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Why China’s $80B South-North Water Project Is Quietly Failing

November 8, 2026 · 19 min

The South-North Water Transfer is the largest water diversion project ever built. It moves water more than a thousand kilometers from the wet Yangtze basin to China’s dry north, and by 2026 its central route alone had delivered more than 80 billion cubic meters to nearly 118 million people. By the headline numbers, it works.

This video argues that the project is failing quietly rather than dramatically. Canals don’t collapse. They silt up, their linings crack, and their pumps run longer every year. The water still arrives, but three physical forces, silt, frost and energy, keep raising the price of keeping it that way.

A national water grid

Northern China holds about half the country’s people and only about seven percent of its water, and decades of overpumping had drained its groundwater. Approved in 2002, the project is three routes linking the Yangtze, Huai, Yellow and Hai rivers across roughly 4,350 kilometers, with a design target of 44.8 billion cubic meters a year. The central route is a gravity canal that flows downhill for over a thousand kilometers without a pump, made possible by raising the Danjiangkou dam and tunneling under the Yellow River. It now serves 27 cities and 243 counties. Cost estimates range from about 62 billion dollars to around 80 billion for the finished eastern and central routes, depending on what is counted.

Silt and salt

Long stretches cross alluvial and swelling clay soils. Summer rains from July to September cut the banks, and the eroded material settles wherever the flow slows. Near Diaonan, repeated slope collapses filled a central route reach with sediment and forced continuous dredging to hold design flow. Where groundwater rises, evaporation leaves “white salt frost” crusts that damage soil, plants and some lining materials. Downstream reservoirs also accumulate nutrients in their sediment, with total nitrogen and carbon rising about 2.35 and 3.05 times.

Frost heave

In the cold northern sections, freezing soil pulls water up into ice lenses that lift the concrete slabs above them. When they thaw, the slabs settle unevenly, crack, bulge and dislocate, and the anti-seepage lining starts leaking. A sand and gravel cushion cut peak heave in tests from about 4.26 to 0.95 centimeters, but it has to be designed for each stretch and installed under a canal that can’t be shut down. Older canals in Henan and Xinjiang show what deferred repairs look like.

The pumping bill

The eastern route has no gravity to lean on. It runs about 1,152 kilometers and relies on roughly 23 pumping stations with about 454 megawatts of installed power. From late 2013 to mid-2017 it used about 2.35 billion kilowatt-hours to move 15.5 billion cubic meters, roughly 0.15 kWh per cubic meter, with a footprint of about 1.93 million tonnes of CO2 equivalent. The 2022 Yangtze drought showed how water and power shortages can arrive together. The route also reused the polluted Grand Canal, which required hundreds of cleanup projects.

Shortfalls and side effects

The central route was designed for 9.5 billion cubic meters a year but has averaged about 9.02 billion, falling to 2.26 billion in dry years. A new Yangtze-to-Han transfer props up the reservoir but lowers water quality on the lower Han. One study estimated more than 38,000 tonnes of pollutants redistributed between basins, and resettlement displaced roughly 330,000 to 375,000 people. The western route, climbing above 3,000 meters onto the plateau, remains unbuilt.

A success that keeps costing more

The project has recharged aquifers and supplies drinking water to cities that badly needed it. A 2025 review credited it with better water security for more than 150 million people, while noting rising costs, resettlement and uncertain long-term environmental effects. Critics also argue it adds supply without fixing how the north uses water.

Key takeaways

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