Soil is a surface, loose part of the Earth’s crust that is formed by the wearing of all types of rocks, the transport of small fragments and the deposition of transported fragments and particles. Soils can be divided into fine and coarse grained, and they differ from each other in their properties. Soil quality refers to the ability of soil to boost plant growth, regulate infiltration and distribution of precipitation as well as to prevent water and air pollution by buffering potential pollutants. Soil quality is determined by chemical, physical and biological properties such as the content of organic matter, soil pH, depth, density, porosity, texture and water retention capacity. Chemical properties of soil determine the ability of the soil to be supplied with nutrients and to absorb pollutants. Chemical properties of soil are important for plant growth and reproduction as well as soil fertility. It is important to understand how soil chemical properties affect the ability of soil to release and store nutrients. Physical properties are important for sustainable soil use and for agriculture. The amount and rate of adsorption of oxygen, nutrients and water depends on the ability of soil to supply the roots with nutrients. Biological properties include all plants and animals that belong to micro and macro groups of organisms and play a major role in agricultural plant production. The complex network of organisms found it soil can affect its development as well as physical and chemical properties.