Traditional pool chemistry teaches arbitrary ranges (e.g., pH 7.2–7.8, Alkalinity 80–120). Orenda water science focuses on saturation equilibrium, bather waste digestion, and cyanuric acid control.
Water is never neutral; it is either dissolving calcium carbonate (corrosive / etching) or dropping calcium carbonate (scaling). The Langelier Saturation Index (LSI) tells you exact equilibrium.
Chlorine was designed to kill germs, but non-living organic waste (body oils, sweat, cosmetics, desert pollen) consumes up to 80% of chlorine demand, creating smelly chloramines.
Phosphates are the essential fertilizer for algae. High desert winds deposit massive amounts of dust into Antelope Valley pools, driving phosphates well over 1,000 ppb.
Cyanuric Acid (stabilizer) protects chlorine from UV rays, but over 50 ppm CYA creates severe chlorine over-stabilization (chlorine lock). At 100 ppm CYA, over 98% of your chlorine is bound and inactive.
In summer, your pool water is 88°F (TF = 0.7). In winter, night freezes drop water to 40°F (TF = 0.2). This represents a massive -0.50 LSI drop without changing a single chemical! Water becomes hungry for calcium and aggressively dissolves plaster, quartz, and heater copper coils.
Lancaster municipal tap water arrives at 200+ ppm Calcium Hardness and pH 8.2. In 105°F desert heat, an average pool loses 2 inches of water per week to evaporation. Auto-fill valves constantly add more calcium, driving calcium hardness over 600 ppm within 2 years.
Mojave desert wind events blow fine silt and agricultural fertilizers into pool water. Without proactive phosphate removal and enzyme digestion, chlorine quickly gets locked up and algae blooms overnight.
AV Pool Pro technicians test your water on-site using the LaMotte WaterLink® Spin Touch® lab-grade spectrophotometer. Every service visit includes an exact Orenda LSI equilibrium audit.