Horticultural Crops - Understanding the Basics - Soil ManagementTable of ContentsHorticultural crop growers share many of the same management concerns of other producers. Although horticultural crops vary substantially, they all require skilled management to produce a high quality product. These crops rely on intensive management of soil, water, nutrient resources and pest populations. Soil ManagementSoil is vital to all crop production, whether sod, vegetables or fruit. Healthy and productive soil helps crops develop good root systems and reduces crop stress caused by drought or excess rainfall. Intensive production of horticultural crops creates some unique challenges in soil management. Soil ErosionSoil erosion is a concern in many horticultural crops. Highly productive land is valuable and the supply is limited. Water and wind erosion can remove nutrients, other crop inputs, soil and organic matter. The crops, themselves, may also be damaged or stressed by erosion, increasing the possibility of disease. The following table shows a number of practices available to reduce or stop erosion. Erosion control structures, such as berms and terraces, are covered in the Field Crop Production book.
Figure 1. Example of soil erosion. Soil erosion can be particularly destructive
to horticultural soils: removing crop inputs, soil and organic matter
and damaging or stressing the crop.
X = Effective Control Possible
Figure 2. Wind erosion. The impact of wind erosion is often underestimated. If soil is visibly moving, more than 11 tonnes/hectare of soil is being moved.
Figure 3. Crop residue. Most horticultural crops leave soil exposed. Even relatively small amounts of residue can reduce wind and water erosion. Tillage and residue management involves leaving some crop residues to protect the soil. Residue acts in two ways:
To protect soils, at least 20% residue cover should be left-but any amount will help. See the Field Crop Production book for a more detailed discussion of reduced tillage and equipment modifications.
Figure 4. Rye cover crop. A rye cover after processing tomatoes add organic matter, holds some excess nutrients and protects the soil over winter. Cover crops are planted to protect the soil surface and to maintain soil structure. They also help tie up excess nutrients, add organic matter to soil and control pests. There is a variety of cover crops available. Some are suited for specific uses. You must know what you want from a cover crop when making the selection. Ask yourself the following questions:
Cover Crop Suggestions - GrassesCover Crop: Winter Rye
Cover Crop: Winter Wheat
Cover Crop: Barley
Cover Crop: Oats
Cover Crop: Ryegrass
Cover Crop: Italian Ryegrass
Cover Crop: Fescues
Cover Crop: Corn
Cover Crop: Sorghum-Sudan
Cover Crop Suggestion - LegumesCover Crop: Red Clover
Cover Crop: Ladino Clover
Cover Crop: Sweet Clover
Cover Crop: Alfalfa
Cover Crop: Hairy Vetch
Cover Crop: Austrian Winter Peas
Cover Crop: Field Peas
Cover Crop: Soybeans
Cover Crop Suggestion - BrassicasCover Crop: Spring Canola
Cover Crop: Winter Canola
Cover Crop: Tame Mustard
Cover Crop: Oil Radish
Cover Crop Suggestions - OtherCover Crop: Buckwheat
Note: Seeding success dependent upon weather, particularly summer
seedings. Nematode Rating Codes^ = Poor or non-host Windbreaks and wind barriers are covered in detail in the book on Farm Forestry and Wildlife Habitat Management. Wind barriers include a variety of possibilities, from short-term grain interseedings in muck crops to grass strips and fence-like materials to protect vegetables. Barriers reduce the speed of wind and lower its ability to carry soil. The area protected by a tree windbreak is about 10 times its height. The amount of protection provided by other types of barriers varies depending on height and the flexibility of the material.
Figure 5. Illustration of a tree windbreak Figure 6. Illustration of a grass wind strip Wind barriers reduce the speed and soil carrying ability of the wind. Tree windbreaks protect an area about ten times their height. Grass wind barriers are more flexible and can be pushed down by high winds, reducing the protected distance to five to seven times the barrier height. Strip cropping involves planting strips or sections of a field with crops having different growth habits. For example, growers may alternate strips of early vegetables with later-seeded vegetables. Although management may increase, the soil surface is better protected. Soil StructureMaintaining good soil structure is also a challenge for growers of intensively managed crops. Soil structure refers to how well soil particles are organized and held together as soil crumbs or clods. Structure influences the general health of the crop in the following ways:
Figure 7. A good root system is essential to production, allowing the plant to exploit soil water and nutrients. Soil CompactionTillage and cultivation tend to break down soil clods and organic matter. Organic matter is the glue that holds soil particles together. Production of high-quality horticultural crops requires timely operations. Sometimes, this means tilling, spraying or harvesting on soils that are too wet. In addition, to be cost-effective, many of these operations have become highly mechanized. Running heavy equipment in wet conditions may cause soil compaction. Compaction means that the soil has become packed and pore spaces are reduced which decreases the soil's ability to hold both air and water.
Figure 8. Scheduled harvest of perishable crops sometimes forces working on wet soils. Try to avoid compaction using other measures and plan to rotate away from the problem crops. Reducing Compaction
Tillage and crop roots usually break up shallow or surface compaction. However, deep compaction or plow pans can be more difficult to deal with. Deep-rooted crops and frost action may help. Research shows that frost takes at least three winters to reduce compaction, assuming that no further compaction has taken place. Deep tillage or subsoiling is a prescription treatment for the worst areas.
Figure 9. Given the soil conditions, this deep tillage implement
is where it should be - parked. Subsoiling must be done properly, or problems
can be made worse. It is important to subsoil properly or compaction is just moved deeper:
Subsoiling is only a temporary solution and does not remove what caused compaction in the first place. Soil Organic MatterSoil organic matter is a very small part of the soil with a large role to play. Many soils used in horticultural production have soil organic matter levels between 2 and 4%. About 40 to 45% of the soil organic matter is very stable and resists decomposition. Another 40 to 45% is moderately stable. This portion is protected or held within soil clods and on clay particles and is very important to soil fertility, accounting for 40 to 50% of nutrients released each year. The remaining 10 to 15% is composed of living and dead organisms and decomposes easily.
Figure 10. Tillage equipment Reducing tillage where possible will help to retain soil productivity by reducing soil compaction and erosion losses of soil and organic matter.
Figure 11. Pie chart: organic matter 5%; mineral particles - sand, silt, clay: 45% ; water 25%; air 25% Figure 12. Organic matter: easily decomposable organic matter: 10-15%; very stable organic matter (humus - 1000 years old) : 40-45%; moderately decomposable organic matter (half life of 20-40 years): 40-45%
Figure 13. Easily decomposable organic matter: living organisms (bacteria, algae, fungi, earthworms, nematodes, etc.): 20-40%; readily decomposable soil organic matter (crop residue and roots, dead organisms): 60-85% Organic matter is only a small portion of the soil, but it is very important to soil fertility and good soil structure. Maintaining adequate soil organic matter levels is crucial to consistent production of horticultural crops.
For more information: Toll Free: 1-877-424-1300 Local: (519) 826-4047 E-mail: ag.info.omafra@ontario.ca
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