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Cropping
A natural supply of potassium
in both the exchangeable and fixed soil pools has historically been available
in much of Australia and New Zealand's most productive cropping areas.
On the other hand, some soils
do not have a natural supply of slow-release fixed potassium, such as
the sandy soils of Western Australia. Once the exchangeable potassium
pool is depleted, there is no natural replenishment from soil supplies.
But as soil reserves are depleted
over time, even the more fertile soils will begin to lack sufficient potassium
and will fail to meet the large potassium demand of high-yielding crops.
Some important points to remember
about potassium in cropping include:
Potassium is removed
from fields through grain and hay. Since vegetative plant material is
often much richer in potassium than grain, more potassium is lost when
hay is removed.
Potassium is needed
early in the life cycle of most annual crops. This results in a rapid
uptake period in which crops take up potassium at a very high daily
rate. Different crop species have differing maximum uptake rates, although
maize and cotton are particularly high.
As improvements in
plant breeding and farming systems develop - as well as the use of other
limiting nutrients - crop requirements for potassium will increase.
Sometimes chronic
potassium deficiency can occur. This usually happens in severely deficient
soils where yields are extremely low. In these cases, small potash applications
do not produce any yield responses, but large applications do. This
is probably due to soil fixation of added potassium before any is available
for plant growth.
Move
on for more information about:
Nutrient
Removal in Grain and Hay >>
Potassium
Uptake Rates >>
How Requirements
Increase with Yield Potential >>
Chronic Deficiency
>>
Potassium
Deficiency Symptoms >>
Research
Projects >>
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