- published: 07 May 2015
- views: 9698
Fertile soil has the following properties:
In lands used for agriculture and other human activities, fertile soil typically arises from the use of soil conservation practices. Basically the ability of a soil to supply plant nutrients.
Bioavailable nitrogen is the element in soil that is most often lacking. Phosphorus and potassium are also needed in substantial amounts. For this reason these three elements are always identified on a commercial fertilizer analysis. For example a 10-10-15 fertilizer has 10 percent nitrogen, 10 percent (P2O5) available phosphorus and 15 percent (K2O) water soluble potassium. Sulfur is the fourth element that may be identified in a commercial analysis - e.g. 21-0-0-24 which would contain 21% nitrogen and 24% sulfate.
Inorganic fertilizers are generally less expensive and have higher concentrations of nutrients than organic fertilizers. Some have criticized the use of inorganic fertilizers, claiming that the water-soluble nitrogen doesn't provide for the long-term needs of the plant and creates water pollution. Slow-release fertilizers may reduce leaching loss of nutrients and may make the nutrients that they provide available over a longer period of time.
Soil is a natural body that consists of layers (soil horizons), composed primarily of minerals, which differ from their parent materials in their texture, structure, consistency, color, chemical, biological and other physical characteristics. The end result, soil, is the end product of the influence of the climate (temperature, precipitation), relief (slope), organisms (flora and fauna), parent materials (original minerals), temperature, and time. In engineering, soil is referred to as regolith, or loose rock material. Strictly speaking, soil is the depth of regolith that influences and has been influenced by plant roots and may range in depth from centimeters to many meters.
Soil is composed of particles of broken rock (materials) that have been altered by chemical and mechanical processes that include weathering, erosion and precipitation. Soil is altered from its parent material by the interactions between the lithosphere, hydrosphere, atmosphere, and biosphere. It is a mixture of mineral and organic materials that are in solid, gaseous and aqueous states. Soil is commonly referred to as earth or dirt; technically, the term dirt should be restricted to displaced soil.
Secrets to Soil Fertility Exposed!
Soil Fertility Best Management Practices
Build Amazing Fertile Garden Soil Using Free and Local Resources in your Mulch or Compost
Integrated soil fertility video
How To Improve Soil Fertility Naturally and Organically -Chemical Free
The Future of Soil Fertility
Soil Fertility Part 1
Build Soil Fertility with Wood Chips, Food Scraps & Bokashi
Haikyuu!! - Team of Soil Fertility [チームの地力 Chīmu no Jiriki]
2 Less-Known Methods To Improve Soil Fertility
Soils and Soil Fertility for Small Farms Thursday, January 21, 2016
How to Test the pH of Your Soil
Gary Zimmer: What is Soil Fertility?
Rainwater Harvesting and Improve Soil Fertility Methods in ICRISAT : Paadi Pantalu | ExpressTV