Subsurface tile drainage, open ditch work, and field drainage systems for farm fields and agricultural land in Central New York. Improve yields and protect topsoil.
Backwell installs subsurface tile drainage systems, open drainage ditches, and field drainage infrastructure for agricultural operations throughout Syracuse, Onondaga County, and the surrounding area. Proper drainage is critical to farming productivity in Central New York — wet fields delay planting, compact under equipment, and reduce yields. We solve drainage problems permanently with the right combination of tile work, outlet structures, and surface grading.
Our agricultural drainage work includes subsurface perforated tile installation at designed depths and spacing, open ditch excavation and maintenance, outlet structure installation, and integration with existing farm drainage systems. We work with farmers, landowners, and agricultural engineers to design systems that address your specific drainage challenges and meet NRCS requirements where applicable.
Contact us for a free consultation on agricultural drainage in Syracuse. We will walk your fields, identify problem areas, and propose a drainage solution that works for your operation.
Syracuse sits at the south end of Onondaga Lake in the heart of Onondaga County, on a landscape where the flat lake plain meets the rising Onondaga Escarpment. Native soils across the city's commercial corridors are a mix of Honeoye silt loam and Palmyra gravelly loam on the higher ground — University Hill, Westcott, Strathmore — with Lamson and Minoa fine sandy loams on the flats near the lake and muck pockets in the former wetland legacy areas around Ley Creek.
Drainage is dominated by Onondaga Creek, Harbor Brook, and Ley Creek, all feeding Onondaga Lake, and commercial earthwork frequently falls under the Onondaga Lake AOC cleanup framework in addition to the city's MS4 stormwater program. Site work in Syracuse consistently involves variable historic fill in the urban core, shallow Onondaga limestone along the escarpment and on University Hill, dewatering on lake-adjacent parcels, and structural fill importation where native lowland fines lose bearing under load. Frost-susceptible silt loams push utility burial across the city.