Hi Tara. Topic 1 is the foundation topic of 0680 and it is also the longest, so it is worth knowing up front what shape it is. It has two halves that look different but are marked in exactly the same way. The first half (1.1 to 1.3) is about solid resources — rocks, ores and minerals: where they come from, how we dig them up, what that does to a place, and how a country makes them last. The second half (1.4 to 1.6) is about energy resources — where fossil fuels came from, the alternatives, how each one actually turns into electricity, and what makes demand for energy go up.
Here is the thing that will earn you the most marks in this topic, and it has nothing to do with rocks. Look at how many objectives begin with the word “Discuss the benefits and limitations of…”. There are four of them in Topic 1 alone: 1.2.6, 1.3.4, 1.4.4 and 1.6.2. Those are the 6-mark and 8-mark questions. Cambridge is politically neutral and the mark scheme is built to reward a candidate who gives both sides properly and then makes a judgement. A candidate who writes six lines against mining and one line for it does not get 6 marks — she gets about 3, because half the mark scheme is untouched. So every time you meet a “discuss” table in this guide, learn it as a pair of columns, not as an opinion.
The second thing: the definitions in this topic are given to you word for word in the syllabus, which means they can be asked back word for word. Ore, permeability, finite resource, sustainable management of resources and fracking are all one-mark gifts if you have them exactly, and all one-mark losses if you paraphrase them into something vaguer. They are boxed in yellow throughout. Learn those five sentences before you learn anything else in Topic 1.
And the third: two things in here are ordered chains — the rock cycle and the formation of fossil fuels. Chains are marked step by step, in order. If you write the steps out of order you lose the sequencing marks even when every word is correct. So they are taught as chains and then drilled as chains.
Every question in 0680 opens with one of these, and each one is asking for a different shape of answer. Writing a good explanation when the paper said “state” wastes time you need later; writing a bare fact when it said “explain” caps you at one mark. Four of these are used constantly on Paper 2 and are easy to miss: identify, state, calculate and compare.
| Command word | What the answer looks like |
|---|---|
| State | A short fact or a definition, with no reason and no example. One line is a complete answer. If the syllabus gives you the wording — ore, permeability, finite resource, sustainable management, fracking — give it back word for word. |
| Identify | Pick the thing out of the source in front of you. This is the standard opener on a source-led question, and the answer is a name, a letter, or a single value read off a graph, a table or a map. Do not explain it and do not add a second answer as insurance — a wrong extra can cancel a right one. |
| Describe | Say what happens or what you can see, in order where there is an order. For a figure, describe the trend and quote figures from the source as you go. No reasons: the reasons belong to explain. |
| Explain | Give the reason. Aim to get the words because and so that into every explain answer — if neither word fits anywhere in what you have written, you have probably described instead. |
| Calculate | Work out a number. Show the working on its own line, and keep the unit with the answer. For a percentage change, divide by the starting value. Percentage points (34 − 22 = 12) are not the same thing as a percentage change (12 ÷ 22 = 55 %). |
| Compare | Both things in the same sentence, with similarities and differences, and figures where the source gives them. “P generates 80 % from fossil fuels whereas R generates 8 %” is a comparison. Two separate paragraphs, one about P and one about R, are two descriptions, and comparison marks are usually reserved for the linking word — whereas, compared with, both. |
| Suggest | Apply what you know to a situation you have not met before. There is no single expected answer; anything sensible that fits the context and uses the material counts. This is the AO3 skill, and it is what Paper 2 is mostly made of. |
| Discuss | Two columns — benefits and limitations — then a judgement that says who gains, who bears the cost, and over what timescale. A one-sided answer leaves half the marks untouched however well it is written. |
| Evaluate | The highest of the nine. Weigh the evidence on both sides and reach a supported judgement. What is being marked is the weighing, not which side you land on. |
Three families, three ways of being made
Every rock on Earth belongs to one of three families, and the family name tells you how it was made rather than what it looks like. That is the useful way to hold it: igneous rocks froze from molten rock, sedimentary rocks were stuck together from bits, metamorphic rocks were changed in the solid state by heat and pressure. Cambridge names seven rocks and only seven, so you can afford to know each one properly.
Igneous: granite and basalt
Igneous rocks form when molten rock cools and crystallises. The single fact that carries the marks is that crystal size records cooling rate. Slow cooling gives the atoms time to arrange themselves into big crystals; fast cooling freezes them before they can, so the crystals are tiny.
Granite forms when magma cools slowly, deep underground, insulated by the rock above it. The result is large, easily visible interlocking crystals — you can see the individual pink, white and black grains with the naked eye. Because the crystals interlock, granite is hard, strong and impermeable, which is why it is quarried for building stone, kerbstones and worktops.
Basalt forms when lava cools quickly at the Earth's surface, after a volcanic eruption, in contact with air or water. The crystals are so small you need a lens to see them. Basalt is dark, dense and also impermeable, and it is quarried and crushed for road aggregate. Basalt is the rock of the Deccan Traps, which is most of the plateau under Karnataka and Maharashtra, so you are standing on the exam example.
Big crystals means the rock cooled slowly, deep down: granite. Small crystals means it cooled quickly, at the surface: basalt. If a question shows you a photograph or describes crystal size, that one sentence is the whole answer, and the “because it cooled slowly/quickly” is where the explain mark lives.
Sedimentary: limestone, sandstone and shale
Sedimentary rocks are made from sediment — loose particles — that settles in layers, usually under water, and is then squeezed and glued into solid rock. Because they are built in layers you can often see the bedding, and because the particles never perfectly fill the space between each other, most sedimentary rocks contain pore spaces. Hold on to that: it is why 1.1.3 and 1.1.4 exist.
| Rock | What it is made from | How it forms |
|---|---|---|
| Limestone | Calcium carbonate, mostly from the shells and skeletons of dead marine organisms | Shells settle on a warm shallow sea floor, build up over millions of years, and are compacted and cemented into rock |
| Sandstone | Sand grains, mostly quartz, eroded from older rocks | Sand is transported by rivers or wind, deposited in layers, then compacted and cemented by minerals crystallising between the grains |
| Shale | Very fine clay and mud particles | The finest particles settle only in still water, and are compacted so tightly that almost no pore space is left between them |
Notice that shale is made of the smallest particles and is the odd one out of the three — and it is the odd one out again in 1.1.4, and again in 1.6, because fracking is done in shale. That is not a coincidence: the tiny flat particles pack together so tightly that gas trapped inside cannot escape, which is exactly why the gas is still there and why you have to fracture the rock to get it.
Metamorphic: marble and slate
Metamorphic rocks are existing rocks that have been changed by heat and pressure without melting. That last phrase matters. If it melted it would be igneous. Metamorphism happens deep underground, where rock is buried under kilometres of other rock, or where it sits next to a body of hot magma.
- Marble is metamorphosed limestone. Heat and pressure destroy the fossils and shells and recrystallise the calcium carbonate into an even mass of interlocking crystals. That is why marble is uniform, hard, and takes a polish — and why the fossils that were in the limestone are gone.
