C1 CHEMISTRY LIMESTONE Balanced Equations H H C H Ionic Bonding

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Presentation transcript:

C1 CHEMISTRY LIMESTONE Balanced Equations H H C H Ionic Bonding Definitions Atom – Element – Compound – Mixture – Group 0 or 8 are UNREACTIVE They have a full outer shell of electrons Particles that make up all substances. A substance made up of only one kind of atom. A substance made of different types of atoms joined together. A substance existing of atoms that can be easily separated as they are not joined together. Periodic table arranges elements by ATOMIC NUMBER (proton number/the small one) No charge Max 2 electrons Max 8 electrons E.g. 2,8,8 (Argon) The number of outer shell electrons match the group the element is found in. E.g. Lithium 2,1 is a group 1 element. Protons and neutrons both have a mass of 1 Balanced Equations Used for building Carbonates Decompose when heated = Oxide + CO2 React with acid = Salt + water + CO2 LIMESTONE Calcium Carbonate CaCO3 The number of electrons an atom has effect the way it reacts Limewater The test for CO2 HEAT (thermal decomposition) = CaO Calcium Oxide Covalent Bonding Non-metals sharing elections Ca(OH)2 Or Calcium Hydroxide comes from adding water to CaO Each side should also weigh the same. Nothing is lost and nothing extra is made. H H C H A balanced equation has the same number of atoms of each element on both sides Using Molecules: In this equation, the large number in front of the chemical symbol tells use the molecules needed. e.g. 1 CH4 molecule reacts with 2 O2 molecules Limestone is heated in a Rotary Lime Kiln You then have Cement or Mortar by adding water and sand. If you add crushed rocks you get Concrete Good: More jobs Bad: Destroy habitats and Landscape QUARRYING Would you want to live next to one? Ionic Bonding Metals – Very useful e.g. Copper wires conduct well Most need to be ALLOYED to make them harder Lose or gain an electron Get a charge +/- Attract one another! Metals which are un-reactive are found in their NATIVE STATE e.g. GOLD More reactive metals are found as METALS ORES and need to be EXTRACTED TRANSITION METALS C1 CHEMISTRY Charged particles IONS

Reactivity Series RECYCLING VEGETABLE OIL CRUDE OIL IRON Pure iron is too soft to be useful. Adding small amounts of other elements can improve its properties. This is ALLOYING. IRON + ‘other elements’ STEEL VEGETABLE OIL Can be HARDENED by adding HYDROGEN making them solid at room temperature for things like spreads and margarines To harden you will need: Nickel Catalyst 60oC Hydrogen to be added and break double bonds Are extracted by pressing or distillation Are high in energy Can be used as fuels Are UNSATURATED High Boiling Point So useful for cooking (frying instead of boiling) Gives a different flavour, texture and loads more energy (too much will make you obese) e.g. More easily shaped, harder, resistant to corrosion Unsaturated fats are better for you than Saturated fats RECYCLING CRACKING HYDROCARBONS Make big molecules into small ones! -heat them with steam and a catalyst You can make ETHANOL using ETHENE and STEAM with a catalyst (from crude oil) Non-Biodegradable plastics are BAD! They don’t rot away. Biodegradable plastics will decompose = less rubbish! You can make ETHANOL using YEAST enzymes. (from plants) + CO2 OR Products: Alkanes (used for fuel) + Alkenes (used for plastics, medicines, dyes and explosives) Saves energy Saves natural recourses Less pollution Made from vegetable oils Less harmful to environment CARBON NEUTRAL Lose farming land Disruption of habitats Making Plastics: Small molecules (monomers) added together make new long molecules (polymers) Reactivity Series Test for double bonds: Bromine water (iodine water will also work) Alkenes (with double bonds) go CLEAR! This helps you decide how to extract a metal from its ORE. If its below CARBON it can be reduced in a BLAST Furnace. If its a metal above it CARBON cannot help extract it. CRUDE OIL A mixture of hydrocarbon compounds RENEWABLE ENERGY e.g. ethanol from sugar Test it! Make it useful New polymers are designed to work for specific jobs. SMART POLYMERS can change in different temperatures and light. We are also able to recycle plastics to find more uses for them. Extracting reactive metals You might need to smelt or roast the ore and then use electrolysis to make it pure Hydrogen and Carbon ONLY! Carbon Dioxide made from burning fuels is a GREEN HOUSE GAS adding to GLOBAL WARMING FRACTIONAL DISTILLATION Size effects BOILING POINT Getting clever! Scientist are using bacteria and plants to remove copper from ores where its too small to mine. BIOLEACHING or PHYTOMINING Pure copper Impure copper (copper ore) Filters and CATALYTIS CONVERTERS can be fitted to factories and cars to reduce pollution Cu 2+ You can also get PARTICULATES or Soot! Bad for you and the environment (Global Dimming) Sulfur impurities also burnt cause … Impurities: include gold and silver (can be sold) Electrolysis can be expensive but will help extract Copper, Aluminium and Titanium Alkanes – Saturated hydrocarbons. No double bonds, Maximum Hydrogen, Formula: CnH2n+2 Alkenes – Unsaturated hydrocarbons. Double bonds, Less Hydrogen Formula: CnH2n High temperatures in engines can also cause the nitrogen from the air to form acids too. Burning fuels in plenty of oxygen gives CO2 + H2O COMPLETE COMBUSTION Burning without enough oxygen gives CO (carbon monoxide) + H2O INCOMPLETE COMBUSTION – BAD! Very useful and NON-CORROSIVE (wont rust away)

