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 Macedon, Wayne 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 Macedon. We will walk your fields, identify problem areas, and propose a drainage solution that works for your operation.
Macedon lies in western Wayne County along the Erie Canal, inside the Finger Lakes drumlin field east of Rochester. Soils across the town's commercial corridors along Route 31 and the NYS Thruway interchange are predominantly Honeoye silt loam and Lima silt loam on the drumlin flanks, with Palmyra gravelly loam on the outwash benches and Canandaigua silty clay loam and Wayland silt loam in the low ground along the canal and Mud Creek.
The Erie Canal and its feeder channels control drainage across the northern half of the town, and any earthwork inside or adjacent to the canal prism triggers NYS Canal Corp review. Commercial excavation in Macedon typically involves cobbly, stony trenching on the drumlins, structural fill importation on the clay-loam flats, and stormwater design tied to the Ganargua Creek and Genesee River watershed. Shallow bedrock appears only on the highest drumlin summits. Frost depth is moderate by regional standards, reflecting the transition between lake-moderated and interior climate zones.