Hi Tara. Topic 2 has only three sub-topics, which makes it look small on the syllabus page. It is not. 2.2 alone has twelve lettered strategies for increasing food production and nine lettered impacts of doing it badly, and 2.3 has another fifteen items across causes, impacts and strategies. So treat this topic as three long sections rather than three quick ones.
The good news is that the three sub-topics chain together, and once you see the chain you can stop learning them as three separate lists. 2.1 is what soil is and what makes it grow crops. 2.2 is what farmers do to grow more, and what goes wrong when it is done unsustainably. 2.3 is the single worst thing that goes wrong — soil erosion — taken through its causes, its impacts and the strategies that fix it. Notice that the last item of 2.2.4 is “soil erosion” and the first item of 2.3.1 is “unsustainable agricultural practices”. The syllabus is deliberately handing you the join. Learn it as cause → impact → strategy, because that is exactly the shape of a six-mark question.
One warning about tone, and it matters for your marks. This topic makes it very easy to write an answer that says intensive farming is bad, monocultures are bad, fertilisers are bad and pesticides are bad. That answer will not score well, and not because the examiner disagrees with you — because it is only half of the question. Intensive agriculture and monoculture exist because they produce far more food per hectare, and food shortage is also an environmental and social problem. The syllabus wants the trade-off: what a practice achieves, what it costs, who bears that cost, and over what timescale. Every table in this guide has two columns for that reason.
Two definitions are given word for word and can be asked back word for word: weather (2.1.4) and sustainable food production (2.2.2). They are boxed in yellow. There is also a definition of genetically modified organisms embedded in 2.2.3(d) that is worth learning in the syllabus's own words. Start with those three sentences.
Almost every mark lost on a question you knew is lost here: the paper says state and the candidate writes a paragraph, or it says explain and the candidate writes a list. Cambridge uses these words with fixed meanings, and Paper 2 in particular opens with the short ones because it is a source-led paper — it wants you to read the figure first and theorise afterwards.
| Command word | What it is asking for, and how long the answer should be |
|---|---|
| State | Give a short fact or a single value. No reason, no sentence needed. “State the month with the highest rainfall” → January. One or two words is a complete answer, and adding more wastes time you need later. |
| Identify | Pick something out of a source you have been given — a figure, a table, a map, a photograph. It is the standard opener on a source-led question. The answer is in the source, so do not answer it from memory; find it and quote it, with its unit if it has one. |
| Calculate | Work out a number, and show the working, because the method usually carries a mark of its own. Give the unit and do not round more than the data justifies. Percentage change is (change ÷ original) × 100; “original” means the value you started from, which is the one candidates get wrong. |
| Describe | Say what is happening or what something is like, without saying why. Describing a trend means: overall direction, then any change of direction, then figures from the source to support it — a described trend with no numbers in it rarely gets full marks. |
| Explain | Give the reason or the mechanism. Every sentence needs a because or a so in it. If your answer would still make sense with all the connectives removed, you have described rather than explained. |
| Suggest | Apply what you know to a situation you have not met before. There is no single learned answer; the examiner wants sensible reasoning that fits the context in front of you. This is the AO3 skill itself, and it is why the source matters more than your notes. |
| Compare | Write about both things in the same sentence, using comparative words: higher than, faster than, whereas. Two separate descriptions, one per paragraph, is not a comparison and is marked as if the second half is missing. |
| Discuss the benefits and limitations | Both columns, whether or not you think one side wins. This is the shape of the six-mark question in this topic, and half the marks sit in the column candidates leave out. |
| Evaluate | Go one step past discuss: weigh the two sides and reach a judgement, then say what your judgement depends on. “Terracing is the more effective strategy on a steep slope because it removes the gradient the water runs down, but only where there is enough labour to build and maintain it; on gentle slopes contour ploughing achieves most of the benefit for almost no cost.” An evaluation with no conclusion in it loses the marks that separate it from a discussion. |
One habit worth building now. Underline the command word and the mark allocation before you write anything. Six marks means roughly six creditable points, and on a discuss or evaluate question it means points on both sides.