- Slate is metamorphosed shale (or mudstone). Pressure applied from one direction rotates the flat clay particles until they all lie the same way, which is why slate splits into thin flat sheets. That property is called cleavage and it is the reason slate is quarried for roofing.
limestone → marble and shale → slate. Sedimentary parent, metamorphic child. A very common question is “name the rock from which marble is formed” for one mark, followed by “describe the conditions required” for two — and the two marks are high temperature and high pressure, not “it gets squashed”. Say both, and say that the rock does not melt.
1.1.2 The rock cycle — an ordered chain
The rock cycle is the one diagram in Topic 1 you should be able to draw from memory, because a question that hands you a blank cycle with three or four boxes missing is a standard opener. The syllabus names eight processes and they are the only eight you need: weathering, erosion, transportation, deposition, sedimentation, compaction, cementation and crystallisation.
The eight processes, in the order they happen
| # | Process | What is actually happening |
|---|---|---|
| 1 | Weathering | Rock is broken down in place by rain, frost, temperature change, plant roots or chemical attack. Nothing moves yet. This is the step most candidates confuse with the next one. |
| 2 | Erosion | The loosened fragments are picked up and worn away by moving water, wind, ice or gravity. Erosion involves movement; weathering does not. |
| 3 | Transportation | Rivers, wind, glaciers and waves carry the fragments away. The further they travel the smaller and rounder they get. |
| 4 | Deposition | When the water or wind slows down it can no longer carry the load, so the particles are dropped — the heaviest first, the finest last and furthest out. |
| 5 | Sedimentation | The dropped particles settle out and build up in layers on a sea, lake or river bed over long periods. |
| 6 | Compaction | The weight of the layers above squeezes the lower layers, pressing the particles together and forcing out the water between them. |
| 7 | Cementation | Minerals dissolved in the remaining water crystallise in the gaps and glue the particles together. Now it is a sedimentary rock. |
| 8 | Crystallisation | Somewhere else in the cycle, molten rock cools and its minerals grow into interlocking crystals, forming igneous rock. Slow cooling, big crystals; fast cooling, small ones. |
W E T D S C C — Weathering, Erosion, Transportation, Deposition, Sedimentation, Compaction, Cementation. “We Eat Tea, Drink Some Cold Coffee.” The eighth process, crystallisation, is not part of that chain at all — it belongs to the igneous branch, and putting it in the sedimentary sequence is a classic wrong answer.
This distinction is tested almost every year. Weathering breaks rock down where it stands. Erosion removes the pieces. Frost splitting a boulder on a mountainside is weathering. The stream carrying the splinters downhill is erosion followed by transportation. If a question gives you two marks for “describe the difference”, the second mark is almost always the word in situ or the phrase without movement.
1.1.3 Permeability — a definition to learn word for word
Permeability is the ability of water to pass through the pore spaces of rock and soil.
Two words in that sentence are doing the work: water and pore spaces. If you write “permeability is how easily water goes through a rock” you may be given the mark, but if you write “permeability is how hard a rock is” or “how much water it holds” you will not. Holding water is porosity; letting it through is permeability.
Why does the syllabus care? Because permeability decides where groundwater goes, which decides where aquifers form, where wells work, where a landfill will leak and where a reservoir can be built. It comes back in Topic 3 when you meet water supply, and it comes back in 1.6, where the fact that shale is impermeable is the entire reason fracking exists as a technique.
1.1.4 Classifying the seven rocks
| Permeable — water passes through | Impermeable — water does not pass through |
|---|---|
| Most sedimentary rocks: limestone and sandstone. Sandstone has connected pore spaces between its rounded grains; limestone lets water through its joints and cracks, and the water slowly dissolves it, opening the gaps wider. | Igneous (granite, basalt) and metamorphic (marble, slate), because interlocking crystals leave no connected gaps. Plus some sedimentary rocks: shale, whose clay particles are so fine and so flat that they pack with almost no connected pore space. |
The syllabus says most sedimentary rocks, and it names shale as the exception in the same breath. That single exception is worth remembering because it is the one they test, and because shale is the fracking rock. If you are asked to classify shale, the answer is sedimentary but impermeable.
- (c)Name, in the correct order, the processes shown by arrow X and then by arrow Y. [3]
- (d)A core taken at the sea bed site shows a mudstone layer 12.0 m thick. The accumulation rate measured there is 0.60 mm per year. Calculate how long that layer took to build up. Show your working. [2]
- (e)Explain why the rock in box B is more likely to be permeable than the rock in box C. [3]
- (f)Suggest one reason why the rock in box C is unlikely to contain a fossil in its original shape. [2]
1.2.1 What an ore is
An ore is rock containing minerals and metals.
Short enough that there is no excuse for losing the mark. What you must not do is add your own economics to it — you may have read elsewhere that an ore is rock from which a metal can be extracted “profitably”. That is a fine idea, and it belongs in 1.2.3 where cost and profit are a factor in the decision to extract, but it is not the definition 0680 gives.
The chain is worth keeping straight. A mineral is a naturally occurring solid with a definite chemical composition — quartz, calcite, haematite. A rock is a mixture of minerals. An ore is a rock that happens to contain enough of a useful mineral or metal to be worth digging up. The proportion of useful metal in the ore is called the ore grade, and it comes up again in 1.2.3.
1.2.2 Three ways of getting it out
The syllabus gives you three families of extraction method, and the exam question is nearly always “describe” or “suggest which method is suitable and why”. The deciding factor is almost always how deep the deposit is.
| Family | Named methods | How it works and when it is used |
|---|---|---|
| (a) Surface extraction | opencast, open-pit, open-cut, strip mining | Used when the deposit lies at or near the surface. The soil and rock lying above the deposit — the overburden — is stripped off and the deposit is dug out from the open air. Opencast, open-pit and open-cut are three names for the same idea — working the deposit from an open excavation at the surface instead of from tunnels — and Cambridge uses them interchangeably, so a paper that says “open-cut” is asking about the method you have learned as open-pit. Open-pit works downwards in a series of benches to make a deep bowl; strip mining removes one long strip at a time and dumps the overburden into the strip already worked. Cheap per tonne, fast, safer for workers, but it clears a large area of land. |
| (b) Subsurface extraction | deep mining, shaft mining | Used when the deposit is too deep for the overburden to be worth removing. A vertical shaft is sunk and horizontal tunnels are driven out to the seam; the material is brought up the shaft. It disturbs far less surface land, but it is expensive, slow, and hazardous — roof collapse, flooding, dust and gas — and it needs ventilation, pumping and support all the time the mine is open. |
| (c) Biological extraction | phytomining, bioleaching | Phytomining: plants are grown on low-grade ore or on old mine waste; they absorb metal compounds through their roots and concentrate them in their tissues; the plants are harvested and burned, and the metal is recovered from the ash. Bioleaching: bacteria are used on low-grade ore to produce a solution (a leachate) containing the metal compound, from which the metal is then obtained. Both work on ore too poor for ordinary mining, both use much less energy and disturb much less land — and both are slow. |
Shallow deposit → surface. Deep deposit → subsurface. Low-grade ore or old waste tips → biological. If a question describes a coal seam 400 m down, do not suggest opencast, however much you would like to write about it. And if a question says “the ore contains only 0.2 % copper”, that number is there to point you at bioleaching or phytomining.
