Phosphate

This article is about the orthophosphate ion. For the organophosphorus derivatives, see Organophosphate. For other phosphates, see phosphoric acids and phosphates.

Not to be confused with phosphate soda, phosphonate, or phosphorus.

Phosphate

Aromatic ball and stick model of phosphate Space-filling model of phosphate
Names
IUPAC name Phosphate
Other names Orthophosphate Tetraoxophosphate(V) Tetraoxidophosphate(V)
Identifiers
CAS Number	14265-44-2 Y
3D model (JSmol)	hypervalent form: Interactive image ionic form: Interactive image
Beilstein Reference	3903772
ChEBI	CHEBI:18367 Y
ChemSpider	1032 Y
Gmelin Reference	1997
MeSH	Phosphates
PubChem CID	1061
UNII	NK08V8K8HR Y
InChI InChI=1S/H3O4P/c1-5(2,3)4/h(H3,1,2,3,4)/p-3 Y Key: NBIIXXVUZAFLBC-UHFFFAOYSA-K Y
SMILES hypervalent form: [O-]P([O-])([O-])=O ionic form: [O-][P+]([O-])([O-])[O-]
Properties
Chemical formula	PO3− 4
Molar mass	94.9714 g mol−1
Conjugate acid	Monohydrogen phosphate
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa). Y verify (what is YN ?) Infobox references

In chemistry, a phosphate is an anion, salt, functional group or ester derived from a phosphoric acid. It most commonly means orthophosphate, a derivative of orthophosphoric acid, a.k.a. phosphoric acid H₃PO₄.

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
₂PO
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.

• 
  H
  ₃PO
  ₄
  Phosphoric
  acid
• 
  [H
  ₂PO
  ₄]⁻
  
  Dihydrogen
  phosphate
• 
  [HPO
  ₄]²⁻
  
  Hydrogen
  phosphate
• 
  [PO
  ₄]³⁻
  
  Phosphate or orthophosphate

In organic chemistry, phosphate or orthophosphate is an organophosphate, an ester of orthophosphoric acid of the form PO
₄RR′R″ where one or more hydrogen atoms are replaced by organic groups. An example is trimethyl phosphate, (CH
₃)
₃PO
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. The addition and removal of phosphate groups (phosphorylation and dephosphorylation) are key steps in cell metabolism.

Orthophosphates can condense to form pyrophosphates.

Chemical properties

The phosphate ion has a molar mass of 94.97 g/mol, and consists of a central phosphorus atom surrounded by four oxygen atoms in a tetrahedral arrangement. It is the conjugate base of the hydrogen phosphate ion H(PO
₄)²⁻
, which in turn is the conjugate base of the dihydrogen phosphate ion H
₂(PO
₄)⁻
, which in turn is the conjugate base of orthophosphoric acid, H
₃PO
₄.

Many phosphates are soluble in water at standard temperature and pressure. The sodium, potassium, rubidium, caesium, and ammonium phosphates are all water-soluble. Most other phosphates are only slightly soluble or are insoluble in water. As a rule, the hydrogen and dihydrogen phosphates are slightly more soluble than the corresponding phosphates.

Equilibria in solution

Phosphoric acid speciation

In water solution, orthophosphoric acid and its three derived anions coexist according to the dissociation and recombination equilibria below

Equilibrium	Dissociation constant Ka	pKa
H3PO4 ⇌ H2PO−4 + H+	$K_{a1}={\frac {[{\ce {H+}}][{\ce {H2PO4-}}]}{[{\ce {H3PO4}}]}}\approx 7.5\times 10^{-3}$	pKa1 = 2.14
H2PO−4 ⇌ HPO2−4 + H+	$K_{a2}={\frac {[{\ce {H+}}][{\ce {HPO4^2-}}]}{[{\ce {H2PO4-}}]}}\approx 6.2\times 10^{-8}$	pKa2 = 7.20
HPO2−4 ⇌ PO3−4 + H+	$K_{a3}={\frac {[{\ce {H+}}][{\ce {PO4^3-}}]}{[{\ce {HPO4^2-}}]}}\approx 2.14\times 10^{-13}$	pKa3 = 12.37

Values are at 25 °C and 0 ionic strength.

