Explain how water consumption varies with economic development, describe the global water‑resource base and the human‑water‑cycle, and evaluate the physical and human factors that influence water supply and demand.
Cambridge expects candidates to know the four major natural water‑resource categories, their approximate share of the Earth’s fresh water, and the relevance of reservoirs.
The human‑water‑cycle is a **system**: water moves between stores (rivers, aquifers, reservoirs) via transfers (abstraction, conveyance) and produces outputs (use, disposal). Human activities modify each stage.
| Stage | Definition | Typical Human Modification (example) |
|---|---|---|
| Capture | Extraction from natural stores (river abstraction, well‑pumping) | Irrigation intake from the Nile |
| Storage | Holding water in reservoirs, dams or aquifers | Three‑Gorges Dam reservoir |
| Use | Application in domestic, industrial or agricultural activities | Cooling‑water circuit in a steel plant |
| Disposal | Return of used water to the environment (run‑off, effluent) | Untreated wastewater discharged into the Ganges |
| Reuse | Recovery and recycling of water for a second use | Water‑recycling plant in Singapore |
As a country moves from Stage 1 → Stage 2 → Stage 3, the pattern of water use changes not only in magnitude but also in sectoral composition. The rise in per‑capita consumption during Stage 2 reflects increased domestic demand (appliances, indoor plumbing) and industrial expansion. In Stage 3, technological improvements, water‑saving policies and a shift toward less water‑intensive services cause the per‑capita curve to level off or decline, illustrating the syllabus’s “change over time” concept.
| Development Stage | Typical GDP per capita (US$) | Per‑capita water consumption Wpc (m³ yr⁻¹) | Water‑use intensity WUI (m³ US$⁻¹) |
|---|---|---|---|
| Low‑income | ≤ 2 000 | ≈ 50 | ≈ 0.025 |
| Middle‑income | 2 000 – 12 000 | ≈ 150 | ≈ 0.0125 |
| High‑income | > 12 000 | ≈ 200 | ≈ 0.0083 |
The water‑use intensity is calculated as:
$$WUI=\frac{W_{\text{total}}}{\text{GDP}}$$
where Wtotal is total annual water abstraction (m³) and GDP is gross domestic product (US$).
Two thresholds are used in the syllabus:
In water‑scarce regions (e.g., the Middle East) the three‑stage curve is shifted left: even low‑income economies show relatively high domestic per‑capita use, and the Stage 3 plateau occurs at a lower absolute value because of limited supply. In water‑rich regions (e.g., Canada) the curve is broader and the plateau occurs at higher values.
| Driver | Effect on Water Availability | Illustrative Example |
|---|---|---|
| Climate (precipitation & temperature) | Controls recharge of rivers and aquifers | Monsoon‑driven flow of the Ganges supports Bangladesh’s agriculture |
| Geology & soil type | Determines groundwater storage capacity | Karst limestone in the Yucatán yields high‑yield aquifers |
| Relief & drainage pattern | Influences runoff speed and flood risk | Steep Andes create rapid river discharge in Peru |
| Water‑body size & connectivity | Sets the volume of surface water that can be abstracted | Great Lakes provide a vast, shared supply for the US‑Canada border |
| Trans‑boundary arrangements | Can restrict or enhance access depending on treaties | Indus Water Treaty governs allocations between India and Pakistan |
| Land‑use change (deforestation, urbanisation) | Alters runoff, infiltration and sediment load, affecting both surface and groundwater availability | Deforestation in the Amazon reduces groundwater recharge and increases river sedimentation |
| Driver | Effect on Water Demand | Illustrative Example |
|---|---|---|
| Population size & growth | Directly raises domestic and municipal demand | Rapid urban growth in Lagos increases per‑capita water needs |
| GDP per capita & income | Higher incomes raise domestic appliance use and service‑sector water demand | Japan’s high per‑capita consumption despite low industrial water use |
| Sectoral composition (agri‑industrial‑service) | Industrial and agricultural sectors are the most water‑intensive | Brazil’s soy‑expansion drives massive irrigation demand |
| Seasonality & climate‑linked demand | Peak irrigation in dry months; higher domestic use in hot summers | Australian Murray‑Darling basin sees irrigation spikes in summer |
| Technology & efficiency | Improved cooling, drip‑irrigation, and leak‑reduction lower demand | China’s adoption of closed‑loop cooling in power stations |
| Policy, pricing & regulation | Tariffs and allocation rules can curb wasteful use | UK’s increasing water charges encourage household conservation |
| Cultural factors | Values, habits and social norms influence water‑use behaviour (e.g., bathing frequency, garden watering) | High‑frequency showers in Mediterranean cultures increase domestic demand |
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