1.2.3 The factors that decide whether to extract at all
A company does not dig a mine because the metal is there. It digs when eight separate things line up, and the syllabus names all eight. This is a favourite “suggest three factors…” question, and a favourite Paper 2 source-material question where you are given a report about a proposed mine and asked to decide.
| Factor | The question it answers | Why it can stop a mine |
|---|---|---|
| (a) Exploration | Is there anything there, and how sure are we? | Surveying, sampling and test drilling cost money before a single tonne is sold. If exploration cannot prove a large enough deposit, nothing goes ahead. |
| (b) Geology | What is the rock like around and above the deposit? | Hard rock is slow and expensive to cut; unstable or water-bearing rock means constant support and pumping; the depth and thickness of the seam decide which method is even possible. |
| (c) Accessibility and terrain | Can we get machinery in and ore out? | A deposit under a mountain, in dense forest, offshore or far from any road may need a new road, railway or port built first, and that cost is added to every tonne. |
| (d) Quantity and quality of deposit (ore grade) | How much is there and how rich is it? | Low grade means more rock moved, more energy used and more waste produced per tonne of metal. A small high-grade deposit and a huge low-grade one can be equally attractive; a small low-grade one is not. |
| (e) Climate | Can we work here, all year? | Extreme heat, deep cold, a long monsoon or seasonal flooding can shut a site for months, and workers must be housed and supplied through it. |
| (f) Environmental impact assessment | What will this do to the area, and will permission be given? | An EIA is a formal study, usually required by law before permission is granted. It can force a change of method, expensive mitigation, or refusal. |
| (g) Supply and demand | Does the world want this material? | Prices move. A metal in short supply and high demand justifies a difficult mine; if demand falls or a substitute appears, the same mine is abandoned. |
| (h) Cost and profit | Does the money work? | All the factors above end up here. Extraction, processing, transport, wages, restoration and taxes are set against the expected price. If the sums do not work, the deposit stays where it is. |
Group them into three: what is in the ground (exploration, geology, ore grade), what is on top of the ground (accessibility and terrain, climate, the EIA), and what is on the balance sheet (supply and demand, cost and profit). Three groups is much easier to recall under pressure than eight bullets, and if a question asks for “three factors” you can take one from each group and be certain they are genuinely different points.
1.2.4 Impacts — environmental, economic and social
Read the wording of this objective carefully: describe and explain the environmental, economic and social impacts. Explain means give the mechanism — the “because”. And notice that the syllabus asks for economic and social impacts as well as environmental ones, which means not all of the impacts are negative. Employment, local economies and infrastructure are on the list precisely because they are the other side of the argument. A candidate who lists only harms has answered a third of the question.
| Impact | Type | Describe and explain |
|---|---|---|
| (a) Loss of habitat and biodiversity | Environmental | Vegetation and soil are cleared over the whole working area, so the organisms living there lose food, shelter and breeding sites. Populations fall, and species that cannot move or that are found nowhere else may be lost from the area. Access roads also fragment what is left, cutting large habitats into small isolated pieces. |
| (b) Air, land, noise, visual and water pollution | Environmental | Air: dust from blasting, crushing and haul roads, plus exhaust gases from heavy machinery. Land: spoil heaps and tailings, which may contain toxic metals. Noise: blasting, drilling and lorries, day and night, affecting residents and wildlife. Visual: pits, tips and machinery in a landscape people value. Water: sediment washed into rivers, and acidic or metal-rich drainage from exposed rock and tailings entering surface water and groundwater. |
| (c) Water usage | Environmental / social | Mining uses very large volumes of water for washing, separating and dust suppression, and deep mines must be pumped continuously. This can lower the water table and reduce what is available to farms and households nearby, which matters most in exactly the dry regions where many mines are. |
| (d) Waste management | Environmental | Most of what is dug up is not the product. Overburden, waste rock and tailings must be stored somewhere, usually in tips or behind tailings dams. They occupy land, can be unstable, and can release sediment and dissolved metals for decades after the mine closes. |
| (e) Changes in employment opportunities | Economic / social | A mine creates jobs directly and in the businesses that supply it, often in areas with few alternatives, and wages are typically above local levels. But the jobs may go to incomers rather than local people, they may need skills the area does not have, and they end when the deposit does — and a town built on one mine has nothing to move to. |
| (f) Local and national economies | Economic | Wages are spent locally, supporting shops and services (the multiplier effect); the company pays taxes and royalties; exports earn foreign currency for the national economy. Against that, an economy that depends on one commodity is exposed when the world price falls, and profits from foreign-owned mines may leave the country. |
| (g) Facilities and infrastructure | Social / economic | Roads, railways, ports, power lines, water supply, housing, schools and clinics are often built for the mine and used by everyone. That is a real and lasting gain. The same influx can also overload existing services, push up local prices and rents, and leave infrastructure that has no purpose once the mine closes. |
“Mining causes water pollution” is a description and scores one mark at most. “Mining causes water pollution because rainwater runs off the tailings, dissolving metal compounds, and carries them into the river, so that fish are poisoned and the water is unsafe to drink” contains the mechanism and the consequence, and that is where the second and third marks are. Train yourself to write because and so that in every explain answer.
1.2.5 Repairing the landscape afterwards
The syllabus splits management of damaged land into two ideas, and the difference between them is worth a mark on its own. Land restoration tries to return the land to something like its original condition. Repurposing accepts that the land has changed and gives it a new, useful job.
| (a) Land restoration | What is actually done |
|---|---|
| Replacement of overburden | The soil and rock stripped at the start is stored separately and put back at the end, in the right order, with the topsoil last. Storing the topsoil separately is the whole trick — mixed spoil is not soil and very little will grow in it. |
| Soil improvement | Adding organic matter, fertiliser and lime to restore nutrients, structure and pH, so that plants can establish on ground that has been compacted and stripped. |
| Bioremediation | Using living organisms — bacteria, fungi or plants — to break down or take up pollutants left in the soil and water, so that contamination is reduced without digging everything out and moving it elsewhere. |
| Tree planting | Trees stabilise the surface with their roots, reduce erosion and surface run-off, provide habitat, and screen the site visually. It is slow: a planted wood takes decades to resemble the one that was cleared. |
| (b) Repurposing land | What is actually done |
|---|---|
| Landfill | A worked-out pit is lined and used to bury waste, then capped and covered. It solves two problems at once — a hole and a waste stream — but requires a liner and long-term monitoring of leachate and methane. |
| Lakes | The pit is allowed or helped to flood. This can create a water supply, a fishery or a wetland habitat, but water in a mine void can be acidic or metal-rich and may need treating first. |
| Recreation | Sites become parks, sports pitches, climbing and watersports centres or visitor attractions, which brings income and jobs and keeps the land in public use. |
| Nature reserves | The disturbed ground is managed for wildlife. Bare rock, cliffs and shallow pools are habitats that are rare in an ordinary farmed landscape, so some quarries end up more biodiverse than the farmland around them. |
1.2.6 Discuss: benefits and limitations of these strategies
This is a “discuss” objective, so it is worth 4 to 8 marks and the mark scheme has two columns. Learn it as two columns.
