The Fertilizer Assocition of Ireland
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HEALTH AND ENVIRONMENT
PLANT NUTRIENTS
FREQUENTLY ASKED QUESTIONS
Plant Nutrients - Trace Elements
Nitrogen Phosphorus Potassium Secondary Elements Trace Elements Soil Activity
As the name implies, only very small amounts of trace elements are needed for healthy plant growth. Sufficient is normally available in the soil or in recycled soil organic matter but this is not always so. For specific crops and particularly where the soil is abnormally acid or alkaline, trace element deficiencies may occur. These can be corrected by adding whichever nutrient the crop is short of. Leaf colour and size are useful in detecting deficiencies.
Effects of soil pH on the availability of nutrients.
Most crops grow best between pH 6 and 7 (7 is neutral, below 7 is acid and above 7 is alkaline). Adding lime will bring acid soils up to the ideal pH. However, there is no practical field-scale treatment for soils which are too alkaline but the pH will slowly reduce with time.
Trace Elements
Where only one trace element is required, the use of a trace element ‘cocktail’ i.e. a mixture of several trace elements, is to be discouraged and is a waste of money. In addition, the particular trace element that is required may not be supplied in adequate amounts by the ‘cocktail’.
Grass : Under Irish conditions, responses in pasture growth to trace element application are rare. The importance of trace element levels in pastures therefore, relates principally to animals, and not to plant requirement. The trace elements which are associated directly with clinical deficiency in animals are cobalt, copper, iodine, manganese, selenium and zinc. Molybdenum is important because at high levels in the herbage it reduces the availability of copper for absorption. Soil analysis is a better indicator of availability than herbage analysis for cobalt and iodine whereas herbage analysis is more reliable for copper, manganese, seleniumand zinc.
Cobalt (Co)
The soils giving rise to low cobalt pastures are typically those formed from granite and sandstones but even soils rich in cobalt can support low cobalt pastures if the total manganese content of the soil is also high. Hence, when determining the level of cobalt in a soil it is also necessary to analyse for total manganese in order to know whether cobalt can be applied to the soil or if it must be fed directly to the animals. If the manganese is high (>600 mg 1-1) the cobalt should be fed directly.
Copper (Cu)
Soils derived from sandstones, granites and peat soils are likely to have low Cu levels. The amount of Cu normally absorbed from food by the ruminant is less than 10%. Its absorption is also subject to interference by molybdenum, sulphur and to a lesser extent iron and zinc. Another factor which can be involved is dietary soil. It is known that grazing animals can ingest large amounts of soil which will reduce Cu availability. Obviously the higher the stocking rate the greater the soil intake.
Soil Cu tests, although useful, are not capable of being used as definitive diagnostic tests owing to the complexity of the problem of Cu availability and utilisation by the ruminant. It is better to use herbage Cu levels together with Mo and S values.
In heavy textured soils, Cu is not considered deficient unless the EDTA soil extractable copper level falls below 1.0mg1-1, whereas in light textured soils it may be low up to 2.5mg1-1. On peat soils a level of 5mg 1-1 maybe necessary.

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