Who this guide is for
- Owners who have noticed water standing somewhere on a site
- Operators inheriting drainage features with no record
- Self-builders reviewing a scheme with several features in series
- Anyone about to report a drainage feature as faulty
- Readers who want the readings for each feature set side by side
Establish which arrangement it is before reading anything
The sharpest available test is whether the arrangement has a designed outflow connection. An infiltration structure has none, because everything entering leaves through the surrounding soil and the overflow exists for the day that stops being true. Attenuation always has one, because its purpose is to limit the rate at which water leaves.
Where that cannot be established on site, it is established from the drawings and the handover record. The entries are consistent that the visible feature is frequently identical in both cases, and only the documentation tells them apart.
An attenuation store
Filling is the expected behaviour, and a store that never fills is not doing the work its site is relying on. What carries the information is the emptying, because the store is ready for the next event only once the control has passed everything held from the last.
The entry is explicit that storage standing full is not evidence the system is working, and that on a store which should have recovered it is evidence something has stopped. The same sight is therefore read differently depending on when it is seen relative to the rain.
An infiltration structure
Standing water immediately after a heavy event is expected here too. Water arrives quickly and the ground accepts it slowly, and the void exists only to reconcile those two clocks.
The entry draws the line by duration rather than by presence: water still standing long afterwards says something about the ground rather than about the structure. A part-full void when the next event arrives behaves like a smaller one, which is how an arrangement that performed through a dry summer surcharges in a wet autumn with nothing altered.
A permeable pavement
Two different observations are available on a pavement and they point at different layers. Water standing on the surface usually reports a blockage in the openings or the laying course rather than an inability of the ground to take water, because permeability is a chain and the chain is only as open as its most closed link.
A full storage layer beneath is the observation that means opposite things. Lined, the store cannot empty downward at all and the flow control is the only exit; unlined, the ground sets the pace. Which of the pavement's three possible roles it was built for decides which reading applies.
A rain garden
The feature is arranged to drain down between events rather than to hold a standing water level at all, so it is not a pond and was never intended to look like one. Brief ponding in the surface zone is the working range being used.
Water held for a long time after rain is telling you about the medium or the underdrain rather than about the weather. Where the base is lined, the underdrain and its outfall are the only exit, so the same observation can be reporting a surcharged pipe well away from the feature.
A swale
A swale is wet by design and its surroundings have to tolerate that, so water moving along it is the arrangement working. The design question the entry raises is what happens along the route if the swale ponds for longer than intended once it silts.
Where an underdrain is present, a clogging soil interface becomes a maintenance matter rather than a failure, because a downward exit still exists. Where it is absent, standing water along the channel is reporting on the soil interface being sealed by the sediment the vegetation was meant to trap.
A roof arranged to hold water
This is the reading that reverses most completely. Water standing on an attenuation roof is the design working, and the entry warns directly that clearing the restriction to make the roof drain faster defeats the purpose and disables the arrangement the site's drainage was designed around.
It also notes the uncomfortable fact underneath: such a roof looks exactly like a defective flat roof holding water. Recording that the behaviour is intended, and how the restriction works, is what gives anyone arriving later a reason not to clear it.
The observation worth making instead
Across all of these, the useful measurement is time rather than level. How long the feature takes to clear, whether that is changing, and whether rain returning before it has cleared is a routine event on this site are what the records treat as diagnostic.
What a particular drain-down time means, and whether it is within what the design assumed, is a determination for the drainage designer. What an owner can do is establish the baseline while the arrangement is still new and keep it with the property.
Reading a drainage feature checklist
- 1Establish whether the arrangement has a designed outflow connection
- 2Find out from the record whether the feature is lined or open to the ground
- 3Confirm which role a permeable pavement was built for before reading its store
- 4Note whether water is on the surface or within the layers beneath it
- 5Record how long after rain the observation was made
- 6Record how long the feature then takes to clear
- 7Compare that against any earlier observation of the same feature
- 8Check whether anything new drains onto the feature since it was built
- 9Check the inlets upstream, since surcharge frequently surfaces there first
- 10For a roof holding water, confirm from the record that the behaviour is intended
- 11Photograph what you see, with the date and the weather preceding it
- 12Report the observation rather than acting on it, and say which feature it came from
Common mistakes to avoid
- Reading a full store as proof an arrangement is working
- Reading a full store as proof an arrangement has failed
- Clearing a flow restriction on a roof built to hold water
- Assuming surface ponding on a permeable pavement reports the ground beneath
- Treating a rain garden as a pond and its brief ponding as a defect
- Diagnosing a lined feature as though it could infiltrate
- Making the observation without recording when it rained
When to involve a professional
- What a given observation means is a determination for the drainage designer
- Establish whether the arrangement attenuates, infiltrates or is lined before reading it
- Standing water on a roof designed to hold it is intended behaviour
- Standing water in a landscape carries safety and amenity considerations
- Requirements vary by location and project; verify with your professionals
Frequently asked questions
Questions readers ask about this topic
How do I tell an attenuating feature from an infiltrating one?
Look for a designed outflow connection. Attenuation always has one, because it exists to throttle the rate water leaves. Infiltration has none, since everything entering leaves through the soil and its overflow exists only for the day that stops being true.
Water stands on my permeable drive after rain. Is the ground refusing it?
The entry suggests the more likely reading is a blockage in the surface openings or the laying course, because permeability is a chain and water fills the layer above the most closed link. Which layer is responsible is established by someone who can look into the build-up.
How long should a feature take to clear?
No general answer exists, because drain-down depends on the ground, the medium, the control and what arrives. What the records treat as diagnostic is change: a feature taking noticeably longer each season with nothing visibly altered is the observation worth reporting.
Should I clear a restriction that seems to be holding water back?
Not before establishing what it is. On a roof arranged to attenuate, the restriction is the element the whole concept depends on, and enlarging or removing it in the belief the roof drains poorly disables the arrangement the site drainage was built around.
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