Local Soil Conditions: Merrimack County soils reflect a complex glacial legacy of till uplands, stratified outwash terraces, and glaciolacustrine deposits along the Merrimack River valley. Dominant upland series include Marlow-Berkshire-Peru associations — coarse-loamy Haplorthods and Fragiorthods formed in glacial till with stony, moderately well-drained profiles. The Merrimack River terrace soils include Merrimack sandy loam and Windsor loamy sand — excessively drained, rapid-percolation Entisols with minimal treatment capacity. Glaciolacustrine silt loam soils (Raynham, Walpole series) occupy former lake bottom positions in the Penacook lowlands with very slow percolation and seasonal saturation.
Water Table: Upland till positions in Merrimack County have seasonal perched water tables at 18–36 inches in spring (March–May). The Merrimack River flood terrace has a shallow year-round water table at 2–4 feet. Glaciolacustrine positions near the Penacook lowland can have water tables within 12 inches of the surface during spring high water. The Lakes Region to the north (Lake Winnisquam, Northwood Lake drainage) has shallow water tables in low-lying areas adjacent to water bodies under NH Shoreland Water Quality Protection Act jurisdiction.
Climate Impact: Concord has a humid continental climate with cold, snowy winters — average January highs of 31°F and 64 inches of annual snowfall. The city sits in the Merrimack River valley, which provides slight moderation compared to the surrounding uplands, but frost penetration still reaches 44–48 inches in most winters. Spring snowmelt is rapid and intense, producing the highest-stress period for drain fields from late March through May. Concord averages 37 inches of annual precipitation fairly evenly distributed, with no pronounced dry season that would give drain fields extended recovery periods.