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C1 Revision
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The periodic table of elements
The periodic table of elements shows us metals (left) and non-metals (right) Each group has similar chemical properties
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Atoms The smallest particle of an element
Atoms have the same amount of positive and negative charges so they are neutral Type of sub-atomic particle Relative charge Proton +1 positive Neutron 0 (neutral) Electron -1
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Mass number Atomic number No. of neutrons = mass no. – atomic no.
Atomic number = number of protons No. of protons = no. of electrons The mass number = no. of protons + neutrons Therefore No. of neutrons = mass no. – atomic no.
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Arrangement of electrons
Electrons are arranged around the nucleus of atoms in shells The first shell can hold up to 2 electrons The second shell can hold up to 8 electrons The third shell can hold up to 8 electrons Then the fourth shell fills up Lithium 2,1
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Electrons and the periodic table
Elements in the same group all have the same number of electrons in their outer shell. This means that they share similar properties Group 1 elements all have 1 electron in the outer shell – they are all very reactive Group 0 elements (noble gases) have full outer shells – they are unreactive
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Group 1 – alkali metals Alkali metals are all soft, stored in oil, low density, react with oxygen and all react violently with water and form alkaline (pH>7) solutions. Lithium + water lithium hydroxide + hydrogen Sodium + oxygen sodium oxide
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Forming compounds When atoms of different types of elements join together they form ‘compounds’ When metals react with non-metals they lose or gain electrons & form ions Metals lose electrons and become positive ions (+) Non-metals gain electrons – negative ions (-) Oppositely charged ions are attracted to each other and form an ionic bond
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Forming compounds when non-metals react with non-metals they share electrons This is called covalent bonding A covalent bond is a shared pair of electrons solid line Cl – Cl Cl covalent bond
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calcium carbonate calcium oxide + carbon dioxide
Chemical equations These show us the reactants (on the left) and the products (on the right) calcium carbonate calcium oxide + carbon dioxide CaCO3 CaO CO2 No atoms are lost or made in the reaction and so the total mass of the products is equal to the total mass of the reactants- conservation of mass
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Limestone Calcium carbonate (CaCO3)
Limestone can be heated with clay to make cement Cement is mixed with sand and water to make mortar Cement is mixed with water, sand and crushed rock to produce concrete Useful as a building material but is damaged by acid rain When carbonates react with acids, carbon dioxide is given off as well as making a salt and water.
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1. Calcium carbonate calcium oxide + carbon dioxide
Limestone reactions 1. Calcium carbonate calcium oxide + carbon dioxide CaCO3 CaO CO2 2. Calcium oxide + water calcium hydroxide Calcium hydroxide is an alkali ( Limewater). It can be used to neutralise acids. It is used by farmers to neutralise acidic soil, and to neutralise acidic industrial gases. 3. Calcium hydroxide + carbon dioxide calcium carbonate + water This is the test for carbon dioxide.
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Magnesium carbonate magnesium oxide + carbon dioxide
Other Carbonates The carbonates of magnesium, copper, zinc, calcium and sodium can be thermally decomposed too They always form a metal oxide and carbon dioxide Magnesium carbonate magnesium oxide + carbon dioxide
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Advantages of using limestone and producing building materials form it
Disadvantages Can build houses and roads from it Neutralise acidic soil Neutralises sulphur dioxide in power station chimneys Jobs for local people Landscape can be restored after use Makes the landscape ugly Dust pollution Sound pollution from blasting Destroys animal habitats To make cement needs energy which is got from burning fossil fuels- global warming
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Advantages of limestone + its products over other materials
Disadvantages Widely available Cheaper than granite/marble More hardwearing than marble Concrete can be poured into moulds Doesn’t rot like wood Doesn’t corrode like metals Can be reinforced with steel Concrete is ugly looking Concrete has a low tensile strength
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Extracting metals Metals are found naturally in the Earth’s crust
They are often chemically combined with other elements – this is called the ore Whether it is worth extracting a metal depends on: 1. How easy it is to extract it from its ore How much metal the ore contains
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Extracting metals electrolysis carbon reduction Other methods
The way we extract a metal depends on its place in the reactivity series Most reactive Least reactive Potassium Sodium Calcium Magnesium Aluminium Carbon Zinc Iron Tin Lead Copper Silver Gold Platinum electrolysis carbon reduction Other methods