2.1.1 What soil is made of
Soil is not dirt and it is not simply crushed rock. It is a mixture of four components, and every one of them has to be there for a crop to grow. The syllabus lists them in this order, and a “describe the composition of soil” question expects all four.
| Component | What it consists of |
|---|---|
| (a) Mineral particles | Sand, silt and clay — fragments of weathered rock, differing in size. Sand particles are the largest, silt is intermediate, clay is the smallest. This is the mineral skeleton of the soil and it comes from the rock beneath, by the weathering you met in Topic 1. |
| (b) Organic content | Two things, and the syllabus wants both. First, living organisms: plants, animals, fungi and bacteria — roots, earthworms, insects, and the decomposers. Second, organic matter from decomposition — the partly broken down remains of dead plants and animals, often called humus. |
| (c) Gases | Air in the pore spaces between the particles. Roots and soil organisms respire and need oxygen; a soil with no air in it is a soil in which roots die. |
| (d) Water | Water held in and around the pore spaces, carrying dissolved mineral ions. This is the only way a root can take up nutrients — they must be in solution. |
The syllabus states plainly that you do not need to know what proportion of a soil is mineral, organic, air or water. So do not try to memorise those figures and do not quote them in an answer. You need the four components and what each one does. Anything more is time spent on something that cannot be asked.
Rock, life, air, water. Mineral particles (rock), organic content (life, living and dead), gases (air), water. If you can say those four words you can build the whole answer out from them, and each one leads straight into a reason it matters for crop growth.
2.1.2 Why the composition matters for crop growth
This is the objective that turns the list above into marks. Each component is here again, but now with the word because attached.
| Feature of the soil | Why it matters for a crop |
|---|---|
| (a) Mineral particles: sand, silt and clay | Particle size controls almost everything else. Sand particles are large, so the gaps between them are large: water drains through quickly, the soil is well aerated and easy to work, but it dries out fast and nutrients are washed away with the water. Clay particles are tiny and flat, so the gaps are tiny: water is held tightly and nutrients are retained, but the soil drains poorly, becomes waterlogged, holds little air and is heavy to cultivate. Silt is intermediate on every count. A crop needs the balance between these, which is what 2.1.3 is about. |
| (b) Nutrient content | Plants need mineral ions dissolved in soil water, supplied both by the organic content as it decomposes and as inorganic ions already in the soil. The three the syllabus names are nitrogen as nitrate ions, NO₃⁻, needed for amino acids and proteins and so for leaf growth; phosphorus as phosphate ions, PO₄³⁻, needed for root development and energy transfer; and potassium as potassium ions, K⁺, needed for flowering, fruiting and general regulation inside the plant. Shortage of any one limits yield however good the rest of the soil is. |
| (c) pH: acidic, neutral and alkaline | pH controls how available the mineral ions are: at the wrong pH, ions become locked into forms the roots cannot absorb, so a soil can be full of nutrients the crop cannot reach. It also affects the soil organisms and the decomposers. Most crops do best at a roughly neutral pH, and farmers add lime to raise the pH of an acidic soil. |
| (d) Pore spaces | The gaps between particles are where the air and water sit, and where roots grow through. Too few pore spaces — a compacted or heavy clay soil — and roots cannot penetrate, water cannot drain and air cannot reach the roots. Too many large pores and everything drains straight through. |
| (e) Gas content | Roots respire, and so do the soil bacteria and fungi that release nutrients from organic matter. Respiration needs oxygen. In a waterlogged soil the pore spaces fill with water, oxygen is excluded, root respiration fails and the roots die — which is why drainage is a farming problem and not just a comfort. |
| (f) Water content and drainage | Water is needed as a raw material for photosynthesis, to keep cells turgid so the plant stays upright, and as the solvent that carries mineral ions into the root. But the soil must also drain: standing water excludes air. A crop needs a soil that holds enough water to survive a dry spell and lets the excess go. |
| (g) Ease of cultivation | The farmer has to plough, sow, weed and harvest. A heavy wet clay is difficult and slow to work and can only be worked in a narrow window of weather; a light sandy soil is easy but blows and washes away. Ease of cultivation is an economic factor as much as a biological one — it decides labour, fuel and machinery costs. |
2.1.3 Why loam is the best medium for crop growth
Loam is a soil containing a mixture of sand, silt and clay together with organic matter. The exam question is almost always explain why it is a good growing medium, and the syllabus gives you five reasons. Learn them as five, because a 5-mark question is a real possibility.
| Reason | The mechanism |
|---|---|
| (a) Ideal combination of mineral particles and pore spaces | The mixture of large sand grains and small clay particles produces a range of pore sizes: large pores that let air in and excess water out, and small pores that hold water against gravity. Neither a pure sand nor a pure clay can do both. |
| (b) Retains moisture | The clay and the organic matter hold water in the small pores, so the crop has a supply through dry spells and does not wilt after a few days without rain. |
| (c) Contains organic content and inorganic ions | Decomposing organic matter releases nitrate, phosphate and potassium ions steadily into the soil water, so nutrients are supplied continuously rather than in a single dose, and the soil holds on to them. |
| (d) Allows excess water to drain | The large pores let surplus water pass through, so the soil does not become waterlogged, air can reach the roots and root respiration continues. |
| (e) Easy to cultivate | Loam is neither as heavy and sticky as clay nor as loose as sand, so it can be ploughed and sown over a wider range of weather, with less fuel, machinery wear and labour. |
“Loam holds enough water and nutrients to feed the crop, but drains and aerates enough not to drown it — and it is easy to plough.” That single sentence contains four of the five marks. Add “because it mixes large sand pores with small clay pores” and you have the fifth.