| Benefits | Limitations |
|---|---|
| Land is returned to productive use — farming, forestry, housing or recreation — instead of being abandoned as derelict ground. | Restoration is expensive, and the cost falls at the end of a project when the deposit is exhausted and income has stopped. Companies may under-provide for it, or the operator may have gone. |
| Habitats and biodiversity can be re-established, and some repurposed sites (flooded pits, quarry faces) support species that the surrounding farmland does not. | A restored habitat is not the original one. Soil structure, seed banks and fungal networks take decades or centuries to rebuild, and species found nowhere else are not recovered by planting trees. |
| Erosion, dust and landslip are reduced once vegetation cover is re-established, protecting rivers downstream from silting. | Vegetation takes years to establish on compacted, nutrient-poor, sometimes contaminated ground, and may need repeated replanting and continued soil improvement. |
| Pollution is reduced: bioremediation can lower contamination in place, and capping and lining stop leachate reaching groundwater. | Bioremediation is slow and works only for certain pollutants; some metals cannot be broken down at all, only moved or locked up. Monitoring may be needed for decades. |
| Repurposing creates new jobs and income — recreation, tourism, waste management, fisheries — which partly replaces the employment lost when the mine closed. | The new jobs are usually fewer and lower paid than the mining jobs, so a mining town is rarely made whole by a country park. |
| Visual amenity improves, and local people regain access to land that was fenced off, which matters for health and for property values. | Landscapes cannot always be put back: a deep open pit or a large spoil heap changes the landform permanently, whatever is planted on it. |
For every “discuss” question in this subject, make four moves: benefit → limitation → who bears the cost → over what timescale. Here: the benefit is land back in use; the limitation is that the ecosystem is not the same one; the cost is borne by the company if legislation forces it and by the taxpayer or the local community if it does not; and the timescale is that the profit is made in years while the recovery takes decades. That last sentence, on its own, is often the judgement mark.
- (c)Describe how the land use of the site changed between Map 1 and Map 2. Quote areas from the maps. [4]
- (d)Calculate the percentage of the 400 ha site that was bare industrial land in Map 1. Show your working. [2]
- (e)Explain why the 130 ha of waste rock and tailings has to be treated before grassland will grow on it. [3]
- (f)Discuss the benefits and limitations of repurposing the pit as a lake rather than filling it in. [6]
Two definitions, both examinable word for word
A finite resource is a natural resource that is used up at a faster rate than it is replaced.
Sustainable management of resources is the use of strategies that ensure the needs of the present are met without compromising the ability of future generations to meet their own needs.
The second one is long, so break it into its two halves and learn them as a pair: meet the needs of the present … without compromising future generations. Both halves must be there. A candidate who writes only “using resources carefully so they last” has the idea but not the mark.
Look carefully at the definition of a finite resource, because it is not quite what most people assume. It does not say “a resource that will run out” or “a resource with a fixed amount”. It says it is used up faster than it is replaced. That is a statement about rates. Rocks, ores and minerals are being formed right now — the rock cycle never stopped — but at a rate of millimetres per thousand years, while we extract them by the billion tonnes per year. It is the mismatch between the two rates that makes them finite, and saying so is often the second mark.
That framing also explains why sustainable management is possible at all. If you cannot speed up the rate of replacement — and you cannot make new granite — then the only lever left is the rate of use. Every one of the seven strategies below is a way of pulling that lever.
1.3.3 The seven strategies
| Strategy | How it works | Where it runs into trouble |
|---|---|---|
| (a) Reduce and reuse | Use less material in the first place — thinner packaging, smaller components, designing products to last — and use items again in their existing form rather than treating them as waste. Reuse needs no reprocessing energy at all, which is why it sits above recycling. | Reducing consumption means persuading people and firms to buy less or design differently, which cuts against how most products are sold. Reuse depends on items being made repairable and on systems existing to collect and redistribute them. |
| (b) Recycling: accessibility, ease and education | Used material is collected, sorted, reprocessed and made into new products, so less ore is extracted. The three words the syllabus attaches are the conditions for it working: accessibility (collection points and kerbside collection close to people), ease (simple sorting, clear labelling, so it takes almost no effort), and education (people knowing what can be recycled and why it matters). | Recycling still costs energy and money, sorting mixed or contaminated material is difficult, and some products are made of materials bonded together that cannot be separated economically. Metals recycle very well and repeatedly; many composites do not. |
| (c) Increased efficiency of extraction | Better technology recovers more of the metal from the same rock, and makes previously uneconomic low-grade deposits worth working. Less ore has to be mined per tonne of metal produced, and less waste is created. | New equipment and processes are expensive to install, and higher efficiency can simply make extraction cheaper, encouraging more of it rather than less. |
| (d) Avoiding resource depletion | Deliberately controlling the rate of extraction so that a deposit is not exhausted — quotas on output, limits on licences, leaving some deposits unworked as reserves for the future. | It restricts income now for a benefit that arrives later, and a country that restricts its own output may simply lose the market to one that does not. |
| (e) Legislation | Laws that set the rules: mining licences and quotas, compulsory environmental impact assessments, required restoration bonds, recycling targets, bans on certain practices, taxes on raw material use. | A law is only as good as the political will behind it, laws stop at national borders, and industry may relocate to countries with weaker rules rather than comply. |
| (f) Enforcement | The machinery that makes legislation real: inspection, monitoring, licensing officers, fines and prosecution, and the power to close a site. The syllabus lists it separately from legislation precisely because the two are not the same thing. | Enforcement needs trained staff, equipment and money, over the whole life of every site. Illegal and informal mining is hard to police in remote areas, and fines that are smaller than the profit do not change behaviour. |
| (g) Use of alternative materials | Substituting a scarce material with a more abundant or renewable one — timber or bamboo instead of steel in some construction, aluminium or plastics instead of copper, glass fibre instead of metal cable, synthetic materials instead of scarce minerals. Demand for the finite resource falls. | The substitute may perform less well, cost more, or have its own environmental cost — plastics from petroleum, or timber from felled forest. Swapping one pressure for another is not automatically sustainable. |
If a question asks for three strategies and you write “pass laws” and “make sure the laws are followed”, you get two marks, not one, because the syllabus lists them separately. This is quiet free marks. The same trick works with “reduce” and “reuse”, which are one lettered item but two distinct actions — though be careful, an examiner may treat those as one point, so make the third point come from a different letter.
