Leak Detection Bexley

Same-day appointments are usually available in Bexley, and next-day almost always. If water is actively escaping, tell us when you book. Live leaks are prioritised and we can talk you through isolating the supply while an engineer travels.

Not on a leak arising within your own property that we cannot find: in Bexley that detection fee is waived. Trace it instead to a neighbour's pipework, a shared riser or the water main beyond your boundary and the fee stands, because that is a located leak, and it is the finding that moves the repair bill off you.

Yes. Trace and access reports documenting the cause, precise origin and affected areas are available for every Bexley detection visit, typically within 48 hours. They are structured the way UK loss adjusters expect.

All of it, including Bexleyheath, Sidcup, Welling, Erith, Crayford. We cover every London borough, so coverage never depends on which side of a postcode line you live.

No, and on a suspended timber floor it is close to expected. Once water reaches the void it is routed by the timber and by the fall of the oversite, not by where it came from. The reliable approach is to open the void rather than the floor: a borescope through an airbrick or a lifted board in an unfinished area, relative humidity and timber moisture readings taken at several points along the joist run so a gradient can be established, and the direction of that gradient followed back. A gradient that climbs towards the rear wall points to the bathroom stack. A gradient that is flat and highest near the airbricks usually points to ventilation and ground moisture instead.

By testing what the water is, not only how much there is. Mains supply water and heating system water carry different dissolved content from ground moisture, and a chloride or conductivity check on a sample drawn from the wet timber will usually separate them. Heating water additionally carries inhibitor and corrosion product and tends to stain differently. Alongside that, an isolated meter test on the incoming supply and a timed pressure decay on the sealed heating tell you whether either system is actually losing volume. If both hold and the sample reads as ground moisture, the correct finding is a ventilation and oversite issue, and we say so rather than recommending pipework to be opened.

By measuring the timber rather than judging the air. Structural softwood in a ventilated subfloor sits in equilibrium at a moisture content in the mid teens by percentage, and wet rot becomes a realistic risk when it stays above roughly twenty per cent for a sustained period. A resistance meter with insulated probe pins driven into the joist at depth gives a reading of the timber itself, which is what matters, whereas a surface reading on a board tells you about the last hour. Readings are taken at several points along the run and repeated over successive visits, because a falling trend is the evidence that drying is working. Where mechanical drying is used, the void needs air movement as well as dehumidification, since a sealed void with a dehumidifier in it will dry the air and leave the joist wet.

Frequently. A suspended timber floor depends on a through draught between opposing walls to carry away moisture evaporating from the ground beneath, and that draught is entirely dependent on the airbricks staying clear. Raised garden levels, patios laid over them, render carried across them, insulation packed into the void and modern extensions built across one elevation all reduce or eliminate the cross flow. Once the void stops ventilating, ground moisture accumulates, timber moisture content climbs and the underside of the boards can be persistently damp with no plumbing fault whatever. Counting the airbricks on each elevation, confirming they are open through the full wall thickness rather than blocked internally, and checking that the extension has not sealed one side is a short exercise with a definite answer.