2.1.4 Weather — a definition to learn word for word
Weather is the day-to-day conditions of the atmosphere in a location.
Three parts: day-to-day, conditions of the atmosphere, in a location. The reason the syllabus is fussy is that weather has a partner definition — climate, which you meet in Topic 4 — and the difference between them is timescale. Weather is what it is doing today; climate is the pattern over many years. Candidates lose the mark by writing one and being asked for the other.
2.1.5 Wet seasons and dry seasons
This is a short, stated objective: some areas of the world experience wet seasons and dry seasons that impact crop growth. You do not need a mechanism for why monsoons happen — you need to be able to say what a strongly seasonal rainfall pattern does to farming.
In the wet season there is plenty of water for growth, but heavy rain also causes flooding, waterlogged soil in which roots cannot respire, leaching of nutrients out of the soil, and erosion of bare ground. In the dry season crops may fail for lack of water, soil dries and cracks, and bare dry soil is blown away by wind. The practical effect is that the growing season is limited to part of the year, so the timing of planting matters enormously, and a wet season that arrives late or fails can lose an entire harvest. It is also the reason irrigation, rainwater harvesting and mulching matter so much in 2.2.3.
2.1.6 Conditions for the optimum rate of photosynthesis and crop growth
A crop's yield depends on how much photosynthesis it can do over the season, and the syllabus asks you to describe and interpret the conditions for that — interpret meaning you may be given climate data for two places and asked which will produce more.
| Condition | What it means, and how it limits yield |
|---|---|
| (a) Length of growing season | The period of the year when temperature, water and light are all sufficient for a crop to grow. A long growing season means more total photosynthesis, a larger yield, and possibly more than one harvest from the same land in a year. A short season, whether limited by cold winters or by a short wet season, caps the yield however good the soil is. |
| (b) Optimum weather conditions | Chiefly temperature and rainfall. Photosynthesis and growth speed up as temperature rises to an optimum, because the enzymes controlling them work faster; above that optimum the rate falls again, because the enzymes are denatured — damaged so that they no longer work. (0680 wants the shape of that curve, a rise to an optimum and then a fall; the biochemistry behind it belongs to Biology and is background here.) Very high temperatures also cause water loss and wilting. Too little rainfall and the crop cannot photosynthesise or stay turgid; too much and the soil waterlogs and nutrients leach away. Wind, frost, hail and storms all damage crops directly. |
| (c) Daylight hours | Light supplies the energy for photosynthesis, so more hours of daylight means more hours of photosynthesis per day and a greater yield. Day length varies with latitude and season: near the equator it is roughly constant all year, while at high latitudes summer days are long and winter days very short, which is one reason growing seasons are short there. Cloud cover reduces light intensity even when the day is long. |
If a question gives you a table of monthly temperature and rainfall for two locations and asks which is better for growing maize, do not answer from general knowledge. Quote the figures. “Location A has six months above 20 °C with more than 60 mm of rain, while location B has only three, so A has the longer growing season and will give the higher yield.” The marks are for reading the data and linking it to a mechanism, not for knowing about maize.
| Location | J | F | M | A | M | J | J | A | S | O | N | D |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| A — mean temperature / °C | 24 | 25 | 26 | 26 | 25 | 23 | 22 | 23 | 25 | 26 | 25 | 24 |
| A — rainfall / mm | 210 | 195 | 175 | 120 | 45 | 10 | 5 | 8 | 30 | 55 | 160 | 200 |
| B — mean temperature / °C | 9 | 11 | 15 | 19 | 19 | 24 | 26 | 25 | 23 | 18 | 14 | 10 |
| B — rainfall / mm | 30 | 35 | 55 | 70 | 90 | 120 | 140 | 130 | 55 | 45 | 40 | 32 |
As a percentage of the Location B total: (371 ÷ 842) × 100 = 44.1 per cent, which is about 44 per cent more. The trap is dividing by the Location A total instead; “more than B” means B is the value you started from.