1.3.4 Discuss: benefits and limitations of these strategies
| Benefits | Limitations |
|---|---|
| Deposits last longer, so the resource remains available to future generations — which is the definition of sustainable management being met. | Every strategy costs money now for a benefit that mostly arrives later, and governments and companies work to much shorter timescales than that. |
| Less extraction means less habitat loss, less waste rock, less pollution and less water use, so the environmental impacts in 1.2.4 are reduced at source. | Recycling, substitution and more efficient extraction all have their own energy demands, transport and emissions; the saving is real but smaller than it first appears. |
| Recycling metals uses far less energy than extracting them from ore, so it lowers both costs and emissions once the collection system exists. | Collection systems are expensive to build and depend on people using them, which requires sustained education and convenient access. |
| New industries and jobs are created in collection, sorting and reprocessing, some of them local and long-term. | Jobs may be lost in extraction, often in exactly the regions that have the fewest alternatives, so the gain and the loss fall on different people. |
| Legislation with real enforcement makes standards the same for every company, so a business that behaves well is not undercut by one that does not. | Enforcement is costly and uneven, rules stop at borders, and firms may move production to countries with weaker legislation, which moves the impact rather than removing it. |
| Reducing dependence on imported raw materials improves a country's security of supply and protects it from price shocks. | Countries whose economies depend on exporting minerals lose income if global demand falls, and they usually have least ability to absorb it. |
“These strategies extend the life of the resource, but the costs fall now and on the producer, while the benefits fall later and on everyone — which is why they generally require legislation and enforcement rather than goodwill.” That sentence names who bears the cost and over what timescale, which is what an evaluation mark is looking for.
| Year | Average ore grade mined (% copper) | Waste rock per tonne of copper (tonnes) | Energy per tonne of copper (GJ) | Share of copper supply from recycling (%) |
|---|---|---|---|---|
| 1980 | 1.60 | 62 | 40 | 22 |
| 1995 | 1.10 | 90 | 52 | 26 |
| 2010 | 0.80 | 124 | 68 | 30 |
| 2024 | 0.55 | 181 | 95 | 34 |
- (c)Describe the trend in average ore grade between 1980 and 2024. Quote figures. [3]
- (d)Calculate the percentage fall in average ore grade between 1980 and 2024. Show your working. [2]
- (e)Explain, using the table, why a falling ore grade makes recycling more attractive. [4]
- (f)Discuss the benefits and limitations of relying on recycling to meet a rising demand for copper. [6]
1.4.1 Where fossil fuels came from — the second ordered chain
All three fossil fuels start the same way and diverge at one step: what died, and where. Coal comes from land plants; petroleum and natural gas come from marine organisms. After that the story is the same — burial, heat, pressure, time. Because it is a chain, it is marked as a chain, so learn the steps in order.
| Fuel | The chain, in order |
|---|---|
| (a) Coal | Dead land plants (trees, ferns) fall into swamp water → the water has little oxygen, so decomposers cannot break them down fully → the partly decayed plant material builds up as peat → it is buried under sediment → over millions of years the weight of the layers above compresses it and raises the temperature → water and gases are driven out, the carbon content rises, and coal is formed in seams. |
| (b) Petroleum (oil) | Dead marine organisms — plankton and other tiny sea life — sink to the sea floor → they are buried in mud in the absence of oxygen, so they do not decay completely → more sediment buries them deeper → over millions of years high pressure and high temperature convert the remains to liquid petroleum → being less dense than water it moves upwards through permeable rock until it is trapped beneath a layer of impermeable rock. |
| (c) Natural gas (methane) | Formed by the same process from the same marine organisms, but at greater depth, where temperatures are higher. The organic material is converted to gas rather than liquid. Being the least dense, the gas collects above the oil, held under the same impermeable cap rock — which is why drilling for one often finds the other. |
Dead. Buried. Airless. Squeezed. Every fossil-fuel formation answer needs: named dead organisms, burial under sediment, absence of oxygen so decomposition is incomplete, and heat and pressure over millions of years. The most commonly dropped mark is the anaerobic one — if oxygen had been present, decomposers would have broken the material down completely and there would be no fuel.
“Oil is made from dead dinosaurs” is the popular version and it will not earn a mark. Say marine organisms or plankton. And for coal, say land plants in a swamp, not “trees underground”.
1.4.2 Classifying energy resources
Renewable (the syllabus also calls them non-finite) means the resource is replaced as fast as it is used, or is effectively inexhaustible. Non-renewable (finite) means it is used faster than it is replaced — the same definition you learned in 1.3.1.
| (a) Renewable / non-finite | (b) Non-renewable / finite |
|---|---|
|
Biofuels: bioethanol, biomass, biogas and wood Geothermal power Hydro-electric power Tidal power Wave power Solar power Wind power |
Fossil fuels: coal, petroleum (oil) and natural gas Nuclear power using uranium |
Nuclear power produces almost no carbon dioxide during generation, which makes people want to file it with the renewables. The syllabus is explicit: nuclear power using uranium is non-renewable, because uranium is a mined finite ore. Low-carbon and renewable are two different claims — keep them apart and you will not lose the mark.
The other classification trap is biofuels. Wood, biomass, biogas and bioethanol are renewable, because the plants they come from can be regrown within a human timescale. They still release carbon dioxide when burned. Renewable does not mean clean.
1.4.3 How each resource actually generates electricity
Almost all of these end in the same place: something spins a turbine, the turbine turns a generator, and the generator produces electricity. Learn that sentence once and then all you have to remember for each resource is what spins the turbine. Solar photovoltaic cells are the one genuine exception — they produce electricity directly, with no turbine at all.
| Resource | What turns the turbine (or what happens instead) |
|---|---|
| Coal, oil, natural gas | The fuel is burned in a power station; the heat released boils water to make high-pressure steam; the steam drives a turbine which turns a generator. Gas can also be burned to drive a gas turbine directly. |
| Nuclear (uranium) | Uranium nuclei undergo fission in a reactor, releasing heat; the heat boils water to steam; steam drives a turbine and generator. Same ending as coal — only the source of the heat differs, and no fuel is burned. |
| Biomass, wood, biogas, bioethanol | Burned to release heat, which boils water to steam and drives a turbine and generator, exactly as coal does. Biogas is produced by anaerobic digestion of organic waste first; bioethanol is made by fermentation of crops and is mostly used as a vehicle fuel rather than for electricity. |
| Geothermal power | Water is pumped down into hot rock deep underground, or hot water and steam are taken from a natural reservoir; the steam returns to the surface and drives a turbine and generator. It needs a region where hot rock is close enough to the surface. |
| Hydro-electric power | A dam holds water in a reservoir at height; water is released through pipes and its movement drives a turbine and generator. The higher the drop and the greater the flow, the more electricity is produced. |
| Tidal power | A barrage is built across an estuary; the rising and falling tide forces water through turbines set into the barrage, turning generators. Output is intermittent but entirely predictable, because tides are. |
| Wave power | Floating or shoreline devices are moved up and down by passing waves; that movement drives a turbine or generator, either directly or by forcing air or fluid through it. |
| Solar power | Two routes. Photovoltaic cells convert light energy directly into electricity, with no moving parts and no turbine. Concentrated solar uses mirrors to focus sunlight onto a fluid, heating it to make steam that drives a turbine and generator. |
| Wind power | Moving air turns the blades of a turbine, which turns a generator. Turbines are grouped into wind farms, on land or offshore where wind speeds are higher and steadier. |
“Heat or movement turns a turbine, the turbine turns a generator, the generator makes electricity.” Coal, gas, oil, nuclear, biomass and geothermal all get there by making steam. Hydro, tidal, wave and wind get there by moving something directly. Only photovoltaic solar skips the turbine entirely. If you can sort a resource into those three groups you can describe its generation without memorising nine separate paragraphs.
