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4 Ways to Bring Flooded Fields Back

Lessons learned from 2011 in bringing flooded fields back to production.

Nebraska producers have been here before. 

In 2011, the flooded Missouri River wreaked havoc on the farm fields in the Missouri River basin. John Wilson, Extension educator in Burt County, Nebraska, says there are lessons learned from that time that are applicable today. “From our experience in 2011, farmers found that they needed to work on things in three stages to repair flood-damaged fields,” he says in an article posted at the University of Nebraska-Lincoln Crop Watch. 

1. Remove debris and sediment.

There are two general types of debris: plant material and other debris. The kind of "other" debris will make a difference on how it is handled. Plant material, primarily cornstalks and trees, can be burned on the tract of land where it was found (if it is zoned agricultural) and the ashes buried there.

If a layer of cornstalks or other crop residue isn’t too deep, it can be incorporated into the soil with normal tillage operations. One concern, and this will be a recurring theme, is to not perform tillage when the soil is too wet. This will cause compaction and create more of a problem than it solves. Also, burying high-carbon crop residues may temporarily tie up nitrogen in the soil as microbes break it down.

In 2011, Nebraska farmers encountered varied from a lot of smaller “junk” such as tires, posts, and boards to propane tanks and vehicles to wooden decks, cabins, and whole homes that had floated into fields. There are two options for this type of debris. It can be buried onsite if the land is zoned agricultural, or it can be taken to an approved landfill.

In the case of buildings, an asbestos inspection may be required by the Nebraska Health and Human Services (NHHS). Call 402/471-0386 to see if you need an inspection. For other information on handling miscellaneous debris, contact the Waste Management Section of the Nebraska Department of Environmental Quality (NDEQ) at 402/471-4210.

Sedimentation from floods can pose a great challenge for crop production on agricultural land. The difference in texture of the deposition and the native soil below can cause major production issues. Burt says that in 2011, deposits varied from 1 inch or 2 to over 30 feet deep. The depth of the deposition will determine how it is best handled:

  • 0-2 inches: incorporate with normal tillage operations.
  • 2-8 inches: incorporate with chisel or moldboard plow.
  • More than 8 inches: spread or remove to a depth of 8 inches or less and incorporate as listed above.
  • Tillage in the native soil should be the depth of the sand plus 1.5 times the depth of sand; for example, you would till 10 inches deep for 4 inches of sand [4 + (1.5 x 4) = 10].
  • Avoid tillage or other field operations until soil is dry enough to reduce the chance of compaction.

2. Repair Erosion

The degree of erosion can vary from a few inches to many feet and different levels will need to be managed differently.

  • Tillage – if soil can be smoothed and farmed following a normal tillage operation
  • Earth moving – if erosion is too deep to be corrected with tillage, but can be filled, then farmed. Fill eroded areas or top-dress with native soil from other parts of the field, depending on the depth of the erosion.
  • Abandonment – may be the only option if erosion is too deep to correct economically, even with earth moving.

If you’re using sediment depositions to fill eroded areas, use native soil from another area in the field for the final 3 feet to avoid droughty areas.

Avoid field operations until the soil is dry enough to reduce chances of compaction. After major erosion repairs, sample the soil in the repaired area. (Consider sampling from both the repaired area and undisturbed area to determine if fertility should be managed differently in each.) Use traffic lanes if making multiple trips in the same field to correct erosion.

3. Manage Other Factors

Growers may encounter soil crusting, which occurs when the surface soil texture changes and the loss of structure causes effects resembling compaction. This can restrict root penetration and reduce water infiltration. Tillage should remedy a shallow (less than 2 inches) crust. Don’t do tillage when the soil is too wet!

Also, sedimentation and removal of crop residues from the soil surface may lead to wind erosion. The easiest way to reduce this is by seeding a cover crop as soon as conditions permit. There are several options:

  • Aerial seeding success depends on timely rains and may not be as effective because of a lack of seed to soil contact. However, this does allow the earliest seeding in a field where ground operations might be impossible. The whole field can be done at once, regardless of conditions.
  • Broadcast seeding followed by light tillage provides better seed-to-soil contact, but is dependent on being able to get into a field. Often the whole field may not be seeded at the same time.
  • Drilling gives the best seed-to-soil contact and seed distribution, which leads to more rapid germination and establishment. Also, drills may provide some soil smoothing and cause less compaction than tillage to incorporate seeds.

Besides reducing wind erosion, cover crops significantly increased corn yields (+30 bu/A) but not soybean yields in 2012 on ground that was flooded in 2011. We don’t know if cover crops will have the same effect on yields in a flood of shorter duration. This study was conducted on a field that was under water for over three months in 2011.

Other Crop-Management Practices

There are many other management decisions such as tillage, fertility recommendations, cover crop termination, inoculation, seeding practices, and weed control that require special consideration following a flood. 

For more information on these topics and other flood-related issues, go to https://flood.unl.edu, including the Crops section.

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