2.2.1 The types of agriculture
Four pairs or groups of terms, and they are classifications on different axes — a single farm can be described by several of them at once. A commercial arable monoculture is all three things simultaneously, and being able to say so is the sign that you have understood the classification rather than memorised it.
| Type | What it means |
|---|---|
| (a) Arable, pastoral and mixed | Arable farming grows crops. Pastoral farming raises livestock, usually on grass. Mixed farming does both on the same farm, which lets the manure from the animals fertilise the crops and the crop residues feed the animals. That circularity is why mixed farming keeps appearing in the sustainability answers later on. |
| (b) Subsistence and commercial | Subsistence farming produces food mainly to feed the farmer and the family, with little or no surplus to sell. It is usually small-scale, labour-intensive and low-input. Commercial farming produces food to sell for profit, is usually larger, more mechanised and higher-input, and is oriented to whatever the market will buy. |
| (c) Intensive | A high input of labour, machinery, fertiliser, pesticide, irrigation or feed per unit area, in order to obtain a high yield from a small area of land. It can be either commercial or subsistence: rice paddies worked by hand and a glasshouse tomato operation are both intensive. |
| (d) Monoculture | Growing a single crop species over a large area, often year after year on the same land. It allows the whole farm to be planted, treated and harvested with one set of specialised machinery at one time, which is highly efficient and cuts costs per tonne. |
“Intensive” and “monoculture” are descriptions of how a farm operates, not verdicts on it. Intensive farming produces much more food per hectare, which means less land has to be farmed in total to feed a given population, and that can leave more land as natural habitat. Monoculture lowers the cost of food, which matters most to the people with the least money. Both also carry real costs, which is the whole of 2.2.4. An examiner is looking for you to hold both facts at once; an answer that only attacks them is marked as incomplete, not as principled.
2.2.2 Sustainable food production — a definition to learn word for word
Sustainable food production is the production of sufficient food for the present generation using methods that ensure future generations can grow food from the same land.
Notice the first half: sufficient food for the present generation. Sustainability in this syllabus never means growing less food. It means growing enough, by methods that leave the land able to do it again. If your answer to a sustainability question is “farm less intensively” without saying how the food is still produced, you have only answered the second half.
2.2.3 Twelve strategies to increase food production and crop yield
This is the longest list in the topic. Read the command word: describe and explain, so each strategy needs a mechanism, not just a name. The table gives you the mechanism and, where it matters, the cost — because several of these strategies reappear in 2.2.4 as the things that cause harm when overused.
| Strategy | How it raises yield — the mechanism |
|---|---|
| (a) Mixed cropping, intercropping and crop rotation | Mixed cropping grows more than one crop in the same field, so that if one fails the other still yields. Intercropping grows two crops in alternating rows, so the ground is covered, weeds are suppressed and light and water are used more fully. Crop rotation grows different crops on a field in successive years: different crops take up different ions in different proportions, so no single nutrient is stripped out, and pests and diseases specific to one crop cannot build up in the soil. Including a legume in the rotation restores nitrogen to the soil naturally. |
| (b) Improved methods of irrigation | Trickle or drip irrigation delivers water through pipes directly to the base of each plant, so almost none is lost to evaporation or to the ground between plants; it also keeps the soil from being saturated, which reduces salinisation and waterlogging. Rainwater harvesting collects and stores rain from roofs and surfaces during the wet season for use in the dry one. Automated watering systems use timers and soil-moisture sensors to apply exactly the amount of water needed, when it is needed, so less is wasted and the crop is never short. |
| (c) Mechanisation | Tractors, seed drills, sprayers and combine harvesters allow a much larger area to be worked by fewer people and much faster, so sowing and harvesting happen at the optimum time rather than being spread over weeks. Machines also apply seed, water and chemicals more evenly and precisely than hand labour. The costs are the purchase price, the fuel, the loss of agricultural employment, and soil compaction under heavy machinery. |
| (d) Genetically modified organisms | The syllabus defines this as changing the genetic material of an organism by removing, changing or inserting individual genes to give favourable characteristics. Crops can be given resistance to particular pests or diseases, tolerance of drought or salt, tolerance of a specific herbicide, faster growth, or improved nutritional content. Yields rise and losses fall, and pesticide use may drop where a crop is pest-resistant. Against that: seed is usually more expensive and often has to be bought each season, small farmers may become dependent on one supplier, pests can evolve resistance, there are concerns about effects on non-target organisms and about gene transfer to wild relatives, and public acceptance and regulation vary widely between countries. |
