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 Ovid, Seneca 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 Ovid. We will walk your fields, identify problem areas, and propose a drainage solution that works for your operation.
Ovid sits on the central plateau between Seneca and Cayuga lakes in Seneca County, on the narrow ridge of terrain that divides the two Finger Lakes watersheds. Soils across the village and surrounding agricultural-to-commercial parcels are predominantly Ovid silt loam — the series named for the town — along with Honeoye silt loam on the better-drained till, Lansing silt loam on the middle slopes, and Lima silt loam on the lower ground.
Drainage falls to both sides of the ridge through short, steep tributaries feeding Seneca Lake and Cayuga Lake respectively. Commercial site work in Ovid regularly involves managing fragipan-restricted subsurface drainage across essentially all of the silt loam uplands, slope stability on the steeper western and eastern flanks of the ridge, and stormwater design that has to satisfy Finger Lakes watershed protection standards for either receiving lake. Shallow shale bedrock can appear on the highest ridge sections. Frost depth is moderate given the lake-moderated microclimate. Projects along Route 96 that climb toward Willard and toward Lodi routinely require rock excavation and slope stability engineering on the steeper ridge flanks.