Agronomy Library > Getting Started

Direct Seeding Implications for Nutrient Management
Author: Ron Heller, Reduced Tillage LINKAGES
Date Created: March 26, 2008
Last Reviewed: March 26, 2008

Direct seeding practices can result in crop yields as good or better than traditional tillage-based cropping systems. Reducing tillage has proven to be economical as well as environmentally friendly. Direct savings on farm fuel, labor, and machinery-life plus the elimination of soil erosion are real and immediate benefits. Generally, moisture conservation and improvements in soil quality can be expected over time with important implications for nutrient cycling and higher yield potential as soil disturbance is reduced.
 
Biologically, the fertility implications of less tillage are:
  • Slower decomposition of surface crop residues (stubble, straw and chaff)
  • Increased soil organic matter levels over time
  • Moderation in soil temperature extremes
  • Superior crop water-use and nutrient uptake
There are other specific interactions that begin to occur when tillage stops. A transition period will arise for nitrogen cycling and other nutrient equilibriums. Crop residues return carbon, nitrogen and other essential nutrients in various degrees back to the soil. Soil disturbance interferes with the microbial function of soil in association with plant roots. (ie: mycorrhizae fungi). Climate, soil texture, crop rotation, and fertilizer management are important factors that influence how quickly and to what extent these direct seeding transformations take place.
 
Direct seeding usually improves soil moisture reserves by trapping snow and capturing run-off. High levels of crop residue protect the topsoil from heat and wind while increasing field water holding capacity. An increased yield outcome subsequently impacts removal and availability of soil nutrients. The degree of change in soil fertility tends to be greater for LDS than high disturbance systems because soil displacement and residue incorporation are minimized. Primarily, a direct seeding implement needs only to:
  • Create enough soil exposure in the seed furrow to allow timely seeding into cooler soils.
  • Provide adequate placement of fertilizer (balanced nutrient package).
 
Nutrient Management Adjustments for Direct Seeding
 
Direct seeding carries yield advantages overtime because early seeding into a firm moist seedbed stabilizes crop establishment, lowers weed competition, and provides nutrient efficiency. Earlier seeding in dryland prairie normally implies a yield advantage because of a short growing season and limited soil moisture. By eliminating extra field operations otherwise needed for fertilizer application or seedbed preparation, direct seeding allows timely seeding. Nutrient management adjustments for unexpected seedbed conditions (too cold, too wet, or too dry, etc.) can be made while direct seeding. A flexible crop rotation along with residue management and a pre-seed weed control strategy are integral steps.
Experienced direct seeders have discovered the benefits of timely, precision-fertilizer placement. The main factors influencing nutrient placement in a direct seeding system are fertilizer type, rates, and timing.
 
Alberta’s sustainable cropping program, Reduced Tillage LINKAGES (RTL) promotes the adoption of low disturbance direct seeding (LDS) = less than 40% stubble knockdown after seeding[1]. Simultaneous, or one-pass seed and fertilizer placement within an LDS system has further implications for nutrient management. Important terms distinguish fertilizer placement capabilities of a direct seeding implement:
  • Single-shoot (SS) systems place seed and fertilizer together in the seedrow.
  • Double-shoot (DS) systems separate seed and fertilizer placement.
 An SS system implies concern for crop injury due to seed and seedling damage from seed-placed fertilizer. In DS systems, there are various methods that address this concern, in particular for fertilizer-N (nitrogen).[2]
 
Direct seeding requires fertilizer use and placement to be just right to become profitable. In order to maintain optimum yields, it is important to have a good understanding of fertility for P (phosphorus) and K (potassium), as well as meet the high demand for N (nitrogen) sometime into the growing season. Sulfur (S) deficiency and micronutrient management are issues that should also be addressed.
 
Starter Fertilizer
 
A common misconception is that seed-placed nutrients are required. In reality, a crop seed doesn’t need anything more to resume its biological heritage than air and moisture (for germination) plus sunlight to warm the soil and foster emergence. Shortly after roots and leaves begin to form however, there should then be a “balanced” nutrient package readily available so the plant can commence and sustain photosynthesis.
 
Cool soil temperatures can impede root development, and the fact that P & K are not very mobile in the soil (unlike fertilizer-N) suggest these nutrients should be placed nearby the seed, according to soil-test recommendations. However, combining so-called starter fertilizer with seed can create unnecessary problems. Solutions for common fertilizer placement troubles in direct seeding include:
  • Use a DS system to safely separate seed and fertilizer for efficient direct seeding of a wide range of crops in variable soil conditions.
  • Follow seedbed utilization (SBU) guidelines for SS systems to avoid potential crop injury due to unsafe rates of fertilizer-N. Fertilizer-type often determines which direct seeding implement works best.
  • Problems can still arise in the form of seed-bash[3] and blow-out[4] (air-seeding) and/or seedrow toxicity[5] if small seeds are combined with heavy rates of granular starter fertilizer.
  • Farmers can conduct on-farm evaluations for nutrient placement and rates in direct seeding systems. Switching off the fertilizer clutch and observing the crop emergence can accomplish a simple check-strip trial for starter fertilizer.
  • Where possible, it is better to separate seed and fertilizer. Precision-placement of crop nutrients will favor the growing crop over weeds.
 
