Basics of Compaction
Soils (often medium- and fine-textured soils) are vulnerable to compaction when they are at or near field capacity. Field capacity is the point at which the pore space surrounding soil particles is completely occupied with water. Water in the soil acts as a lubricant between soil aggregates. When heavy machinery puts pressure on field capacity soils, aggregates become tightly packed together.
The resulting compacted soil has fewer large pores, reduced pore volume, and increased bulk density. Plant roots growing in this environment experience aeration-related problems. Water is held instead of infiltrated through the soil profile. Soil compaction degrades land at a global level and is attributed to machinery growing heavier each decade since the 1950s.1,2
Emergence and Stand Counts. With conventional tillage, up to 100 percent of the field area can be trafficked during a single cropping cycle.3 Increased machinery traffic causes delays and variability in corn seedling emergence. Compaction from greater pressures per square inch, such as from road tires, has been shown to decrease corn plant population more than soils without compaction. Soil surface unevenness from tire-made ruts contributes to variability in seeding depth control. Uneven emergence can also be an issue with residue remaining from previous corn crops (Figure 1).
Figure 1. Corn residue in continuous corn can cause uneven emergence. Reduced tillage passes preserves soil structure and helps mend compaction but may require planters to have row cleaner attachments to prepare seedbeds.
Height. Table 1 shows effects of soil compaction on corn height. Corn is a tall crop and may be more sensitive to height differences caused by compaction. At six weeks post-planting, corn had a 21 percent height advantage when grown on non-compacted soils compared to soils with annual road tire compaction. Height differences were still noticeable at harvest, and yield trends lower with plants shortened by compaction.
Table 1. Soil compaction effects on corn height six weeks after planting and at harvest.*
Ear Development and Yield Potential
Effects of compaction on ear development and yield potential are not typically consistent across fields. Corn plants are sometimes able to produce larger ears as compaction causes lower populations.
However, corn can also respond by producing more ears of smaller size when grown on soils compacted by wheel traffic.4 Multiple factors affect the depth of compaction, and healthy plant development is greatly influenced by moisture stress.
Yield potential is related to ear size. A 19 to 50 percent corn yield reduction has been reported in compacted versus non-compacted soil.1,4,5 Severe subsoil compaction can occur in a single pass with a load of 18 metric tons per axle. Such compaction can affect corn yields for five to 12 years.4
Freeze-Thaw versus Summer Cracking. Deep compaction naturally begins to be corrected by drying during the summer months. Soils crack as they dry, and this shrink-swell process is one way clay-type soils are alleviated of compaction. Cracks can be several feet below the soil surface. Winter freezing remedies compaction in the top soil. Several dozen freeze-thaw cycles on fields with high soil moisture (greater than 85 percent of pore space filled with water) are needed to break up compaction.6 Realistically, Canadian soils may experience two to three freeze-thaw cycles per year.
Cover Crops. Cover crops can be a better alternative to machinery implements for breaking up compaction. Cover crop root growth repairs soils by stabilizing aggregates, creating pore spaces for infiltration, and breaking through plow pans. Cover crops planted on acres with compaction issues help drain wet soils and create root channels for commodity crops to grow through. These beneficial soil services are unique to cover crop growth. Unfortunately, deep-ripping implements intended to break compaction only result in positive crop responses about 25 percent of the time.6
Follow Tracks. Up to 80 percent of soil compaction occurs during the first pass across the field.7,8 Unchecked, the machinery footprint can cover the entire field. With overlaps included, a seedbed with wheel-tracks on 145 percent of the area can be created by conventional tillage passes.3 The change to controlled traffic pathways may take several years to achieve. Field operations become more efficient and less machine power is required with controlled field traffic. Consider the following:
Figure 2. Tire inflation for road travel is typically 40 psi. Field work should be done with tires inflated closer to 8 to 15 psi levels.8
- Grain carts are the heaviest machinery (carrying more than 20 metric tons) and should be the first equipment to be considered in pathway control (Figure 2).4,7
- Avoid diagonally crossing fields.
- Properly inflate tires to reduce surface compaction. Tire pressure for field work is about 8 to 15 psi while adequate 40 psi is the inflation used for road conditions.8
- Eliminate tillage passes especially if the intention is to dry out fields.
Axle Loads. High axle loads combined with over-inflated tires can create ruts with double the soil compaction compared to ruts made by the same equipment with proper adjustment.6 Deep compaction runs vertically (0.6 to 0.9 m) and horizontally from ruts. Compaction zones can be localized to the top 15 to 25 cm of soil when axle loads are under 9 metric tons.4
Soil compaction cannot be entirely avoided but should be prevented, minimized, and controlled as much as possible. Even minor topsoil compaction can cause up to 15 percent yield loss for a few years.9 This loss becomes permanent if management remains unchanged. Reduction of compaction in the topsoil and subsoil creates soil with increased water infiltration and storage. The improved water/soil environment allows earlier planting dates, decreases stress on plant roots, and reduces disease potential. Tillage proposes to dry soils for these same reasons but actually causes soils to weaken and have limited drainage (Figure 3). Soils are a critical resource to grow healthy, profitable crops and should be preserved for future use.
Figure 3. Poor water infiltration is shown in deep ruts. Additional root systems from cover crops, and cycles of wetting and drying over years should help alleviate this deep compaction.
1 Eswaran, H., Lal, R., and Reich, P.F. 2001. Land degradation: an overview. United State Department of Agriculture. Natural Resources Conservation Service. https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/use/?cid=nrcs142p2_054028
2Duiker, S.W. 2005. Effects of soil compaction. PennState Extension. https://extension.psu.edu/effects-of-soil-compaction
3Duttmann, R., Malte, S., Nolde, M., and Horn, R. 2014. Predicting soil compaction risks related to field traffic during silage maize harvest. Soil Science Society of America Journal. Vol 78. Pgs. 408-421.
4DeJong-Hughes, J. 2018. Soil compaction. University of Minnesota. https://extension.umn.edu/soil-management-and-health/soil-compaction#sources-1200560
5Khan Sial, J. 1987. Effects of controlled traffic in corn plots. Iowa State University. Digital Repository Retrospective Theses and Dissertations.
6Daigh, A.L.M. and Bly, A. 2020. Compaction reaction: soil compaction and ruts following a wet harvest. Crops & Soils. Pgs. 24-28.
7Gates, A. and Weir, T. 2019. 7 tips to avoid soil compaction during harvest. FarmersEdge. https://www.farmersedge.ca/7-tips-to-avoid-soil-compaction-during-harvest/
8Understanding soil compaction. Innovative Farmers Association of Ontario. https://ifao.com/.
92017. Interpreting results from the recorded sensor output. IFAO Compaction action field day. Shawridge Farms, Arthur, Ontario. https://ifao.com/.
Performance may vary from location to location and from year to year, as local growing, soil and weather conditions may vary. Growers should evaluate data from multiple locations and years whenever possible and should consider the impacts of these conditions on the grower’s fields.
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