Local Soil Conditions: Orlando's soils are characterized by Tavares fine sand, Apopka fine sand, and Candler fine sand — excessively to moderately well-drained Entisols and Spodosols formed on ancient sandy ridges and lake margins. Percolation rates in the Tavares and Candler series are rapid (6-20 inches per hour), which initially seems favorable but creates nitrogen leaching risk into the underlying Floridan aquifer. Lake-edge and low-lying areas contain Basinger and Malabar fine sands — poorly drained soils with spodic horizons and seasonal water tables at 0-18 inches. The Orlando metro's lake-dotted landscape means soil conditions change dramatically within short distances.
Water Table: Water table depth is highly variable across the Orlando metro due to the region's more than 300 lakes. Upland ridge areas (Winter Park Ridge, Lake Wales Ridge extensions) maintain water tables at 4-10 feet below grade year-round. Low-lying interdunal swales and lake margins have water tables at 0-24 inches seasonally. Orange County requires a minimum 24-inch separation from the seasonal high water table to drain field bottom; Seminole County enforces the same standard. The Floridan aquifer is unusually shallow in some Orange County locations, driving strict separation requirements for wellhead protection zones.
Climate Impact: Orlando has a humid subtropical climate with hot, humid summers and warm, dry winters. Average annual rainfall is 50 inches, heavily concentrated in the June-September wet season which delivers 30+ inches. The region's 300+ lakes moderate temperatures but create micro-drainage challenges for septic systems near shorelines. Summer afternoon thunderstorms are intense and frequent, with 90+ thunderstorm days per year — more than almost any other metro in the country. Year-round warm temperatures (average 72°F) support robust septic tank biology but also accelerate biomat formation in drain fields during wet periods.