Nitrogen Management
 
Second only to H2O, nitrogen (N) tends to be the most limiting crop nutrient. Direct seeding has several positive implications for N-cycling. Precision-placement of crop nutrients at the time of seeding can reduce:
  • Volatilization – N loss from breakdown of surface-applied N (urea) to gas (N2)
  • Denitrification – N conversion (nitrate and nitrite) in cold wet soil to N2
  • Immobilization – N use by soil organisms during crop residue decomposition
 However, N-efficiency can also be reduced due to:
  • Lack of seedbed moisture – Crops do not grow well in dry soil!
  • Saturated soil – Traditional fertilizer-N forms are all subject to leaching[6].
  • Soil erosion – Any topsoil loss represents a potential loss of crop production
  • Lower mineralization[7] - When tillage stops, an undetermined transition period for available N may arise in direct seeded crops until a new equilibrium is reached.
Normally, the higher the soil moisture, the more likely crop response to N will be. LDS systems optimize soil moisture. In simple SS direct seeding, risk of crop injury from seed-placed N decreases as soil moisture increases. Likewise, crops grown in course sandy soil are more at risk than fine textured clay. Although more complex, high rates of N-fertilizer are best managed with a DS system that separates the fertilizer (safety) without compromising the seedbed (moisture).
 
Sulfur Fertilizer
 
Rotational cropping in a direct seeding system has a unique spin-off for sulfur (S) management, in terms of mobility and crop use.
  • Elemental S fertilizers must be converted to sulphate form overtime by soil microbes.
  • Sulphate forms are highly plant-available, but also bulky in a dry blend.
  • While S deficiency tends to be highly variable in a given field, application in the previous year extends the soil contact needed to enhance crop uptake.
  • Broadcast application is an option because S is not subject to volatilization.
 
Soil Analysis
 
The best fertility management practice is an ongoing soil-testing program that can account for nutrient supply and demand (ie: balance available soil nutrients with crop-use). GPS technology now makes field zoning and variable rate applications possible for advanced nutrient management. New biotechnology for seed treatments and fertilizer coatings is revolutionizing seed and fertilizer use, but still requires more research and development for direct seeding.
 
Weeds and Crop Rotation
 
The operational diversity of a farm mainly revolves around seeding and harvest.
  • Different crop species have different rooting systems. So do weeds. Depending on where and when they are growing, each will have an important advantage (or disadvantage) relative to soil moisture and nutrient placement.
  • Crop residues with higher N content, such as legumes, tend to decompose quickly without tillage, shortening the transition period for available N.
  • Crop rotation also implies herbicide rotation (Group-use, target weed species), a variation in seeding and harvest dates (spring / fall workloads), and a disruption to crop pest cycles (insects and disease).
 
Summary
 
In practice, direct seeding validates all of the above. Early seeding and precision-placed fertilizer, combined with a pre-seed burnoff and timely in-crop spraying for weeds, makes continuous cropping more competitive and profitable compared with crops grown under less intensive tillage-based systems (bare-fallow). Soil remains biologically healthy because of crop rotation and less erosion.
 
The features of a direct seeding implement’s opener width[8] and row spacing[9] have become highly interactive with all aspects of a successful reduced tillage cropping system. They will determine not only the flexibility for nutrient rates and placement, but significantly influence the timing and outcome of fundamental crop rotation, weed control, and residue management strategies.
 
Without incorporation of crop residue (tillage), or in the absence of a diverse crop rotation, stratified nutrient levels or even pH changes may occur overtime. However, this has not been well documented or extensively researched in Alberta and remains a minor concern after more than 20 years of direct seeding.
 


[1]Percent disturbance can be calculated by: Seed Opener Width X 100 divided by Row Spacing. This same formula has also been used in seedbed utilization (SBU) guidelines for safe seed and fertilizer placement.
[2]For more information about seed and fertilizer placement for direct seeding systems, See RTL’s Direct Seeding Equipment Directory-March 2008
[3]Physical damage to fragile seed and coatings can occur from contact with fertilizer granules and high velocity air-seeding.
[4]Shallow seedrow placement of low-volume tiny seeds (like canola) can be compromised when air-seeder velocity is set for heavier high-volume fertilizer rates.
[5]High volumes of seedrow fertilizer can result in salt-toxicity causing poor germination and root pruning similar to drought effects. Moisture, soil texture, and fertilizer-type are important factors.
[6]Topsoil flushing (runoff) or downward movement of N-sources away from the crop’s rooting zone.
[7]Conversion of soil organic matter into plant-available N.
[8]Openers – the term commonly used for seed and/or fertilizer placement in direct seeding.
[9]Wider spacing between seed-openers (shank or disc) ensures better residue clearance for direct seeding.