Local Soil Conditions: Jacksonville's soils vary significantly by county. Duval County is dominated by Leon fine sand and Pomello fine sand — poorly drained Spodosols with spodic hardpan layers 20-40 inches below grade and percolation rates of 1-4 inches per hour in the surface horizon. St. Johns County (Nocatee, Ponte Vedra) features Pellicer and St. Johns series soils with very fine sands and mucky surface layers near marsh edges. Clay County transitions to Atlantic Coastal Plain sediments with mixed sand and sandy clay loam soils of moderate drainage. All three counties require careful site-specific evaluation to determine spodic horizon depth before system design.
Water Table: Seasonal water table depth ranges from 6-18 inches below grade during the wet season (June-September) in low-lying Duval County, and 18-36 inches in the higher-elevation upland zones of Clay and St. Johns counties. The St. Johns River watershed creates persistent elevated water tables across the region. FDOH requires 24 inches separation between seasonal high water table and the bottom of the drain field.
Climate Impact: Jacksonville has a humid subtropical climate, the northernmost major subtropical city in Florida. Annual rainfall averages 52 inches, with a pronounced wet season from June through September. Unlike South Florida, Jacksonville occasionally experiences light freezes (average 15 nights per year below 32°F), which can affect above-ground system components but rarely impacts buried septic infrastructure. The St. Johns River basin and coastal marshes create high ambient humidity and periodic flooding conditions that challenge drain field performance during heavy rain events.