The pK_a values are the pH values where the concentration of each species is equal to that of its conjugate bases. At pH 1 or lower, the phosphoric acid is practically undissociated. Around pH 4.7 (mid-way between the first two pK_a values) the dihydrogen phosphate ion, [H
₂PO
₄]⁻
, is practically the only species present. Around pH 9.8 (mid-way between the second and third pK_a values) the monohydrogen phosphate ion, [HPO
₄]²⁻
, is the only species present. At pH 13 or higher, the acid is completely dissociated as the phosphate ion, (PO
₄)³⁻
.

This means that salts of the mono- and di-phosphate ions can be selectively crystallised from aqueous solution by setting the pH value to either 4.7 or 9.8.

In effect, H
₃PO
₄, H
₂(PO
₄)⁻
and H(PO
₄)²⁻
behave as separate weak acids because the successive pK_a differ by more than 4.

Phosphate can form many polymeric ions such as pyrophosphate, (P
₂O
₇)⁴⁻
, and triphosphate, (P
₃O
₁₀)⁵⁻
. The various metaphosphate ions (which are usually long linear polymers) have an empirical formula of (PO
₃)⁻
and are found in many compounds.

Biochemistry of phosphates

In biological systems, phosphorus can be found as free phosphate anions in solution (inorganic phosphate) or bound to organic molecules as various organophosphates.

Inorganic phosphate is generally denoted P_i and at physiological (homeostatic) pH primarily consists of a mixture of [HPO
₄]²⁻
and [H
₂PO
₄]⁻
ions. At a neutral pH, as in the cytosol (pH = 7.0), the concentrations of the orthophoshoric acid and its three anions have the ratios $${\begin{aligned}{\frac {[{\ce {H2PO4-}}]}{[{\ce {H3PO4}}]}}&\approx 7.5\times 10^{4}\\[4pt]{\frac {[{\ce {HPO4^2-}}]}{[{\ce {H2PO4-}}]}}&\approx 0.62\\[4pt]{\frac {[{\ce {PO4^3-}}]}{[{\ce {HPO4^2-}}]}}&\approx 2.14\times 10^{-6}\end{aligned}}$$

Thus, only [H
₂PO
₄]⁻
and [HPO
₄]²⁻
ions are present in significant amounts in the cytosol (62% [H
₂PO
₄]⁻
, 38% [HPO
₄]²⁻
). In extracellular fluid (pH = 7.4), this proportion is inverted (61% [HPO
₄]²⁻
, 39% [H
₂PO
₄]⁻
).

Inorganic phosphate can also be present as pyrophosphate anions [P
₂O
₇]⁴⁻
, which give orthophosphate by hydrolysis:

[P
₂O
₇]⁴⁻
+ H₂O ⇌ 2 [HPO
₄]²⁻

Organic phosphates are commonly found in the form of esters as nucleotides (e.g. AMP, ADP, and ATP) and in DNA and RNA. Free orthophosphate anions can be released by the hydrolysis of the phosphoanhydride bonds in ATP or ADP. These phosphorylation and dephosphorylation reactions are the immediate storage and source of energy for many metabolic processes. ATP and ADP are often referred to as high-energy phosphates, as are the phosphagens in muscle tissue. Similar reactions exist for the other nucleoside diphosphates and triphosphates.

Bones and teeth

An important occurrence of phosphates in biological systems is as the structural material of bone and teeth. These structures are made of crystalline calcium phosphate in the form of hydroxyapatite. The hard dense enamel of mammalian teeth may contain fluoroapatite, a hydroxy calcium phosphate where some of the hydroxyl groups have been replaced by fluoride ions.

Medical and biological research uses

Phosphates are medicinal salts of phosphorus. Some phosphates, which help cure many urinary tract infections, are used to make urine more acidic. To avoid the development of calcium stones in the urinary tract, some phosphates are used. For patients who are unable to get enough phosphorus in their daily diet, phosphates are used as dietary supplements, usually because of certain disorders or diseases. Injectable phosphates can only be handled by qualified health care providers.