Earth Structure The Carbon Cycle Earth’s Atmosphere Now OIL DOES NOT DISSOLVE IN WATER Wegener’s Big Idea Earth Structure But they can be spread out in each other to make an EMULSION Alfred Wegener suggested the idea of continental drift (moving plates) but people found it hard to believe, they couldn’t see it and had other ideas like land bridges, sinking continents and the crust shrinking. Also he couldn’t explain HOW it worked. It took fossils and rocks evidence to convince people. (Solid) Adding an EMULSIFIER stops the oil and water separating – it will also improve texture Emulsions are used in: Food Cosmetics Paints e.g. Mayonnaise, salad dressings & ice creams Death & Decay Yummy! All our resources come from the crust, oceans and atmosphere. The crust is made up of tectonic plates which are always moving.. Very very very .. Slowly. Experimental Variables Independent Variable – the one I CHANGE Dependent Variable – the one you RECORD Control Variables – the ones you KEEP CONSTANT (the same) Earth’s Early Atmosphere Radiation in the mantle causes CONVECTION CURRENTS which move the plates Formed by volcanoes added CO2, Water and Nitrogen Which cooled and condensed into oceans Plants then appeared and changes CO2 to oxygen! (photosynthesis) When tectonic plates meet and collide or rub against one another we get natural disasters Calculating an average Add up all your results (except any anomalies you are leaving out) 10 + 11 + 12 + 14 = 47 Divide your answer by the number of values you added together. Here 4 values were used.. So 47 4 = 11.75 Just a reminder! The Primordial soup experiment suggested that life started with a lightening spark, others suggested a meteorite or the deep ocean event. Without a time machine we just don’t know what started life on earth! We don’t know when this will happen so we cannot predict these events The Carbon Cycle Takes a very long time! Earth’s Atmosphere Now Answering Evaluation questions You must give a balanced argument if you can! 2 reasons why you might agree or think something is good. 2 reasons why you might disagree or think something is bad. And a conclusive statement. (your end opinion) ALWAYS read the information you have been given. Sometimes the answer is hidden in the question. Death & Decay Formation of Fossil Fuels Mostly oxygen and nitrogen The Problem area Death & Decay Respiration 20% Food chain... Respiration of microorganisms Burning Fossil Fuels Carbon in the atmosphere has increased because we now burn more fossil fuels! Is very quick! Respiration Gases in the air can be separated by fractional distillation for use in industry The Carbon cycle: Shows the movement of carbon in and out of the atmosphere 80% Photosynthesis Respiration Returning Carbon to the Atmosphere