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 Parish, Oswego 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 Parish. We will walk your fields, identify problem areas, and propose a drainage solution that works for your operation.
Parish lies in east-central Oswego County on the lake plain transitioning into the Tug Hill foothills. Soils across the village and the Route 69 / I-81 interchange area are dominated by Scriba fine sandy loam and Ira fine sandy loam on the uplands, with Worth and Empeyville channery silt loams on the rising ground toward Tug Hill and Greenwood mucky peat in the extensive wetland swales.
Drainage flows generally westward through tributaries to the Salmon River and south through tributaries to Oneida Lake, with the continental divide between Great Lakes and Atlantic drainage running close to the town's eastern boundary. Commercial site work in Parish regularly involves managing seasonal high water tables, dealing with hardpan restrictions in the fine sandy loams, and stormwater design that accounts for extremely high annual precipitation on the Tug Hill side. Shallow sandstone bedrock can appear on the rising ground to the east. Frost depth and snowmelt volumes both push pavement, utility, and culvert detail on any commercial project here.