Modern farming operations are largely designed for one thing - maximize profit. Farm
management addresses all factors in the farm business such as capital,
labour, crops, livestock and land. Farm management juggles these factors in an attempt to
maximize profit. Land or soil management attempts to adjust soil factors in a way that maximizes
crop production at the lowest cost. A wise management scheme will look to the future so that
the land continues to produce crops economically for many years, while leaving the soil
in a productive state (Sustainable agriculture) generations. Good soil management
attempts to preserve the best physical,
chemical
and biological characteristics.
Specifically, soil management encompasses all human activities concerning the soil.
The objectives of soil management are to control soil degradation and to
improve soil productivity. Good soil management emphasizes the following:
- preservation of soil organic matter crop rotation and by adding crop residues
- maintenance of good soil structure by crop residue addition and careful tillage practice
- protection of the surface of the soil against erosion through proper
cropping and tillage practices and preservation of soil moisture
- appropriate use of marginal land which is probably not suited to cropping
- conservation of natural wetlands to preserve natural drainage patterns and wildlife.
- careful fertilization and irrigation through soil testing and plant analysis.
appropriate weed and pest control minimizing the use of chemicals.
- economic management for sustainable agriculture - growing for tomorrow not only today.
In short, good soil management
attempts to preserve the best physical,
chemical
and biological
conditions.
In Saskatchewan, there are three major soil problems that affect large areas of the province:
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Physical Conditions
A soil with good physical condition is important to germinating and growing plants and to minimize soil erosion.
When soil is compacted, plant roots have difficulty penetrating the soil,
and air and water do not move as readily. The water and air
are essential for plant growth, so compaction may lead to plant death. Use of
heavy equipment and loss of organic matter are two factors that contribute
to this problem.
Some soils that have formed on parent material rich in sodium salts have naturally poor structure, particularly
in the Bnt horizon (see image).
Man's activities such as the placement of oil and gas pipelines, open gravel pits and
open pit mining, cause soil disruption. Often the fertile A horizons are buried or
scraped away leaving unfertile parent material behind. Natural structure is destroyed and
drainage problems can result making reclamation difficult and expensive.
Good "tilth" is achieved by adding crop residues back to the soil and by
appropriate tillage (or no-till) practices coupled with a good program of
fertilization and pest control. Crop rotations that involve deep rooted plants
such as alfalfa will help improve the structure of subsoils.
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Chemical Conditions
The most important soil chemical conditions
that must be monitored are: soil nutrient levels, pH (acidity or alkalinity), and
salinity.
Pollution is a common problem in soils often resulting from over use of
fertilizers and pesticides. Contamination can also occur from industrial sources such as mining operations,
oil drilling, pipeline bursts and poor toxic waste management.
The image shows saline areas on fields that have been irrigated. Often the salt washed out of the profile
can move considerable distances before surfacing.
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Biological Conditions
The biological activity of soils is directly related
to the quantity and quality of soil organic matter and physical conditions such as
temperature and moisture. The sustainability of soil organic matter
levels is crucial to maintaining a healthy soil organism population.
Soil organisms need organic matter for food and the soil needs humus for
tilth, nutrient supply and water holding capacity. The most important management practice
that affects biological activity is the return of crop residues to the soil.
Modern techniques of leaving standing stubble after combining and direct seeding
directly into the stubble the following spring has many advantages:
- Surface residues, particularly standing stubble, decrease wind and water erosion.
Large raindrops do not get a chance to impact on the bare soil and wash it away in suspension.
- Surface residues help trap snow. In the prairies more than half our annual
precipitation occurs in the in the winter and trapping of snow becomes
important to moisture conservation.
- Surface temperatures and evaporation are also lowered with a covering of crop residues.
- Decomposing residues are the raw material for humus. While they are decomposing the residues
release bound nutrients, which are then available for soil organisms and plants.
- Negative effects of residues must also be considered in good management. Of major
concern is disease which can be passed on to subsequent crops. Weed problems and nutrient
problems will result with poor quality residue. Nitrogen deficiency of the new crop is not
uncommon if crop residues with a high C/N ratio are incorporated into soil. Nitrogen is
removed from the soil (and away from the growing crop) by decomposing organisms as they break down the residues.
The effect is only temporary and the nitrogen is released back to the soil as organisms die.
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