IB ESS HL Topic 4 — Water Paper 2 — HL only Core idea ~11 min read

What Good Water Quality Looks Like (HL)

At HL you need more than “the water is polluted”. You need to know which pollutants matter in aquatic systems, what each one does to living things, and why some water bodies run out of oxygen even when nothing obviously toxic has been added.

📚 What you need to know

The main aquatic pollutants at HL

Organic matter

Untreated sewage and animal waste add a large mass of biological material. Bacteria break it down aerobically, consuming dissolved oxygen as they respire, and the resulting oxygen shortage kills fish and invertebrates. Rivers running through fast-growing cities without adequate treatment show this pattern clearly.

Dissolved substances

Some chemicals dissolve and act at very low concentrations. A well-known example is tributyltin (TBT), once painted onto ship hulls to stop organisms growing on them. It leached into the water and disrupted the hormone systems of marine animals, causing reproductive failure in molluscs and sharp declines in oyster populations before it was banned.

Why TBT is a favourite exam example: it shows a pollutant that was deliberately designed to be toxic to marine life, worked exactly as intended, and then affected species nobody was targeting. It also shows regulation working — populations recovered after the ban.

Persistent organic pollutants (POPs)

POPs such as polychlorinated biphenyls (PCBs) share three dangerous properties:

Put those together and top marine predators end up with the highest loads through biomagnification, causing immune and reproductive problems in animals that live far from any factory.

Plastics

Larger items cause entanglement and blockage of digestive systems. Microplastics enter food chains from the bottom and carry adsorbed toxins with them.

Heat energy

Thermal pollution is warm water discharged from power stations and industrial cooling systems. It causes a double problem: warm water holds less dissolved oxygen, while at the same time it speeds up metabolism, so organisms need more oxygen just as there is less available. Cold-adapted species are pushed out.

Harmful algal blooms

SettingMain organismsToxin and effect
Freshwater lakes and reservoirsCyanobacteria, often called blue-green algaeCyanotoxins contaminate drinking water, damage the liver and affect the nervous system of animals and humans
Coastal and marine watersDinoflagellates, a type of protistNeurotoxins accumulate in shellfish and can cause paralytic shellfish poisoning in people who eat them

HABs damage water quality in two separate ways, and a good answer names both:

The economic consequences are real: fisheries close, shellfish beds are shut for weeks, beaches are declared unsafe, and coastal tourism income drops.

A bloom is not automatically “harmful” in the technical sense. HAB is reserved for blooms that produce toxins or cause serious oxygen depletion. Use the term precisely and you look like you know the topic.

Hypoxia, anoxia and dead zones

Definitions Hypoxic water — oxygen too low to support most aquatic life
Anoxic water — oxygen effectively absent
Dead zone — an area where marine organisms cannot survive

Dead zones cluster in coastal regions receiving high nutrient run-off, especially where a large river drains intensive farmland into a sea that mixes slowly. They cause severe disruption to marine food chains and can collapse local fisheries.

Why layering makes it worse

This is the part most students miss. Nutrients start the problem, but thermal stratification is what locks it in.

THERMAL STRATIFICATION AND DEAD ZONES Warm water floats on cold water, and the two stop mixing WARM SURFACE LAYER oxygen from the air and from photosynthesis THERMOCLINE — sharp change in temperature COLD, DARK BOTTOM WATER no mixing, so oxygen is not resupplied dead material sinks and decomposes here hypoxia or anoxia develops: a dead zone forms Nutrients start the problem; stratification traps it Autumn cooling and storms break the layers and let the water mix again
The red cross marks blocked mixing. Oxygen-rich surface water cannot reach the bottom, so the oxygen used by decomposers down there is never replaced.

🧩 The four causes of hypoxia and anoxia

  1. Eutrophication — excess nutrients fuel blooms; the decomposition of dead algae consumes the oxygen.
  2. Sewage disposal — organic matter gives decomposers even more to work on.
  3. Thermal stratification — layers by temperature stop oxygen-rich surface water reaching the depths.
  4. Global warming — warmer water holds less dissolved oxygen and stratifies more strongly, so hypoxic conditions are expected to become more common.
EXAM PRACTICE

Explain why coastal dead zones are usually worst in late summer. [4]

Point 1: less oxygen can dissolve Warm summer water holds less dissolved oxygen than cold water, so the starting supply is lower. Point 2: demand is higher Warmth speeds up decomposition and respiration, so organisms use oxygen faster. Point 3: no resupply Strong summer stratification stops oxygen-rich surface water mixing downwards. Point 4: peak organic load Spring and summer nutrient run-off has already produced blooms, and that dead algal material is now sinking and decomposing. Low supply, high demand and no mixing all peak together in late summer Whenever a question says “why then” or “why there”, look for several factors coinciding.

💡 Exam tip

⚠️ Common mix-up

Up next: How Sewage Is Treated (HL) — the three stages, and why the technology existing is not the same as the technology being available.

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