Why Lafayette Hill's Hilly Terrain Creates Repair Patterns That Flat Lot Pools Do Not Experience
A pool on a flat suburban lot expands and contracts with temperature changes in a roughly symmetrical way. The soil surrounding the shell sits at the same depth on all sides and carries similar moisture content throughout the season. When thermal movement causes the pool structure to shift slightly, it shifts into soil that responds consistently on all sides. Expansion joints absorb that movement. Over time the joints eventually harden and fail, but when they do, the failure is distributed around the pool perimeter without a strong directional bias.
On a Lafayette Hill hillside property, the soil on the uphill side of the pool shell sits deeper and carries more moisture from the slope above than the soil on the flat downhill edge. When winter cold causes the surrounding soil to contract, the uphill soil contracts differently than the downhill soil. When summer moisture expands the soil, the uphill side expands differently. The pool shell experiences uneven lateral pressure across its faces as a result of this difference. After 40 or more Pennsylvania winters, the cumulative effect of that uneven pressure concentrates repair findings on the uphill face of the pool rather than distributing them evenly.
This is why noting which face of the pool a repair finding appears on matters in Lafayette Hill. A crack on the uphill face of the shell on a hilly property points toward uneven soil pressure and a failed expansion joint on that same face as the primary cause. Addressing the crack without addressing the expansion joint on the uphill face leaves the underlying cause in place. The repair fills the crack and the same stress that opened it begins working on the repair material. Within a season or two the same finding reappears.Â