Why slab leaks are common under older Newark homes

A lot of Newark was built slab-on-grade in the 1960s and 1970s, which means the home sits directly on a concrete slab and the water lines run inside or beneath that slab instead of through a crawlspace. When a supply line under the slab springs a leak, you cannot just look under the house and see it. The water is trapped below the concrete, and the first clue is usually indirect: a water bill that climbs for no reason, a warm spot on the floor over a hot line, or the faint sound of water running when every fixture is off.
After fifty or sixty years, the original copper under those slabs is at the age where pinhole leaks start showing up. Newark's water from the Alameda County Water District is moderately hard, and over decades that mineral content works on copper from the inside, which is one of the reasons a single pinhole can turn into several across the same run. We see this pattern across the older slab homes in Old Town Newark and Lakeshore in particular.







