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You are now in:>>What_is_Soil

                                            WHAT IS SOIL ?

Soil is made up of a mixture of mineral particles, decaying organic matter and living organisms.  It is very much a living thing –

Soil is populated by an amazing variety of living creatures, ranging from tiny microbes such as bacteria and fungi (microbeasts), to smaller insects such as centipedes and other animals such as worms (minibeasts) and larger animals such as moles and rabbits.

A single teaspoonful of soil contains over 4 billion micro-organisms. 

Bacteria, an essential group of soil micro-organisms, are responsible for much of the decomposition of organic material in soils. They are usually present in top soils in very large numbers and play an important role in converting more inert forms of nitrogen to ones that can more readily be taken up by plants.

 
 
                                              Earthworms are another vital species, because they help in the decomposition of organic matter in the soil, as well as improving vital functions such as aeration, water filtration, and drainage. In fertile soils they can number 2 million per hectare or more!
 Soil that is in good heart will be free-draining, easy to dig, have a crumbly texture and  a healthy earthworm population.  Heavy clay soil is sticky and prone to water logging.  It will be cold in Spring and difficult to dig; but it will hold nutrients well.  Sandy soil is very free draining and easy to work.  It will warm up easily in Spring but is nutrient poor.  The best soil is between the two and referred to as Loam 
  

                            

  



 

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