| (e) Controlled environments | Greenhouses let the farmer control temperature, humidity, light and carbon dioxide concentration, so the crop grows at close to its optimum rate all year and the growing season is extended. Hydroponics grows plants with their roots in a nutrient solution rather than soil, so the exact ions needed are supplied and no soil-borne pests are present. Aeroponics suspends the roots in air and sprays them with nutrient solution, which uses even less water. All three give very high yields per unit area and allow production where the soil or climate is unsuitable, at the cost of high energy use and high set-up cost. |
| (f) Managed grazing: livestock rotation | Animals are moved between fenced areas on a planned cycle instead of grazing one area continuously. Each area is grazed hard for a short period and then rested, so the grass recovers and regrows, the roots stay strong, vegetation cover is maintained and the soil is not laid bare. It also breaks the life cycle of parasites and spreads manure evenly. The result is more grass grown per hectare and less overgrazing. |
| (g) Urban farming | Growing food within towns and cities — on rooftops, in allotments, in vertical farms and on unused land. Food is produced close to where it is eaten, so transport, cost and spoilage fall, and land with no agricultural alternative is brought into production. It also improves access to fresh food in cities. The area available is small, so it supplements rather than replaces rural agriculture, and urban soil may need testing for contamination. |
| (h) Agroforestry | Growing trees and crops (or livestock) together on the same land. The trees provide shade and shelter, reduce wind speed and so reduce erosion, their roots bind the soil and draw water and nutrients from deeper layers, and their fallen leaves add organic matter. They also yield a second product — fruit, nuts, timber or fodder — so the farmer has more than one source of income. The crop yield per hectare may be somewhat lower than in a cleared field, but the total output and the long-term soil condition are better. |
| (i) Inorganic NPK fertilisers | Manufactured fertilisers supplying nitrogen, phosphorus and potassium as soluble ions. Because the ions are already dissolved or dissolve quickly, they are available to the roots immediately, the exact quantity of each can be applied, and the effect on yield is large and fast. They are the single biggest reason world crop yields rose in the twentieth century. Their limitations are the energy and cost of manufacture, the fact that they add no organic matter so soil structure is not improved, and the leaching and eutrophication that follow overuse. |
| (j) Organic fertilisers | Crop residue (the stems and leaves left after harvest), manure and mulch (a layer of organic material spread on the surface). They release nutrients slowly as they decompose, so less is leached; they add organic matter, which improves soil structure, water retention and the population of soil organisms; and mulch additionally shades the soil, holds moisture in and suppresses weeds. They are often free or cheap on a mixed farm. Against that, the nutrient content is lower, less predictable and released more slowly, so large quantities must be spread, and the effect on yield in a single season is smaller. |
| (k) Chemical control of pests | Pesticides kill the organisms that reduce yield: insecticides for insect pests, herbicides for weeds competing for light, water and nutrients, and fungicides for fungal diseases. They act quickly, work over large areas, are relatively cheap, and can save a crop that is already under attack. Their limitations are that pests evolve resistance, that non-target organisms including pollinators and the pests' own predators are killed, and that residues can run off into water or persist along a food chain. |
| (l) Biological control of pests | Introducing or encouraging a natural predator, parasite or pathogen of the pest, so that the pest population is reduced without chemicals. It is specific to the target species, so pollinators and other organisms are not harmed; it does not leave residues; and once established it can be self-sustaining and costs little to maintain. Against that, it is slow to take effect, it reduces the pest rather than eliminating it, it does not help in an emergency, and an introduced control organism can itself become a problem if it has no predators in the new area — so it has to be researched carefully first. |
Learn them in four groups rather than as a list of twelve: how you arrange the land (mixed cropping and rotation, managed grazing, agroforestry, urban farming), what you add (inorganic fertilisers, organic fertilisers, irrigation), what you control (chemical pest control, biological pest control, controlled environments), and what you change about the crop or the work (genetically modified organisms, mechanisation). Four groups you can recall under pressure will get you to the item you need.
The mark scheme wants speed against persistence. Chemical: fast, broad, cheap, but resistance develops, non-target organisms are killed and residues spread. Biological: specific, no residues, self-sustaining, but slow, incomplete, and risky if the control organism spreads. Note that neither is simply better — the honest answer is that biological control suits a long-term programme and chemical control suits an outbreak, which is why many farms use both.