Plant metabolism

Plants take up phosphorus through several pathways: the arbuscular mycorrhizal pathway and the direct uptake pathway.

Adverse health effects

Hyperphosphatemia, or a high blood level of phosphates, is associated with elevated mortality in the general population. The most common cause of hyperphosphatemia in people, dogs, and cats is kidney failure. In cases of hyperphosphatemia, limiting consumption of phosphate-rich foods, such as some meats and dairy items and foods with a high phosphate-to-protein ratio, such as soft drinks, fast food, processed foods, condiments, and other products containing phosphate-salt additives is advised.

Phosphates induce vascular calcification, and a high concentration of phosphates in blood was found to be a predictor of cardiovascular events.

Production

Geological occurrence

Phosphate mine near Flaming Gorge, Utah, US, 2008

Train loaded with phosphate rock, Métlaoui, Tunisia, 2012

Phosphates are the naturally occurring form of the element phosphorus, found in many phosphate minerals. In mineralogy and geology, phosphate refers to a rock or ore containing phosphate ions. Inorganic phosphates are mined to obtain phosphorus for use in agriculture and industry.

The largest global producer and exporter of phosphates is Morocco. Within North America, the largest deposits lie in the Bone Valley region of central Florida, the Soda Springs region of southeastern Idaho, and the coast of North Carolina. Smaller deposits are located in Montana, Tennessee, Georgia, and South Carolina. The small island nation of Nauru and its neighbor Banaba Island, which used to have massive phosphate deposits of the best quality, have been mined excessively. Rock phosphate can also be found in Egypt, Israel, Palestine, Western Sahara, Navassa Island, Tunisia, Togo, and Jordan, countries that have large phosphate-mining industries.

Phosphorite mines are primarily found in:

• North America:
  Main article: Phosphate mining in the United States
  United States, especially Florida, with lesser deposits in North Carolina, Idaho, and Tennessee
• Africa: Morocco, Algeria, Egypt, Niger, Senegal, Togo, Tunisia, Mauritania
• Middle East: Saudi Arabia, Jordan, Israel, Syria, Iran and Iraq, at the town of Akashat, near the Jordanian border.
• Central Asia: Kazakhstan
• Oceania: Australia, Makatea, Nauru, and Banaba Island

In 2007, at the current rate of consumption, the supply of phosphorus was estimated to run out in 345 years. However, some scientists thought that a "peak phosphorus" would occur in 30 years and Dana Cordell from Institute for Sustainable Futures said that at "current rates, reserves will be depleted in the next 50 to 100 years". Reserves refer to the amount assumed recoverable at current market prices. In 2012 the USGS estimated world reserves at 71 billion tons, while 0.19 billion tons were mined globally in 2011. Phosphorus comprises 0.1% by mass of the average rock (while, for perspective, its typical concentration in vegetation is 0.03% to 0.2%), and consequently there are quadrillions of tons of phosphorus in Earth's 3×10¹⁹-ton crust, albeit at predominantly lower concentration than the deposits counted as reserves, which are inventoried and cheaper to extract. If it is assumed that the phosphate minerals in phosphate rock are mainly hydroxyapatite and fluoroapatite, phosphate minerals contain roughly 18.5% phosphorus by weight. If phosphate rock contains around 20% of these minerals, the average phosphate rock has roughly 3.7% phosphorus by weight.

Some phosphate rock deposits, such as Mulberry in Florida, are notable for their inclusion of significant quantities of radioactive uranium isotopes. This is a concern because radioactivity can be released into surface waters from application of the resulting phosphate fertilizer.

In December 2012, Cominco Resources announced an updated JORC compliant resource of their Hinda project in Congo-Brazzaville of 531 million tons, making it the largest measured and indicated phosphate deposit in the world.

Around 2018, Norway discovered phosphate deposits almost equal to those in the rest of Earth combined.

In July 2022 China announced quotas on phosphate exportation.

The largest importers in millions of metric tons of phosphate are Brazil 3.2, India 2.9 and the USA 1.6.

Mining

Phosphate imports/exports in 1937

The three principal phosphate producer countries (China, Morocco and the United States) account for about 70% of world production.

