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Pest plants click here Meet the members of our Committee
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SOILSSoil is a dynamic medium made up minerals, organic matter, water, air, and living organisms such as bacteria and earthworms. Soil was formed and is changed by time, parent material, climate, topography and organisms present. The way we manage the soil will have an influence on its character.Soil is not uniform but divided into layers, or horizons. The topsoil is classified as horizon A; it contains all the organic matter and plant roots, and is the most fertile. The B horizon, or sub soil, is beneath; it is less fertile and often contains more clay, iron and aluminium that has been washed down through the profile. Below the sub soil is the parent material from which the soil is formed. Soils in valleys and flat areas tend to be deeper than those on slopes, due to erosion. Western Australian soils are some of the oldest and most weathered in the world, and as a consequence are some of the least fertile. In order to produce cereal crops such as wheat and barley, fertilisers need to be added. Conversely, our native vegetation has produced a huge diversity of plants that are perfectly adapted to these infertile soils.
SOIL TESTING Most Australian soils are degraded. Developing a strategy to improve the fertility of your soils has the potential to greatly increase soil productivity, thus increasing sustainable returns. Here are some basic steps to develop your strategy: When improving soils for livestock pasture, identify the number and type of animals (eg sheep, cattle) that are needed to utilise the pasture.
Independent soil analysis (not connected to any fertiliser supplier) can be obtained from SWEP Analytical Laboratories, Post Office Box 583, Noble Park VIC 3174. Phone (03) 9701 6007
"Live as if you may die tomorrow, but farm as if you will in 1,000 years". This is the objective for those who strive for true sustainability in farm production (taken from SWEP website fact sheet). Back to the Home Page
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