Phosphate is the naturally occurring form of the element phosphorus, found in many phosphate minerals. Elemental phophorus and phosphides are not found (rare phosphide minerals may be found in meteorites).
Similarly, in biological systems, phosphorus is found as phosphate ion and various phosphate esters, among others, the compounds DNA and RNA. Other compunds, such as substituted phosphines, have uses in organic chemistry but do not seem to have any natural counterparts.
For a dilute aqueous solution, phosphate can have four forms. In strongly basic conditions, phosphate ion, PO43-, is prevalent. In weakly basic conditions, the hydrogen phosphate ion, HPO42-, is most common. In weakly acid conditions, dihydrogen phosphate ion, H2PO4-, is most common. In strongly acid conditions, Aqueous Phosphoric acid, H3PO4(aq), predominates. For example, Trisodium phosphate is a strong base, disodium hydrogen phosphate is a weak base, sodium dihydrogen phosphate is a weak acid, while phosphoric acid is a strong acid.
Phosphate can form many polymeric ions, diphosphate (also pyrophosphate), P2O74-, triphosphate, P3O105-, et cetera. The various metaphosphate ions have an empirical formula of PO3- and are found in many compounds.
In a biochemical setting, a free phosphate ion in solution is called inorganic phosphate, to distinguish it from phosphates bound in the form of ATP, or perhaps in DNA or RNA. Inorganic phosphate is generally denoted Pi. Inorganic phosphate can be formed by the reactions of ATP, or ADP, with the formation of the corresponding ADP or Amp, and the release of phosphate ion. Similar reactions exist for the other Nucleoside triphosphates and diphosphates.
In living systems, phosphate ions can also be created by the hydrolysis of a larger ion called Pyrophosphate, which has the structure P2O74 -, and is denoted PPi.
Energy stored by phosphate bonds in the form of ADP or ATP, or other Nucleoside diphosphates or triphosphates, or the phosphagens in muscle tissues, is generally referred to as High energy phosphate.
[image] In Mineralogy and Geology, it refers to a rock or ore containing phosphate ions.
In ecological terms, phosphate is often a Limiting reagent in many environments--the availability of phosphate governs the rate of growth of many organisms. Introduction of non-naturally occurring levels of phosphate to those environments causes an ecological disequilibrium, leading to booms in the population of some organisms and subsequent busts in the populations of others deprived of other nutrients or essential elements by the rapid growth and consumption by the booming population.
Phosphates are often used in laundry Detergent as a water softener, but because of boom-bust cycles tied to emission of phosphates into watersheds, phosphate detergent sale or usage is restricted in some areas.
In Agriculture phosphate refers to one of the three primary Plant nutrients, and it is a component of fertilizers. Rock phosphate is quarried from phosphate beds in sedimentary rocks. In former times it was simply crushed and used as is, but the crude form is now used only in Organic farming. Normally it is chemically treated to make Superphosphate, which has a higher concentration of phosphate and is also more Soluble, therefore more quickly usable by plants.
Fertilizer grades normally have three numbers; the first is the available Nitrogen, the second is the available phosphate, and the third is the available Potash. Thus a 10-10-10 fertilizer would contain ten percent of each, with the remainder being filler.
The largest rock phosphate deposits in North America lie in the Bone Valley region of central Florida, and North Carolina. The small island nation of Nauru, which used to have massive phosphate deposits of the best quality, has been mined excessively.
Leaching of phosphates from fertilized farmland can be a cause of phosphate Pollution in surface waters, leading to Eutrophication (Algal bloom) and consequent Oxygen deficit (anoxia) for fish and other aquatic life in the same manner as phosphate-based detergents.