2.2.4 The impacts of unsustainable agricultural practices
Every item in this list is what happens when something in 2.2.3 is pushed too far. That is the way to hold it: the practice is not the problem, the over is. And each impact has a mechanism, because the command word is again describe and explain.
| Impact | The mechanism, and who it affects |
|---|---|
| (a) Overproduction of food: food wastage | Producing more than is eaten means that the land, water, fertiliser, fuel and labour used to grow the wasted portion are spent for nothing, and the food decomposes in landfill releasing methane. Waste happens at every stage: in the field when prices are too low to harvest, in storage and transport where refrigeration is poor, and in shops and homes. Reducing waste raises the food available without farming any more land at all, which is why it is listed first. |
| (b) Food shortages: cash crops and biofuel crops replacing food crops | Land is used to grow cash crops — coffee, cotton, soya beans, palm oil — or biofuel crops, because these earn more than staple food. The farmer's income rises and the country earns foreign currency, which is a genuine benefit. But less land grows food, so local food supply falls and prices rise, and the people who suffer are those who buy their food rather than grow it. Depending on one export crop also leaves a farmer or a country exposed when its world price falls. |
| (c) Mismanagement of irrigation | Three named consequences. Soil erosion: water applied too heavily washes soil off the surface. Salinisation: irrigation water contains dissolved salts; in a hot climate the water evaporates and leaves the salts behind, and repeated over years the salt concentration in the topsoil rises until crops cannot take up water and the land goes out of production. Water logging: applying more water than drains away fills the pore spaces, excluding air, so roots cannot respire. |
| (d) Overuse of pesticides | Pesticide resistance: a few individuals in the pest population happen to survive; they breed, and the resistant form spreads until the pesticide no longer works, so stronger or more frequent doses are needed. Pest resurgence: a broad pesticide also kills the pest's natural predators, so when the pest recovers there is nothing to hold it back and its numbers rebound higher than before. Impacts on pollinators: bees and other pollinating insects are killed or weakened, and since many crops depend on them, yields of those crops fall. |
| (e) Overuse of fertilisers | The chain runs: leaching — fertiliser applied in excess of what the crop can absorb dissolves in rainwater and drains into rivers and lakes; nutrient enrichment — the added nitrate and phosphate feed the algae and plants already there; eutrophication — algae multiply into a bloom that covers the surface, blocking light so the plants beneath die, and when the algae and plants die the decomposers multiply and use up the dissolved oxygen in the water, so fish and other aquatic animals suffocate. Learn that as an ordered chain: it is marked as one. |
| (f) Exhaustion of nutrients in soils | Growing crops and removing the harvest takes ions out of the soil year after year. If the same crop is grown repeatedly, the same ions are removed in the same proportion; if crop residues are burned or taken away rather than returned, the organic content falls too, so the soil loses both its nutrient store and the structure that organic matter gives it. Yields fall, and more fertiliser is needed each year to get the same result. |
| (g) Removal of natural vegetation | Deforestation clears the trees whose roots bound the soil and whose canopy intercepted the rain, so soil is exposed and washed away. Overcultivation works the land too often and too hard, without rest or added organic matter, breaking down soil structure. Overgrazing keeps too many animals on an area so grass is eaten faster than it regrows and the ground is left bare and trampled. All three end in the same place: exposed soil with nothing holding it. |
| (h) Monoculture and intensification | A single crop across a large area supports far fewer species than a varied landscape, so there is a loss of biodiversity; hedgerows and field margins are removed to make bigger fields, taking away the remaining habitat. Because one crop attracts one set of pests, more pesticide is needed, and because one crop draws the same ions, more fertiliser is needed — and both lead to soil and water pollution. Intensification also concentrates livestock, so slurry and nutrients are produced in quantities the local land cannot absorb. |
| (i) Soil erosion | The end point of most of the above, and the syllabus names it as loss of topsoil and nutrients: the topsoil — the thin upper layer that holds the organic matter and most of the nutrients — is washed or blown away. What is left is less fertile, holds less water and grows less, so yields fall permanently. Topsoil forms at a rate of millimetres per century, so on any human timescale this is a loss that cannot be made good. Sub-topic 2.3 takes this apart properly. |
Leaching → enrichment → algal bloom → light blocked → decomposers use the oxygen. The final mark is nearly always the oxygen: fish die because decomposers respiring aerobically have removed the dissolved oxygen, not because the algae poisoned them. Write “dissolved oxygen” and you have it.
160 to 200 kg: 8.7 − 8.5 = 0.2 t per hectare.
The same 40 kg of nitrogen, and the same cost, buys three times as much grain the first time as the second. Earlier still, 40 to 80 kg gained 1.6 t. This is what diminishing returns means, and quoting two of these steps is worth more than the phrase on its own.
The nitrogen the crop does not take up stays as nitrate ions dissolved in the soil water, and nitrate is very soluble, so rain washes it down through the soil and into groundwater, streams and lakes — this is leaching. In the water it acts as a fertiliser for algae, which is nutrient enrichment, and the sequence that follows is eutrophication: algae multiply and form a surface bloom, the bloom blocks light so the plants beneath it die, bacteria decompose the dead material and use up the dissolved oxygen in doing so, and fish and other aquatic animals suffocate. So the fertiliser above the optimum is paid for twice, once at the farm gate and once in the river.