1.4.4 Discuss: benefits and limitations of each energy resource
This is the largest “discuss” objective in Topic 1 and it is where the extended-response marks live. The table below gives both sides for every resource named in 1.4.2. Read down the limitations column for the renewables and notice that they are real: an answer that treats renewables as free of problems is as unbalanced as one that treats fossil fuels as having no advantages, and both cap out at the same middling mark.
| Resource | Benefits | Limitations |
|---|---|---|
| Coal | Large reserves in many countries; cheap per unit of energy; reliable output that can be run continuously; existing power stations, transport and skilled workforce already in place; supports large employment. | Finite. Burning releases carbon dioxide (a greenhouse gas) and sulfur dioxide (which contributes to acid rain), plus particulates that affect health. Mining causes the land, water and habitat impacts of 1.2.4. Ash must be disposed of. |
| Petroleum (oil) | Very high energy content per kilogram; easy to transport and store as a liquid; essential for vehicles and aircraft where alternatives are limited; the raw material for plastics, fertilisers and medicines. | Finite. Releases carbon dioxide when burned. Extraction and shipping risk spills that affect coasts and marine life. Prices are volatile and supply is concentrated in a few regions, which creates political and economic risk. |
| Natural gas | Cleanest of the three fossil fuels — roughly half the carbon dioxide of coal per unit of electricity, and very little sulfur dioxide or particulate matter. Gas power stations are quick to build and can be turned up or down rapidly to match demand. | Finite, and still a source of carbon dioxide. Methane leaking from wells and pipelines is itself a powerful greenhouse gas. Needs pipelines or liquefaction for transport, so supply can be disrupted, and prices move sharply. |
| Nuclear (uranium) | Very large energy output from a very small mass of fuel; almost no carbon dioxide, sulfur dioxide or particulates during generation; reliable continuous output regardless of weather; a small quantity of uranium lasts a long time. | Uranium is finite and mined, with all the impacts of mining. Radioactive waste stays hazardous for thousands of years and must be stored securely. Power stations are extremely expensive to build and to decommission. Accidents are rare but their consequences are severe and long-lasting, and public acceptance is often low. |
| Biofuels (bioethanol, biomass, biogas, wood) | Renewable, since crops and trees can be regrown. Biogas turns waste that would otherwise be a disposal problem into fuel, and leaves a digestate that can be used as fertiliser. Bioethanol can be blended into petrol using existing engines. Locally produced, so it reduces dependence on imports and supports rural incomes. | Burning releases carbon dioxide, and wood also releases particulates. Growing fuel crops uses land, water and fertiliser that could grow food — the food-versus-fuel problem you meet again in 2.2.4. Energy content per kilogram is lower than fossil fuels. If forests are cut faster than they regrow, wood stops being renewable in practice. |
| Geothermal | Continuous output day and night, independent of weather, so it is one of the few renewables that is genuinely reliable. Very low emissions in operation. A small surface footprint. Running costs are low once built. | Only viable where hot rock lies near the surface, which is a small number of regions. High drilling and construction costs. A site can cool over decades if heat is taken faster than it is replaced, and drilling can release dissolved gases and, in some settings, trigger small earth tremors. |
| Hydro-electric | Large, reliable output with no fuel cost and no emissions during generation. Output can be increased within seconds to meet peak demand. The reservoir can also supply drinking water, irrigation, flood control, fisheries and recreation. Very long working life. | Building a dam floods a large valley, destroying habitats and farmland and displacing people, sometimes in very large numbers. It traps silt, so land downstream loses the sediment that fertilised it and the reservoir gradually fills. It blocks fish migration, changes river flow, and there is a small but serious risk of dam failure. Very high construction cost, and it needs the right river and valley. |
| Tidal | Entirely predictable years in advance, unlike wind or sun, so output can be planned for. No fuel cost, no emissions in operation, high output from a single barrage, and a very long working life. The barrage may also serve as a road crossing and offer flood protection. | Very high construction cost, and only a limited number of estuaries have a large enough tidal range. A barrage alters the estuary it is built in, affecting the mudflats that feeding birds and other estuary organisms depend on, and it obstructs shipping and fish movement. Output stops between tides, so other sources are still needed. |
| Wave | No fuel cost and no emissions in operation. Uses no land. Many countries have long coastlines, so the potential resource is widely distributed, and waves continue at night unlike solar. | Output varies with the weather and is unreliable. Devices must survive storms and salt water, so maintenance costs are high and the technology is much less developed than wind or solar. Installations can interfere with fishing and shipping and alter the shoreline habitat. |
| Solar | No fuel cost, no emissions in operation, and no moving parts in photovoltaic panels so maintenance is low. Panels can be fitted to existing roofs, using no extra land, and can supply remote settlements with no grid connection at all. Output is highest at midday, which in hot countries matches peak demand for cooling. | No output at night and much less on cloudy days, so storage or a back-up supply is needed. Output is poor at high latitudes and in cloudy climates. Large solar farms need land. Manufacturing panels uses energy and mined materials, and panels have to be disposed of or recycled at the end of their life. |
| Wind | No fuel cost and no emissions during generation. Turbines are relatively quick to build and can be added one at a time. Land between turbines can still be farmed. Offshore wind is stronger and steadier, and a single modern turbine supplies a large number of homes. | Output is intermittent and depends on wind speed, so it cannot be relied on to meet demand at a given moment. Turbines are visually intrusive and produce noise, which causes local objection. They can kill birds and bats. Offshore construction and maintenance are expensive, and the best wind sites are often far from the cities that need the electricity. |
Reliable, predictable, intermittent, continuous. These are not the same thing and examiners reward the distinction. Wind and solar are intermittent and hard to predict. Tidal is intermittent but completely predictable. Geothermal, hydro-electric and biomass are continuous and can be run on demand. If you are asked why a country cannot run entirely on wind and solar, the answer is not that they are weak — it is that supply does not match demand in time, which is why 1.5.1 lists battery storage as a strategy.
1.4.5 What makes demand for energy rise
The command word here is describe and explain, so each factor needs its mechanism. Notice that the last three factors on the list are not about demand going up at all — they are about supply going wrong, and about how that changes what people demand and how much they pay.
