Why slab leaks come up so often here
Slab-on-grade has been the standard foundation in San Diego since the tract building of the 1950s, which puts a substantial amount of supply pipe inside or beneath concrete with no crawlspace, no access panel and nothing to lift. A line in that position cannot be inspected, reached or even seen without opening the floor over it — which is what makes locating equipment central here rather than optional: without it, the alternative to finding the leak is not looking at the pipe, it is opening concrete speculatively until something turns up.
The water itself contributes. San Diego's supply is hard — the city's own reporting puts total hardness in the region of 216 to 284 parts per million, roughly 12.6 to 16 grains per gallon, varying with the treatment plant and the seasonal blend of Colorado River and State Water Project water. Mineral-heavy water is the mechanism behind pinhole failures in copper that has been sound for decades: the pipe does not fail because something happened to it, it fails from the inside out, which is why a first slab leak on an older copper system is worth treating as information about the whole run.
Age matters on top of that. A postwar home may still be on its original galvanised supply lines, which fail by internal corrosion along their length rather than at a single identifiable point — and a line failing that way tends to produce a second leak not long after the first. Ground that moves seasonally is a further contributor, because it puts stress on rigid pipe cast into or beneath a slab, and stressed pipe fails at whatever point was already weakest.