How tap water is made
From a river or borehole to your tap, through a sequence of barriers designed so that no single one has to work perfectly.
Public water supply is built on a principle called the multiple barrier approach. No single process is trusted to handle everything, because every process has a failure mode. The barriers are arranged so that the failure of one is caught by another.
The barriers, and what each is for
- Catchment protectionThe first and cheapest barrier: keeping contamination out of the source in the first place, through abstraction protection zones, land management agreements and pollution control.Every contaminant excluded here is one that does not need removing later.
- ScreeningCoarse and fine screens remove debris, leaves and larger material that would damage downstream plant.
- Coagulation and flocculationA metal salt neutralises the charge keeping fine particles suspended so they clump into settleable flocs. Also removes much of the natural organic matter that would otherwise form disinfection by-products.
- SedimentationFlocs settle out under gravity in large tanks, removing the bulk of the solids load before filtration.
- FiltrationSand, multimedia or membrane filtration removes what remains. This is the critical barrier against Cryptosporidium, which chlorine cannot kill.Filter performance is monitored continuously by turbidity, because a microbiological result takes at least a day and a filter can fail in minutes.
- Activated carbonAdsorbs pesticides, taste and odour compounds and other organics that pass through the earlier stages.
- DisinfectionChlorine, ultraviolet light or ozone inactivates bacteria and viruses. UV is used specifically because it works against the chlorine-resistant protozoa.
- ConditioningpH adjustment for corrosion control, orthophosphate dosing where lead pipes remain, and a chlorine residual for the journey through the network.
Why groundwater is different
A borehole in a confined chalk or sandstone aquifer may need almost no treatment. The aquifer has already provided filtration over years or decades of percolation, and the water arrives clear, cool and microbiologically clean. Many groundwater sources go to supply with disinfection alone, sometimes with iron and manganese removal.
The trade-off is that groundwater carries whatever the geology and past land use put into it — nitrate from decades-old fertiliser, naturally occurring arsenic or fluoride — and those are much harder to remove than particles.
What happens after the works
Treated water goes to a service reservoir, which balances the steady output of the works against the peaky demand of a city. From there it enters the distribution network — hundreds of thousands of kilometres of it nationally, much of it a century old.
The network is where a surprising share of water quality problems originate: iron and manganese deposits accumulated over decades and released by a change in flow, ingress through a defect during a pressure loss, or growth in a low-turnover section. This is why a chlorine residual is maintained and why a supplier’s response to a discoloration complaint is usually flushing rather than anything at the works.
Sources
- World Health Organization — Guidelines for Drinking-water Quality. Public but restricted · CC BY-NC-SA 3.0 IGO
- Drinking Water Inspectorate — Drinking water quality in England and Wales. Open — attribution required · Open Government Licence v3.0
- American Water Works Association — AWWA standards, water audits and utility benchmarking. Public but restricted · Publisher terms — public access, reuse not clearly granted