Why 358-Foot Elevation Creates More Underground Plumbing Stress
A pool at 150 feet above sea level in a valley community goes through a thermal cycle each year. Winter contracts the surrounding soil and the pool structure. Summer expands both. The plumbing joints throughout the underground system move slightly with each cycle. Over 40 or 50 years, the accumulation of those tiny movements creates micro fractures in the joint material that eventually become active water loss points. This happens at every elevation. What makes Blue Bell different is the magnitude of each cycle at 358 feet.
The gap between the coldest nights of a Blue Bell January and the warmest days of a Blue Bell July is larger than the same gap in lower-lying communities in the Schuylkill or Wissahickon valleys below. Each thermal cycle like each expansion and contraction of underground plumbing joints moves slightly further in Blue Bell than at lower elevations. Over 40 or 50 years, those slightly larger individual movements accumulate into more total stress on the joints.Â
A pool from the 1970s in Blue Bell at 358 feet has experienced more cumulative thermal movement in its underground plumbing than a pool of the exact same age in a valley community at 150 feet. That additional stress shows up as a higher rate of underground plumbing joint failures on older Blue Bell pool detection visits compared to lower-elevation communities in the same service area.
This does not mean every Blue Bell pool from the 1970s and 1980s has underground plumbing failures waiting to be found. It means that when a Blue Bell pool shows the early signals of a leak like a rising water bill, chemistry that requires more correction each week, the bucket test showing more loss than evaporation explains.