| Irrigation |
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Page 1 of 2 Irrigation is the controlled provision of water in order to successfully cultivate a crop under the following conditions:
Because climate and soil conditions are specific to each area, it is not possible to give an in-depth account of irrigation systems and scheduling, but only to describe the more important terms, guidelines and practical implications.
The rate at which water infiltrates the soil is an inherent property of the soil. It is highest in dry sandy soil and lowest in wet clay soil. Practical implications Excess water leads to reduced air supply (oxygen) in the soil, runoff, erosion and between-row weed contamination.
After water has moved downwards through the soil profile (through gravity and soil water gradients, i.e. redistribution), this point represents the highest limit of the soil’s capacity to store water. Practical implications:
This is often used as a measure that indicates the crop is suffering water stress; irrigation should should be done before this point. Practical implications:
Evapotranspiration : This determines the pattern and rate of evaporation from an open piece of ground, together with the rate of transpiration from the leaf surfaces of the plants. Practical Implications In established stands where the leaves shade the soil, the transpiration rate of the crop is more important than evaporation in the water use of the crop. Because plants need CO for photosynthesis (the amount depends on production potential) they have to transpire, with the result that they will necessarily lose water vapour through their stomata. |
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Lucerne Management 