Production and global reserves of natural phosphate by country in 2019
(USGS, 2021)

Country	Production (millions kg)	Share of global production (%)	Reserves (millions kg)
Algeria	1,300	0.54	2,200,000
Australia	2,700	1.17	1,100,000
Brazil	4,700	3.00	1,600,000
China	95,000	44.83	3,200,000
Egypt	5,000	2.47	2,800,000
Finland	995	-	1,000,000
India	1,480	0.49	46,000
Iraq	200	0.09	430,000
Israel	2,810	1.48	57,000
Jordan	9,220	3.36	800,000
Kazakhstan	1,500	0.72	260,000
Mexico	558	0.76	30,000
Morocco and Western Sahara	35,500	13.45	50,000,000
Peru	4,000	1.79	210,000
Russia	13,100	5.60	600,000
Saudi Arabia	6,500	1.48	1,400,000
Senegal	3,420	0.45	50,000
South Africa	2,100	0.99	1,400,000
Syria	2,000	0.34	1,800,000
Togo	800	0.45	30,000
Tunisia	4,110	1.79	100,000
Uzbekistan	900	-	100,000
United States	23,300	12.37	1,000,000
Vietnam	4,650	1.21	30,000
Other countries	1,140	1.17	840,000
Total	227,000	100	71,000,000

Ecology

Sea surface phosphate from the World Ocean Atlas

Relationship of phosphate to nitrate uptake for photosynthesis in various regions of the ocean. Note that nitrate is more often limiting than phosphate. See the Redfield ratio.

In ecological terms, because of its important role in biological systems, phosphate is a highly sought after resource. Once used, it is often a limiting nutrient in environments, and its availability may govern the rate of growth of organisms. This is generally true of freshwater environments, whereas nitrogen is more often the limiting nutrient in marine (seawater) environments. Addition of high levels of phosphate to environments and to micro-environments in which it is typically rare can have significant ecological consequences. For example, blooms in the populations of some organisms at the expense of others, and the collapse of populations deprived of resources such as oxygen (see eutrophication) can occur. In the context of pollution, phosphates are one component of total dissolved solids, a major indicator of water quality, but not all phosphorus is in a molecular form that algae can break down and consume.

Calcium hydroxyapatite and calcite precipitates can be found around bacteria in alluvial topsoil. As clay minerals promote biomineralization, the presence of bacteria and clay minerals resulted in calcium hydroxyapatite and calcite precipitates.

Phosphate deposits can contain significant amounts of naturally occurring heavy metals. Mining operations processing phosphate rock can leave tailings piles containing elevated levels of cadmium, lead, nickel, copper, chromium, and uranium. Unless carefully managed, these waste products can leach heavy metals into groundwater or nearby estuaries. Uptake of these substances by plants and marine life can lead to concentration of toxic heavy metals in food products.

See also

• Diammonium phosphate - (NH₄)₂HPO₄
• Disodium phosphate – Na₂HPO₄
• Fertilizer
• Hypophosphite – H
  ₂(PO
  ₂)⁻
  
• Metaphosphate – (PO
  ₃)
  _n
• Monosodium phosphate – NaH₂PO₄
• Organophosphorus compounds
• Ouled Abdoun Basin
• Phosphate – OP(OR)₃, such as triphenyl phosphate
• Phosphate conversion coating
• Phosphate soda, a soda fountain beverage
• Phosphinate – OP(OR)R₂
• Phosphine – PR₃
• Phosphine oxide – OPR₃
• Phosphinite – P(OR)R₂
• Phosphite – P(OR)₃
• Phosphogypsum
• Phosphonate – OP(OR)₂R
• Phosphonite – P(OR)₂R
• Phosphorylation
• Polyphosphate – (HPO
  ₃)
  _n
• Pyrophosphate – (P
  ₂O
  ₇)⁴⁻
  
• Sodium tripolyphosphate – Na₅P₃O₁₀

External links

• US Minerals Databrowser provides data graphics covering consumption, production, imports, exports and price for phosphate and 86 other minerals
• Phosphate: analyte monograph – The Association for Clinical Biochemistry and Laboratory Medicine