We are learning that our soil structure is a much more delicate system than we ever realized. Specifically, the soil in northeast Wisconsin presents a unique set of challenges for producers to overcome. Supported by funding from the Great Lakes Restoration Initiative (GLRI), the U.S. Geological Survey (USGS) has partnered with four Fox Demo Farms to measure sediment and nutrient loss in surface and subsurface runoff at edges-of-fields (EOF) (Image 1). Preliminary data show high losses of sediment in surface runoff (about 4,000 pounds per acre averaged annually among four sites) and low losses of sediment in the subsurface tile site (about 50 pounds per acre) relative to the state average noted in a 2011 USGS Scientific Investigations Report (SIR) summarizing EOF data collected in collaboration with the UW-Discovery Farms and Pioneer Farm projects. Per inch of runoff, the average annual loss of sediment at the surface sites was approximately 650 pounds per acre per inch, which is more than double the reported state average (Table 1). Additional results from the EOF monitoring will help guide Natural Resource Conservation Service (NRCS) recommendations for conservation practices.
Preliminary data collected from the EOF monitoring sites shows that annual phosphorus losses are quite high, averaging nearly 6 pounds per acre. This is nearly triple the state average noted in a 2011 USGS report summarizing EOF data collected in collaboration with the UW-Discovery Farms and Pioneer Farm projects. As the graph below illustrates, about 80% of phosphorus leaving the fields is in the particulate form, meaning that most of this phosphorus is attached to soil particles (Figure 1). This suggests that conservation practices aimed at helping to retain soil and reduce erosion could drastically reduce the amount of phosphorus leaving producers’ fields. Again, the results from the EOF monitoring will help guide NRCS recommendations for conservation practices.
Soil Health Principles:
Traditional farming practices can drastically disrupt the soil system, resulting in soil erosion, soil compaction, increased inputs such as commercial fertilizers, and the loss of valuable top-soil due to increased surface runoff. Addressing these four key principles can help improve soil health now and into the future for generations to come.
- Keep it covered: Keep soil covered with either residue or cover crops.
- Living roots: Having a living cover going into the winter, so we continue to “feed the biology” of the soil.
- Crop diversity: The more diversity we can introduce, the better opportunity to feed soil and create a healthier system.
- No disturbance: By not disturbing the soil profile, we allow the structure to develop, which increases infiltration rates and allow the soils to warm up.
Check out the NRCS – Wisconsin’s Rainfall Simulator video:
The video highlights five samples from different farming practices and demonstrates the runoff effects that occur during a rain event. The five farming practices are:
- Conventional Till: Dairy, Rotation
- Continuously tilled for last several years, very little structure and residue
- Reduced Till: Dairy, Rotation with Covers
- Transitioning to less tillage and getting the cover crop established as soon as possible
- No-Till: Dairy, Rotation with Covers (planted late)
- No-till for at least five years, cover crops established a week prior to the demonstration
- No-Till: Dairy, Rotation with Covers
- Transition into a no-till dairy system, 10-way mix of cover crops
- Rotationally Grazed Pasture
- Seeded down for three years
How will the samples handle the rain?
Which samples will have better infiltration rates?
Which samples will have reduced runoff?
- Get covers established as soon as possible.
- The combination of no-till and early cover crops is very important.
- Structure from cover crops reduces the risk of rutting.
- Erosion does not only occur when you have a gully or rill that carries the water and sediment. Sample 1 demonstrates that sheet runoff can occur on cultivated fields with no cover crops.