Against: the last 40 kg gains only 0.2 t, so the fertiliser may cost more than the extra grain is worth; the surplus nitrate is the fraction most likely to leach; and the margin for error is small, since the curve turns over immediately after the peak and a slightly heavy application loses yield.
Judgement: no — a rate near 160 kg is the better choice, because it gives 8.5 t, within 0.2 t of the maximum, for 20 per cent less fertiliser and less leaching. What the judgement depends on is the price of fertiliser against the price of grain, and how close the field is to a watercourse. Splitting the dose across the season, testing the soil first, and using organic fertiliser for part of it would all reduce the loss further.
Why this sub-topic is the one to get right
Soil erosion is where 2.1 and 2.2 arrive. It has the cleanest cause-impact-strategy chain on the whole syllabus, and Cambridge examines it as a chain: a question will give you a photograph or a description of a hillside, ask you to identify the causes, then the consequences, then what could be done. If you can hold the chain, you can answer almost any version of it.
Start from one fact that makes everything else make sense. Topsoil is the thin upper layer that holds the organic matter and most of the nutrients, and it forms at a rate of a few millimetres per century. A single storm can remove what took hundreds of years to build. That is why soil erosion is treated as a permanent loss rather than a temporary problem, and saying so is very often the evaluation mark.
Soil is lost when it is left bare, and it is held when it is covered. Every cause in 2.3.1 is a way of exposing soil; every strategy in 2.3.3 either puts a cover back on it, slows the water moving over it, or slows the wind moving across it. If you forget a specific item in the exam, work back from that sentence and you will construct a creditable answer.
2.3.1 The causes of soil erosion
| Cause | How it exposes or removes the soil |
|---|---|
| (a) Unsustainable agricultural practices | Ploughing up and down a slope creates channels that run water straight downhill. Overcultivation without rest or added organic matter breaks down soil structure so the particles no longer hold together. Removing crop residues instead of returning them leaves the surface bare between harvests. Heavy machinery compacts the soil so rain cannot soak in and runs off the surface instead. |
| (b) Deforestation | Tree roots bind the soil together and the canopy intercepts the rain, so drops reach the ground gently and some water evaporates before it lands. Remove the trees and rain strikes bare soil at full force, dislodging particles, while there are no roots left to hold what remains. Deforested slopes are where erosion is fastest and most visible. |
| (c) Farming on steep slopes | Water runs faster downhill on a steep slope, and faster water carries more and larger particles. Gravity also moves loosened soil directly. The steeper the slope, the more soil a given rainfall removes. |
| (d) Bare soil | Soil with no vegetation cover has nothing to intercept the rain, nothing to bind it and nothing to slow the wind across it. Land is left bare between crops, after overgrazing, after burning, or during preparation for planting — and it is precisely in those gaps that most erosion happens. |
| (e) Wind and water erosion | These are the two agents that actually do the removing. Water: raindrops dislodge particles on impact, and surface run-off carries them away, first as a thin sheet and then in channels that grow deeper as more water is funnelled into them. (Geography names those channels rills while they are small and gullies once they are deep. That classification is background here — 0680 asks only for wind and water as the two agents.) Wind: dry, loose, fine particles with no vegetation to slow the air are lifted and blown away, which is why erosion by wind is worst on dry, bare, flat land. |
2.3.2 The impacts of soil erosion
| Impact | The mechanism |
|---|---|
| (a) Silting of rivers | Eroded soil is carried into rivers, where it settles as sediment. The river bed rises, so the channel holds less water and floods more readily; reservoirs behind dams fill with silt and lose capacity; irrigation channels and harbours must be dredged; and suspended sediment blocks light and smothers the habitats of river organisms. |
| (b) Desertification | Where topsoil is lost and vegetation cannot re-establish, land in dry regions gradually becomes desert-like: less soil holds less water, so fewer plants grow, so less soil is held and more is lost. It is a self-reinforcing loop, which is why it is so difficult to reverse once it starts. |
| (c) Mass movement: landslides, rockslides and mudslides | Without roots binding it and with water saturating it, a slope loses stability and a large volume of material moves downhill at once. This can destroy homes, roads and farmland and cause loss of life, and it happens most where slopes have been deforested or cut into. The three names are just the material that moves and the way it moves: a landslide is soil and loose material sliding down a slope as a mass; a rockslide is the same movement in rock that has broken away from a cliff or a cut face; a mudslide is soil so saturated by heavy rain that it flows rather than slides. One clause each is enough — the objective asks for mass movement as an impact, not for the geology of it. |
| (d) Loss of habitats and biodiversity | Soil is a habitat in itself, for bacteria, fungi, insects and earthworms; losing it removes them and the plants that depend on them. Silt washed downstream also damages river and coastal habitats, so the loss is not confined to the field it came from. |
| (e) Reduction in crop yield | The topsoil carried away is the layer holding the organic matter and most of the nutrients, and the remaining subsoil holds less water and has poorer structure. Yields fall, and the farmer must spend more on fertiliser and irrigation to get less. |
| (f) Malnutrition and famine | Where people depend on the food they grow, falling yields mean less food and less income to buy any. Persistent shortage causes malnutrition, and a harvest failure on already degraded land can cause famine. This is the point at which an environmental problem becomes a human one. |
| (g) Displacement of people | When land can no longer support the people farming it, they move — usually to cities, sometimes across borders. That puts pressure on housing, water and services where they arrive, and the land they leave often degrades further with nobody managing it. |
An answer that reads “topsoil is lost, so yields fall, so farmers have less food and less income, so malnutrition rises and people move away” scores far better than four separate bullet points, because each “so” is the link the mark scheme is looking for. The same trick works upstream: “soil is washed into the river, so the bed rises, so the channel holds less water, so flooding is more frequent.”