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Copper Pure copper is a good conductor of electricity, does not react with water and can be shaped easily Copper can be removed from its ore by smelting ( heating in a furnace) The copper produced is purified using electrolysis This involves passing an electrical current through a copper solution Metal ions are positive so pure copper forms at the negative electrode
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Copper Copper-rich ores are running out
New methods are used to extract copper from low grade ores Phytomining – using plants to extract copper Bioleaching – using bacteria to extract copper Scrap iron can be dipped into a solution of a copper salt to extract copper ( displacement) Solutions can be electrolysed
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Aluminium Aluminium is a very low density metal
Because it is higher than carbon in the reactivity series it is extracted using electrolysis Electrolysis is very expensive because lots of energy is needed to get temperatures high enough to melt the ore and electricity is needed to split the ore This is why we recycle aluminium
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Titanium Titanium is very strong and has a very high melting point
It is used for replacement hip joints It cannot be reduced using carbon because it is more reactive It is reduced (using sodium or magnesium) but this process is very complicated and has lots of steps and large amounts of energy are needed which means the titanium is very expensive
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Iron (III) oxide + carbon iron + carbon dioxide
Iron ore contains iron combined with oxygen Iron is extracted using carbon reduction It is heated in a blast furnace Iron (III) oxide + carbon iron + carbon dioxide Iron straight from the blast furnace still contains some impurities (it is about 96% iron) – it is very brittle and is called cast iron. It can be used to mould different shapes Removing the impurities gives us pure iron – this is too soft for most uses
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Iron To make iron stronger we can add small amounts of other elements
A metal that is mixed with other elements is called an alloy Low carbon steel is easily shaped High carbon steel is hard Stainless steels are resistant to corrosion
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Why recycle metals( or plastics)
Recycling does NOT involve using up valuable limited resources Is cheaper than extraction due to needing less energy NO MORE damage on the landscape Stops filling up landfill sites
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alloys Steel is an alloy of iron containing carbon
Alloys are harder than pure copper, gold iron and aluminium. The “added” atoms distort the layers
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Crude oil Crude oil is a mixture of a large number of compounds. They are NOT chemically combined together We separate the different compounds by fractional distillation This involves separating the different fractions depending on their boiling points
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Fractional distillation of crude oil
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Crude oil Crude oil contains compounds made of only hydrogen and carbon – hydrocarbons Most of the hydrocarbons are alkanes The general formula for alkanes is CnH(2n+2) Alkanes are saturated hydrocarbons because they only have single C-C bonds Propane C3H8
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Monkeys Eat Peanut Butter
AlkAnes Methane Ethane Propane Butane Monkeys Eat Peanut Butter
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e.g. Propane + oxygen carbon dioxide + water
Combustion When hydrocarbons are burned they react with oxygen(OXIDATION) & release energy complete combustion – plenty of oxygen e.g. Propane + oxygen carbon dioxide + water Incomplete combustion happens when there is not enough oxygen – carbon monoxide (CO) (a toxic gas) is produced instead of carbon dioxide
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Products of combustion
Pollutant Environmental problem Sulphur dioxide Acid rain Oxides of nitrogen Carbon dioxide Global warming particulates Global dimming Sulphur can be removed from the fuel before it is burned. Sulphur dioxide is removed from the waste gases before it is released e.g power stations
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Cracking After fractional distillation of crude oil, we are left with lots of less useful long-chain hydrocarbons Long-chain hydrocarbons can be broken down into smaller ones by a process called cracking This involves heating the fraction until it vapourises then passing it over steam or a hot catalyst The products always include smaller alkanes( used as fuels) and alkenes
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Hexane butane + ethene
Cracking hexane (800°C + hot catalyst) Hexane butane + ethene C6H14 C4H10 + C2H4
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Alkenes ( double “e” double bond)
Ethene C2H4 Propene C3H6 Butene C4H8 Alkenes have the general formula CnH2n Alkenes are Unsaturated as they have a double bond
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Testing alkanes and alkenes
Bromine water reacts with alkenes and forms a colourless solution Bromine water stays orange in alkanes
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Biofuels This includes biodiesel and ethanol which are made from plant material They are made from renewable resources Almost carbon neutral But plant crop may be destroyed due to poor weather conditions Using up land that should be growing crops to feed us
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Polymers Alkenes molecules can be used to make plastics
