon monoxide: colourless and odourless, very toxic
cause: incomplete combustion of carbon-based fuels
effect: binds irreversibly with haemoglobin--> less oxygen transported around the body --> loss of consciousness and death
cause: anaerobic bacterial decay of organic substances and waste gases from cattle
effect: major greenhouse gas which causes globalwarming
(air pollutants & harmful effects)
5. unburnt hydrocarbons (CxHy): colourless and naturallyodourless, may be pungent due to fueladditives
cause: vehicle combustionengines
effect: eye and respiratorytractirritation, reacts with nitrogenoxide in presence of sunlight to form smog (brown haze) --> smog produces ozone, SO2 and NO2
cause: lighting, reactions between oxygen and sunlight in upper atmosphere, reaction between unburnt hydrocarbons and nitrogen oxides in presence of sunlight in lower atmosphere
2) flue gas desulfurisation: removes a significant proportion of SO2 from flue gas produced from wasteincinerators
wetscrubbing (CaCO3 mixed with water to form slurry)
CaCO3 (s) + SO2 (g) → CaSO3 (s) + CO2 (g)
(calcium sulfite further oxidised to form calcium sulfate) 2CaSO3 (s) + O2 (g) → 2CaSO4 (s)
(calcium sulfate hydrated - known as gypsum) CaSO4 (s) + 2H2O (l) → 2CaSO4 . 2H2O (s)
gypsum (hydrated calcium sulfate) is used to make drywall, fertilisers, plaster for sculptures and casts that stabilise fractured bones. It is essential in making tofu
(control of air pollution)
(3) low sulfur fuels: in vehicles
excess sulfur can be removed from fossil fuels by treating it with hydrogen gas producing hydrogensulfide
(control of air pollution)
(4) liming
carbonate is added to soil and water bodies to remove excessacid from the acid rain
however, this process is expensive and effects are temporary
the ozone layer: reduces the amount of UVradiation from the sun that reaches the Earth's surface.
it is found in the stratosphere
3O2 (g) →(reversible reaction) ← 2O3 (g) (ozone molecules break up to reformoxygen when they absorb UVradiation)
depletion of ozone layer:
chloroflurocarbons (CFCs): found in aerosol propellants and refrigerants. They interact with UV radiation to produce chlorine atoms which react with ozone
chlorine atoms present at the start of the reaction is regenerated at the end of the 2nd reaction. thus, more O3 molecules are reacted with. (1Cl atom can destroy many O3 molecules)
this can cause skin cancer rates to increase
the carbon cycle describes a set of processes that regulates the amount of CO2 in the atmosphere
the balance between processes that produces CO2 (combustion and respiration) and the processes that removes CO2 (photosynthesis) regulates the amount of CO2 in the atmosphere
global warming is the increase in the averagetemperature of the earth's surface due to increasing amounts of greenhouse gases in the atmosphere
causes of the greenhouse effect:
some solar radiations reaches the atmosphere and passes through it (heat)
combustion of fossil fuels (releases greenhouse gases) → CO2 & CH4
deforestation
(climate change and other consequences)
change in rainfall patterns: leads to desertification of fertileland thus decreasing the amount of food produced globally
(climate change and other consequences)
2. frequent and severe heat wave : leads to high temperatures and possible heat injuries, destructive wildfire (could destroy ecosystems)
(climate change and other consequences)
3. tropical storms ( increase in frequency and intensity of extreme weathers): leading to propertydamage, liveslost, can permanently decrease the fertility of farmland near the coast due to saltwater deposition
(climate change and other consequences)
4. ocean warming and acidification:
coral reefs bleached, habitats lost
fish population depletion
acidified water dissolve the shells of crustaceans
(climate change and other consequences)
5. glacialretreat and melting of polar ice caps:
glacier-fed river levels would change
sea levels would rise, and permanently flood coastal areas
climate - stabilising oceans currents would be disrupted
fossil fuels are from decayedplants and animals millions of years ago. they are mainly organiccompounds containing hydrocarbons (carbon and hydrogen)
combustion is an exothermic process where the thermal energy generated can be converted to other forms of energy
(fossil fuels)
natural gas: mainly methane
colourless and odourless
CH4 (g) + 2O2 (g) --> CO2 (g) + 2H2O (g)
cleanest form of fossil fuel
liquefied before being transported to consumers (it is safer) (gas - liquid reducevolume by 600 times)
an additive like tetrahydrothiophene (THT) has a pungent smell and added to natural gas to alert us in cases of a gasleak
(fossil fuels)
2. crude oil: petroleum
contain mixture of hydrocarbons
from drilling of underground reservoirs
different hydrocarbons in crude oil burns at differenttemperatures and are miscible
it is separated into useful fractions by fractionaldistillation
(fossil fuels)
naturalgas and crudeoil are considered non-renewablesources of energy. there are limitedamounts of these sources and they cannot be replaced quickly enough to keep up with our rate of use.
crude oil have hydrocarbons with 1 - 70carbon atoms per molecules
more carbon atoms in each molecule: higher boiling point, moreviscous (thick and stickyconsistency)
less carbon atoms in each molecule: lower boiling points, lessviscous and burns more easily
(separation of crude oil)
crude oil heated in furnace to 400°c
vapour passed into fractionatingcolumn
fraction with highest boiling point is collected last and condenses at hightemps --> collected at bottom of column
fractions with lowest boiling points condenses at lowertemperatures thus, they riseup before they condense and are collected at the top
(crude oil fractions)
petroleum (70°c)
naphthalene (120°c)
kerosene (170°c)
diesel (270°c)
lubricatingoil
fuel oil
bitumen
90% used as fuels: generate thermal energy and electricity to power householdappliances, motorvehicles and industrialactivities
10% used as petrochemicalfeedstock: manufacture of plastic, detergent, medicine, fertilisers, pesticides, syntheticrubber (dailyproducts)
conversing crude oil --> due to limited supply
take publictransport, drive smaller cars consuming lessfuel
use solar energy, biofuels, nuclear energy (uranium) --> risk of harmfulradiation from nuclear plants
electric vehicles
biofuels are alternativerenewableenergysource to crude oil and natural gas
ethanol obtained fermentation of sugar in sugarcaneplants or corn --> regrown quickly (making it a renewable energy source)
bioethanol is more environmentallysustainable as sugarcane absorbedCO2 when it grows during photosynthesis thus, offsetting the CO2 production when it is burnt