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The phosphate or orthophosphate ion [PO
4
]3−
is derived from phosphoric acid by the removal of three protons H+
. Removal of one proton gives the dihydrogen phosphate ion [H
2
PO
4
]
while removal of two protons gives the hydrogen phosphate ion [HPO
4
]2−
. These names are also used for salts of those anions, such as ammonium dihydrogen phosphate and trisodium phosphate.


In organic chemistry, phosphate or orthophosphate is an organophosphate, an ester of orthophosphoric acid of the form PO
4
RR′R″
where one or more hydrogen atoms are replaced by organic groups. An example is trimethyl phosphate, (CH
3
)
3
PO
4
. The term also refers to the trivalent functional group OP(O-)
3
in such esters. Phosphates may contain sulfur in place of one or more oxygen atoms (thiophosphates and organothiophosphates).


Orthophosphates are especially important among the various phosphates because of their key roles in biochemistry, biogeochemistry, and ecology, and their economic importance for agriculture and industry.[2] The addition and removal of phosphate groups (phosphorylation and dephosphorylation) are key steps in cell metabolism.


Orthophosphates can condense to form pyrophosphates.

North America:

United States, especially Florida, with lesser deposits in North Carolina, Idaho, and Tennessee

Phosphate mining in the United States

Africa: , Algeria, Egypt, Niger, Senegal, Togo, Tunisia, Mauritania

Morocco

Middle East: , Jordan, Israel, Syria, Iran and Iraq, at the town of Akashat, near the Jordanian border.

Saudi Arabia

Central Asia:

Kazakhstan

Oceania: , Makatea, Nauru, and Banaba Island

Australia

provides data graphics covering consumption, production, imports, exports and price for phosphate and 86 other minerals

US Minerals Databrowser

– The Association for Clinical Biochemistry and Laboratory Medicine

Phosphate: analyte monograph