| Factor | Explanation — the mechanism |
|---|---|
| (a) Transport | As countries develop, more people own vehicles and travel further and more often, and freight moves greater distances; air travel grows fastest of all. Almost all of that runs on fuel, so energy demand rises directly with the number of journeys. |
| (b) Personal and national wealth | Richer households buy more appliances — refrigerators, air conditioning, televisions, computers, cars — and use them more. Richer countries build more infrastructure and can afford to import more fuel. Wealth is the strongest single predictor of energy use per person. |
| (c) Climate | Cold regions use large amounts of energy for heating; hot regions use large amounts for air conditioning and refrigeration. Extremes in either direction raise demand, and demand also swings with the seasons, which is why a grid must be built for its peak rather than its average. |
| (d) Human population size | More people need more lighting, cooking, heating, water treatment, transport, food production and manufactured goods. Total demand rises with population even if demand per person stays exactly the same — and in most growing populations it is rising too. |
| (e) Industry | Manufacturing, mining, smelting, cement and chemicals are very energy-intensive. A country that industrialises sees demand rise sharply, and heavy industry can account for a large share of a national total on its own. |
| (f) Disruption to supply | War, political disputes, strikes, accidents, damaged pipelines or extreme weather can cut supply suddenly. Prices rise, users switch to whatever else is available, and governments respond by building reserves and diversifying sources — which changes the pattern of demand between resources. |
| (g) Unreliable supply | Where power cuts are frequent, households and businesses buy diesel generators and batteries and run them as back-up. That raises total energy demand, and usually shifts it onto more expensive and more polluting sources. |
| (h) Scarcity of resources | As a resource becomes scarce its price rises. Users reduce consumption or switch to alternatives, so demand for the scarce resource falls while demand for the substitute rises. Scarcity therefore changes the mix of resources demanded, not just the total. |
- (c)Compare the electricity mix of Country P with that of Country R. [4]
- (d)Calculate the percentage of Country S’s electricity that is generated from finite resources. Show your working. [2]
- (e)Explain how the hydro-electric power in Country Q’s mix is used to generate electricity. [3]
- (f)Suggest which of the four countries is most exposed to a disruption to its energy supply, and justify your choice. [4]
1.5.1 Eight strategies for managing energy resources
The strategies split neatly into two halves and it is worth seeing that before you learn the list. Items (a) to (f) are about using less of what we already have. Items (g) and (h) are about getting more out of what we have, and finding new sources. If a question asks for “two contrasting strategies”, take one from each half.
| Strategy | How it works | Limitation |
|---|---|---|
| (a) Reducing consumption | Simply using less: switching off lights and appliances, lowering heating and raising air-conditioning settings, shorter journeys, less standby power. Costs nothing to start and takes effect immediately. | Depends on millions of individual decisions repeated every day. Behaviour tends to drift back, and there is a floor below which comfort, health and business activity are affected. |
| (b) Insulation | Loft, wall and pipe insulation, double glazing and draught-proofing slow the transfer of heat out of a building in winter and into it in summer, so far less energy is needed to keep the temperature comfortable. | Costs money up front, and the people in the worst-insulated housing are often those least able to pay. It is difficult and expensive to retrofit into old buildings. |
| (c) Energy-efficient devices, including vehicles and electrically propelled vehicles | Appliances, lighting and machinery that deliver the same service for less energy — LED lamps in place of filament bulbs, efficiency-rated appliances, more efficient engines. Electrically propelled vehicles convert a much larger share of their energy into motion than a petrol engine does, and produce no exhaust emissions where they are driven. | New equipment costs more to buy, and manufacturing it uses energy and materials. An electric vehicle is only as clean as the electricity charging it, and its battery needs mined lithium, cobalt and other minerals — which takes you straight back to 1.2.4. |
| (d) Exploiting existing energy resources | Getting more from resources we already have rather than finding new ones: reworking older oil and gas fields with better technology, upgrading power stations to higher efficiency, reducing losses in transmission, and using waste heat from power stations to heat buildings. | Extending the life of fossil-fuel infrastructure keeps emissions going and can delay the switch to alternatives. Older fields become progressively more expensive and more difficult to work. |
| (e) Education on energy conservation | Teaching in schools, public campaigns, energy labels on appliances and clear information on bills, so that people know which actions actually matter and can see the effect of what they do. | Awareness changes behaviour more slowly and less reliably than price or law does, and the effect fades when the campaign stops. |
| (f) Transport policies | Investment in buses, trams and rail; cycle lanes and pedestrian areas; congestion charges and parking restrictions; fuel taxes; car sharing; incentives for electrically propelled vehicles; planning that puts housing near workplaces. Moving people out of individual cars cuts energy use per journey sharply. | Public transport is expensive to build and must be frequent and reliable before people give up cars. Charges and taxes fall hardest on those with the least choice, particularly in rural areas with no alternative service. |
| (g) Battery storage | Large batteries store electricity when generation exceeds demand and release it when demand exceeds generation. This is the direct answer to the intermittency of wind and solar: it lets a grid use a much higher share of renewables without keeping fossil-fuel stations running as back-up. Smaller batteries do the same job for a single household with solar panels. | Batteries are expensive, store a limited amount for a limited time, and gradually lose capacity. Manufacturing them requires mined lithium, cobalt and nickel, with the extraction impacts of 1.2.4, and end-of-life recycling is still developing. |
| (h) Development of new energy resources | Research into, and investment in, resources not yet in wide use — the four named in 1.5.2 below. Reduces dependence on finite resources and can lower emissions. | Research is slow and expensive, and there is no guarantee a technology will work at scale or ever become cheap enough. New infrastructure has to be built for it. |
1.5.2 The four new energy resources you must know
| Resource | How it works | The honest assessment |
|---|---|---|
| (a) Blue hydrogen | Hydrogen fuel produced from natural gas. Burning the hydrogen afterwards produces water rather than carbon dioxide. | It starts from a finite fossil fuel, and carbon dioxide is released during its production, so the emissions are moved rather than removed unless they are captured and stored. It uses existing gas infrastructure, which makes it quicker and cheaper to introduce than green hydrogen. |
| (b) Green hydrogen | Hydrogen fuel produced using renewable resources — renewable electricity is used to split water into hydrogen and oxygen. Burning it produces water only. | Genuinely low-carbon across the whole chain, and it stores renewable energy in a form that can be moved and kept, which helps with intermittency. But it is expensive, a lot of energy is lost in making it and using it again, and it needs a large supply of spare renewable electricity to exist first. |
| (c) Ground source heat pumps | Transfer of heat from the ground for heating. Pipes buried in the ground carry a fluid that absorbs heat from the soil or rock, which is at a fairly steady temperature all year; a pump raises that heat to a useful temperature for the building. | Very efficient, because it moves existing heat instead of generating it, and the ground temperature barely changes with the seasons so it works in winter. But installation means digging or drilling, so it costs a lot up front and needs land, and it runs on electricity, so its emissions depend on the grid. |
| (d) Air source heat pumps | Transfer of heat from the air for heating. A unit outside the building absorbs heat from the outside air — there is usable heat in air well below freezing — and transfers it indoors. | Much cheaper and easier to fit than a ground source pump, with no digging, and it can be retrofitted to most buildings. But efficiency falls as the outside air gets colder, which is exactly when the heating is needed most, and the outdoor unit makes some noise. |
Blue = from natural gas. Green = from renewables. Both burn to give water. The colour tells you where the hydrogen came from, not what comes out of the exhaust — and that is exactly the distinction an examiner is testing.
Say transfers heat, not “produces” or “generates” heat. The syllabus wording is “transfer of heat from the ground/air for heating”, and the reason a heat pump is efficient is precisely that it moves heat that is already there rather than making any. Get that verb right and the definition mark follows.