Small molecules are called monomers Lots of monomers joined together make polymers monomers polymer
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A repeating unit of poly chloroethene (PVC)
Polymers n A repeating unit of poly chloroethene (PVC)
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New polymers New plastics with special properties are being developed
Dental fillings, waterproof fabrics and light sensitive plasters are made with special polymers Smart polymers such as shape memory polymers ‘remember’ their original shape and will return to it when heated e.g. stitches closing a wound using body heat
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Plastic waste Many polymers are not biodegradable – this means microorganisms cannot break them down New biodegradable polymers have been developed using starch and plant products that microorganisms can break down This reduces the amount of plastics in landfills
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Ethanol This is the type of alcohol found in alcoholic drinks
Its formula is C2H5OH Ethanol can be made by fermentation of sugar from plants with yeast Glucose (sugar) ethanol + carbon dioxide Ethanol can also be produced by reacting ethene (from cracking crude oil) with steam using a catalyst Ethene + steam ethanol
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Vegetable oil Some fruits, seeds and nuts are rich in oils that can be extracted The plant material is crushed and the oil is removed by pressing or distillation Vegetable oils provide nutrients and have a high energy content Vegetable oils have higher boiling points than water so foods can be cooked at higher temperatures than by boiling Food cooks faster and has different flavours Food cooked in vegetable oil releases more energy when it is eaten but has a higher calorie content
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Making Margarine Most modern margarines are made from plant oils. The oil is heated and hydrogen is pumped through it. This is called hydrogenation Vegetable oil + hydrogen → margarine Some of the carbon-to-carbon double bonds in the plant oils are broken and extra hydrogen atoms are added. This hardens the oil to make it a solid at room temperature (its melting point has been raised.. This is useful as spreads or for use in cakes and pastries. Nickel catalyst 60 C
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Emulsions Oil does not mix with water
An emulsifier is a special molecule that can be used to mix them and stop them separating creating an emulsion Emulsifiers work by having one end that dissolves in water (hydrophilic) and one that dissolves in oil (hydrophobic) Emulsions include ice cream and mayonnaise
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Structure of the Earth Crust: thin Mantle: thickest section
Core: middle The Earth is made up of many layers The Earth is surrounded by the atmosphere
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Where did the mountains come from?
Before Wegener developed his theory, it was thought that mountains formed because the Earth was cooling down, and in doing so contracted. This was believed to form wrinkles, or mountains, in the Earth’s crust. If the idea was correct, however, mountains would be spread evenly over the Earth's surface. We know this is not the case.
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Alfred Wegener Continental drift.
Wegener proposed idea that the continents were all joined together at one time and slowly moved apart His evidence included: Jigsaw pattern of coastlines Identical fossils and ages on the coasts of south America and Africa Matching rock types and ages But how did they move? He couldn’t explain it and many other scientists believed they were locked in place and maybe there were land bridges in the past that have now gone
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Tectonic plates The crust and mantle are broken up into large pieces (tectonic plates) They move a few centimetres per year due to convection currents caused by radioactive reactions in the mantle Earthquakes are caused when plate boundaries meet and push together, mountains are also formed here.
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The modern atmosphere The Earth’s atmosphere has been the same for about 200 million years
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Air Air is a mixture of gases with different boiling points. These can be separated out using fractional distillation
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The early atmosphere About 4.5 billion years ago when the Earth formed volcanoes released carbon dioxide, water vapour and small amounts of ammonia & methane – this formed the first atmosphere( similar to Venus and Mars) As the Earth cooled the water vapour condensed, fell as rain & this formed the first oceans When life evolved plants used the carbon dioxide & released oxygen during photosynthesis
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How did it all begin( maybe)?
The Miller-Urey experiment simulated a lightning spark in a mixture of gases of the early atmosphere A week later, more than 2% of the carbon in the system had formed compounds from which proteins in living cells are made
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Carbon Most of the carbon dioxide from the Earth’s early atmosphere has been taken up by plants, which were eaten by animals This means that most of the carbon is ‘locked’ in sedimentary rocks and in fossil fuels Carbon dioxide also dissolved in oceans Over the past 200 million years the amount of carbon dioxide in the atmosphere has not changed much – however we are now burning fossil fuels and releasing carbon dioxide
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