2.3.3 Strategies to reduce soil erosion
The syllabus gives each strategy together with the reason it works — that is unusually generous, and it means the mechanism is examinable. Learn each strategy with its mechanism attached.
| Strategy | How it works (the syllabus gives these reasons, so use its words) |
|---|---|
| (a) Terracing | Reduces movement of soil and surface run-off. A long slope is cut into a series of level steps, each with a lip. Water reaching a step stops and soaks in rather than running on, so it never builds up the speed needed to carry soil, and any soil that does move is caught on the step below. Terracing makes steep land farmable at all, but it is very labour-intensive to build and must be maintained, or a collapsed terrace concentrates the water instead. |
| (b) Contour ploughing | Reduces surface run-off. The field is ploughed along the contours — across the slope rather than up and down it — so each furrow lies horizontally and acts as a small barrier holding water back and letting it infiltrate. Ploughing up and down does the opposite: every furrow becomes a channel guiding water straight downhill. It costs nothing extra beyond driving in a different direction, which makes it one of the highest-value strategies on the list. |
| (c) Bunds | Reduces surface run-off, reduces wind speed and wind erosion. Bunds are low banks or walls of earth or stone built across a slope or around a field. They trap water behind them so it soaks in rather than running off, and they trap soil that is already moving. Standing above the surface, they also break the wind at ground level. They are cheap, can be built from local material, and are widely used in dry regions. |
| (d) Wind breaks | Protects crops, reduces wind speed and wind erosion. Rows of trees or hedges planted across the prevailing wind slow the air before it reaches the field, so it can no longer lift dry soil particles, and the crop itself is not damaged or dried out by strong wind. The trees also provide shade, habitat and sometimes fruit or timber. They occupy some land and compete with the crop at the field edge. |
| (e) Maintaining vegetation cover | Roots bind the soil, and the vegetation reduces surface run-off and absorbs water. Keeping something growing — a cover crop between harvests, grass strips, or simply not clearing the land — means the leaves intercept the rain so it does not strike bare soil, the roots hold the particles together, and the plants take up water so less runs off. It is the single most effective thing a farmer can do, and it is the direct answer to cause (d), bare soil. |
| (f) Addition of organic matter | Improves soil structure. Manure, compost, mulch and returned crop residues bind fine particles into larger crumbs that are heavier and harder to wash or blow away, and that leave larger pore spaces so water soaks in instead of running off. Organic matter also holds water like a sponge and feeds the soil organisms whose activity maintains the structure. It works slowly and needs to be repeated. |
Water on a slope → terracing, contour ploughing, bunds. Wind on flat dry land → wind breaks, bunds. Bare soil anywhere → maintain vegetation cover, add organic matter. Bunds appear in two of the three because the syllabus credits them for both water and wind — which makes them a safe answer when you are not sure which agent a question is describing.
| Field | Slope gradient | Ground cover | Soil loss / tonnes per hectare per year |
|---|---|---|---|
| Field P | 3° | crop, soil bare between the rows | 4 |
| Field Q | 8° | crop, soil bare between the rows | 18 |
| Field R | 15° | crop, soil bare between the rows | 42 |
| Field S | 15° | terraced, with a cover crop | 9 |
The impact on the river: the soil washed off these fields is carried into it and settles as sediment, which is silting. The river bed rises, so the channel holds less water and floods more readily; suspended sediment also blocks light and smothers the habitats of river organisms. Field P is the field next to the river, so what leaves it arrives fastest.