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Have you ever looked at the soil in your garden and considered it as anything more than soil? If not you should because there is a lot more there than meets the eye. It performs many functions that you may not be aware of and having good quality soil in your garden is essential for your plants. In this article we will look at the functions of soil,casque beats, what different types there are and finally some ways to make it healthier.
Functions of Soil
The most immediately apparent function of soil is a medium to support plant life. It provides support both physically and biologically. Physical support is provided by allowing the plant to grow its roots through the soil to hold itself in place. Biological support is provided by its ability to hold nutrients and water that the plant needs. It also supports other types of life as well. Microorganisms and insects live in the soil and they in turn aid plant life by helping to decay organic material and adding structure to the soil. Soil allows the growth of food crops which are consumed by humans and also plants used in the creation of medicines. Microorganisms like fungi and bacteria that live in soil and are used to produce antibiotics. All life on earth is dependant on it either directly and indirectly. This includes the plant life in your garden.
What is Soil Made of?
The four major components of soil are mineral matter,casque dr dre, organic matter (humus),louboutin, water and air. Mineral matter refers to the inorganic elements in the soil e.g. stones,ralph lauren, gravel and makes up to 40%-60% of its volume. This part of the soil usually originates from the bedrock that lies beneath the soil. Organic matter (humus) is the decayed remains and waste products of plants and animals and has a great effect on the chemical properties of the soil e.g. availability of nutrients. Almost 40%-60% of a soil's volume can be space and this is occupied by water and air.
Different Types of Soil Texture
Soil texture is defined as the size distribution of different mineral particles. These mineral particles are at their most basic level the following: sand,moncler, silt and clay. Sand particles are 2 to 0.05 mm diameter,giubbotti moncler, silt particles are 0.05 to 0.002 mm diameter and clay particles are
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