1.5.3 Discuss: benefits and limitations of these strategies
| Benefits | Limitations |
|---|---|
| Finite resources last longer, and a country importing less fuel gains security of supply and is less exposed to price shocks and political disruption. | Almost every strategy costs money before it saves any, and the households and countries that would gain most from insulation and efficient devices are usually those least able to pay for them. |
| Lower fuel use means fewer emissions of carbon dioxide, sulfur dioxide and particulates, so air quality and health improve alongside the climate benefit. | Making the equipment — panels, batteries, heat pumps, electric vehicles — itself uses energy and mined minerals, so the saving over the whole life cycle is smaller than the saving at the point of use. |
| Households and businesses save money on bills once the initial cost is repaid, and insulation and efficient devices go on saving for many years with no further action. | Payback times can be long, and people move house or replace equipment before they see the return, which weakens the incentive to invest. |
| Battery storage and new resources let a grid take a much higher share of renewables without keeping fossil-fuel stations idling as back-up. | Storage is still expensive and limited in capacity, and some new resources may never become cheap enough at scale — research can fail, and there is no guarantee of a return. |
| Transport policies reduce congestion, noise and urban air pollution as well as energy use, so the benefits reach people who do not own a car at all. | Charges and fuel taxes fall hardest on those with the fewest alternatives, and public transport has to be built and running reliably before people will give up private vehicles. |
| Education and labelling are cheap, reach large numbers of people, and support every other strategy by making people aware of what is worth doing. | Awareness on its own changes behaviour slowly and inconsistently, which is why education generally has to be combined with price signals or legislation to work. |
The pattern across the whole of 1.5 is the same: the cost is paid now, by the household or the country installing it; the benefit accrues later, and partly to everyone else. That mismatch is the reason governments use subsidies, taxes and legislation instead of waiting for people to act — and saying so is very often the judgement mark in a “discuss” answer.
- (c)Describe the relationship between how much energy a measure saves and how much it costs to install. [3]
- (d)Electricity costs $0.20 per kWh. Calculate the payback time for loft insulation. Show your working. [3]
- (e)Explain why a household on a low income might fit draught-proofing and LED lighting but not a heat pump. [3]
- (f)Discuss the benefits and limitations of relying on energy-efficient devices alone to manage a country’s demand for energy. [6]
1.6.1 The definition, and why the technique exists
Fracking is the extraction of natural gas or petroleum from shale rock by hydraulic fracturing.
Three things must be in it: natural gas or petroleum, shale rock, and hydraulic fracturing. Leave out “shale” and you have described drilling in general; leave out “hydraulic” and you have lost the mechanism.
Now connect it back to 1.1.4, because that is where the understanding is. Shale is a sedimentary rock that is impermeable — its clay particles are so fine and flat that they leave almost no connected pore spaces. Oil and gas formed within the shale cannot flow through it, so an ordinary well drilled into shale produces very little. That is precisely why the gas is still there after millions of years, and why you have to break the rock to release it.
The technique, in order: a well is drilled down to the shale layer and then turned to run horizontally through it, so that a single well pad reaches a long section of rock. A mixture of water, sand and chemicals is then pumped down at very high pressure. The pressure fractures the shale, opening a network of cracks. The sand grains lodge in the cracks and hold them open when the pressure is released, so that gas or oil can flow through the new cracks into the well and up to the surface. The fluid that returns up the well — the flowback — contains the added chemicals plus salts and other substances picked up from the rock, and has to be treated or disposed of.
Background, not required. Sub-topic 1.6 contains exactly two objectives: define fracking (1.6.1) and discuss it (1.6.2). Horizontal drilling, the sand and the flowback are set out above because the discussion does not make sense without them, not because you can be asked for them in their own right. Learn the definition and the two columns; treat the engineering as context.
The sand grains prop the fractures open after the pressure is removed, so that the gas can keep flowing; without the sand the cracks close again and the well stops producing. That is a because-and-so-that answer, which is exactly what explain means, and it is worth writing out once for the practice. Be clear, though, that the proppant itself is background — 1.6 asks only for the definition and the discussion, so the marks live there.
1.6.2 Discuss: benefits and limitations of fracking
This is the most politically loaded objective in Topic 1, and it is therefore the one where a one-sided answer is punished most clearly. Cambridge is neutral. The mark scheme has two columns and expects a judgement that names who gains, who bears the cost, and over what timescale. Learn both columns; do not learn an opinion.
| Benefits | Limitations |
|---|---|
| Access to reserves that were previously unobtainable. Large quantities of gas and oil are held in shale and could not be extracted by conventional drilling at all, so fracking increases the total resource available. | It is still a finite fossil fuel. Burning the gas releases carbon dioxide, so fracking extends the use of fossil fuels rather than replacing them, and investment in it may delay the development of renewable alternatives. |
| Energy security. A country with shale reserves can generate its own gas instead of importing it, which reduces exposure to price shocks and to disruption of supply from other countries. | Very high water use. Millions of litres of water are needed per well, which competes with agriculture and domestic supply — a serious objection in dry regions, which is where several shale basins are. |
| Cheaper gas. Increased supply lowers gas prices for households and industry, which reduces fuel poverty and lowers manufacturing costs. | Risk to water supplies. The fracking fluid contains chemicals, and the flowback returns with dissolved salts and other substances. If a well casing fails or waste is not handled properly, groundwater and surface water can be contaminated. |
| Gas can displace coal. Burning gas rather than coal for the same electricity produces roughly half the carbon dioxide and far less sulfur dioxide and particulate matter, so replacing coal-fired generation improves air quality and lowers emissions. | Methane leakage. Methane escaping from wells and pipelines is itself a powerful greenhouse gas, and enough leakage can offset the advantage gas has over coal. |
| Employment and local income. Drilling creates jobs and brings contracts to local suppliers, and companies and governments receive taxes and royalties. | Small earth tremors. Fracturing rock at high pressure has been linked to small earthquakes near some sites. They are usually too weak to damage buildings, but they cause real public concern and have led to fracking being suspended or banned in several countries. |
| Bridging supply. Supporters argue gas can cover demand while renewable capacity and storage are built, because gas power stations can be turned up and down quickly to balance intermittent wind and solar. | Local disturbance and land use. Well pads, access roads, heavy lorry traffic, noise, dust and floodlighting industrialise a rural area. Shale wells decline quickly, so many wells must be drilled to maintain output, spreading the disturbance further. |
Benefit: more gas, produced domestically, cheaper, and cleaner than the coal it may replace. Limitation: water use, contamination risk, tremors, methane leaks, and it is still a fossil fuel. Who bears the cost: the water, traffic, noise and tremor risk fall on the local community and its farmers, while the tax revenue and the security of supply are national. Timescale: individual shale wells produce for a few years, so the gain is short-lived, while contaminated groundwater and the carbon dioxide released last far longer. That paragraph, adapted to whatever the source material says, will earn the evaluation marks in almost any fracking question.
- (c)Describe what happened to the field’s gas output between 2019 and 2024. Quote figures. [4]
- (d)Each new well uses 15 million litres of water while it is fractured. Calculate the water used by the wells drilled in 2024. [2]
- (e)Explain why output stopped rising in 2024 even though 90 new wells were drilled that year. [3]
- (f)Discuss the benefits and limitations of continuing to develop this field. [8]