Oxyacid

An oxyacid, oxoacid, or ternary acid is an acid that contains oxygen. Specifically, it is a compound that contains hydrogen, oxygen, and at least one other element, with at least one hydrogen atom bond to oxygen that can dissociate to produce the H+ cation and the anion of the acid.[1]

Description

Under Lavoisier's original theory, all acids contained oxygen, which was named from the Greek ὀξύς (oxys: acid, sharp) and the root -γενής (-genes: creator). It was later discovered that some acids, notably hydrochloric acid, did not contain oxygen and so acids were divided into oxyacids and these new hydroacids.

All oxyacids have the acidic hydrogen bound to an oxygen atom, so bond strength (length) is not a factor, as it is with binary nonmetal hydrides. Rather, the electronegativity of the central atom (X) and the number of O atoms determine oxyacid acidity. With the same central atom X, acid strength increases as the number of oxygens attached to X increases. With the same number of oxygens around E, acid strength increases with the electronegativity of X.

Compared to salt of their deprotonated forms, the oxyanions, oxyacids are generally less stable, and many of them only exist formally as hypothetical species, or exist only in solution and cannot be isolated in pure form. There are several general reasons for this: (1) they may condense to form oligomers (e.g., H2CrO4 to H2Cr2O7), or dehydrate all the way to form the anhydride (e.g., H2CO3 to CO2), (2) they may disproportionate to one compound of higher and another of lower oxidation state (e.g., HClO2 to HClO and HClO3), or (3) they might exist almost entirely as another, more stable tautomeric form (e.g., phosphorous acid P(OH)3 exists almost entirely as phosphonic acid HP(=O)(OH)2). Nevertheless, perchloric acid (HClO4), sulfuric acid (H2SO4), and nitric acid (HNO3) are a few common oxyacids that are relatively easily prepared as pure substances.

Imidic acids are created by replacing =O with =NR in an oxyacid.[2]

Properties

An oxyacid molecule contains the structure X−O−H, where other atoms or atom groups can be connected to the central atom X. In a solution, such a molecule can be dissociated into ions in two distinct ways:

  • X−O−H ⇄ (X−O) + H+
  • X−O−H ⇄ X+ + OH[3]

If the central atom X is strongly electronegative, then it strongly attracts the electrons of the oxygen atom. In that case, the bond between the oxygen and hydrogen atom is weak, and the compound ionizes easily in the way of the former of the two chemical equations above. In this case, the compound XOH is an acid, because it releases a proton, that is, a hydrogen ion. For example, nitrogen, sulfur and chlorine are strongly electronegative elements, and therefore nitric acid, sulfuric acid, and perchloric acid, are strong acids.

If, however, the electronegativity of X is low, then the compound is dissociated to ions according to the latter chemical equation, and XOH is an alkaline hydroxide. Examples of such compounds are sodium hydroxide NaOH and calcium hydroxide Ca(OH)2.[3] Owing to the high electronegativity of oxygen, however, most of the common oxobases, such as sodium hydroxide, while strongly basic in water, are only moderately basic in comparison to other bases. For example, the pKa of the conjugate acid of sodium hydroxide, water, is 15.7, while that of sodium amide, ammonia, is closer to 40, making sodium hydroxide a much weaker base than sodium amide.[3]

If the electronegativity of X is somewhere in between, the compound can be amphoteric, and in that case it can dissociate to ions in both ways, in the former case when reacting with bases, and in the latter case when reacting with acids. Examples of this include aliphatic alcohols, such as ethanol.[3]

Inorganic oxyacids typically have a chemical formula of type HmXOn, where X is an atom functioning as a central atom, whereas parameters m and n depend on the oxidation state of the element X. In most cases, the element X is a nonmetal, but some metals, for example chromium and manganese, can form oxyacids when occurring at their highest oxidation states.[3]

When oxyacids are heated, many of them dissociate to water and the anhydride of the acid. In most cases, such anhydrides are oxides of nonmetals. For example, carbon dioxide, CO2, is the anhydride of carbonic acid, H2CO3, and sulfur trioxide, SO3, is the anhydride of sulfuric acid, H2SO4. These anhydrides react quickly with water and form those oxyacids again.[4]

Many organic acids, like carboxylic acids and phenols, are oxyacids.[3] Their molecular structure, however, is much more complicated than that of inorganic oxyacids.

Most of the commonly encountered acids are oxyacids.[3] Indeed, in the 18th century, Lavoisier assumed that all acids contain oxygen and that oxygen causes their acidity. Because of this, he gave to this element its name, oxygenium, derived from Greek and meaning acid-maker, which is still, in a more or less modified form, used in most languages.[5] Later, however, Humphry Davy showed that the so-called muriatic acid did not contain oxygen, despite its being a strong acid; instead, it is a solution of hydrogen chloride, HCl.[6] Such acids which do not contain oxygen are nowadays known as hydroacids.

Names of inorganic oxyacids

Many inorganic oxyacids are traditionally called with names ending with the word acid and which also contain, in a somewhat modified form, the name of the element they contain in addition to hydrogen and oxygen. Well-known examples of such acids are sulfuric acid, nitric acid and phosphoric acid.

This practice is fully well-established, and IUPAC has accepted such names. In light of the current chemical nomenclature, this practice is, however, very exceptional, because systematic names of all other compounds are formed only according to what elements they contain and what is their molecular structure, not according to what other properties (for example, acidity) they have.[7]

IUPAC, however, recommends against calling future compounds not yet discovered with a name ending with the word acid.[7] Indeed, acids can be called with names formed by adding the word hydrogen in front of the corresponding anion; for example, sulfuric acid could just as well be called hydrogen sulfate (or dihydrogen sulfate).[8] In fact, the fully systematic name of sulfuric acid, according to IUPAC's rules, would be dihydroxidodioxidosulfur and that of the sulfate ion, tetraoxidosulfate(2−),[9] Such names, however, are almost never used.

However, the same element can form more than one acid when compounded with hydrogen and oxygen. In such cases, the English practice to distinguish such acids is to use the suffix -ic in the name of the element in the name of the acid containing more oxygen atoms, and the suffix -ous in the name of the element in the name of the acid containing fewer oxygen atoms. Thus, for example, sulfuric acid is H2SO4, and sulfurous acid, H2SO3. Analogously, nitric acid is HNO3, and nitrous acid, HNO2. If there are more than two oxyacids having the same element as the central atom, then, in some cases, acids are distinguished by adding the prefix per- or hypo- to their names. The prefix per-, however, is used only when the central atom is a halogen or a group 7 element.[8] For example, chlorine has the four following oxyacids:

The suffix -ite occurs in names of anions and salts derived from acids whose names end to the suffix -ous. On the other hand, the suffix -ate occurs in names of anions and salts derived from acids whose names end to the suffix -ic. Prefixes hypo- and per- occur in the name of anions and salts; for example the ion ClO
4
is called perchlorate.[8]

In a few cases, the prefixes ortho- and para- occur in names of some oxyacids and their derivative anions. In such cases, the para- acid is what can be thought as remaining of the ortho- acid if a water molecule is separated from the ortho- acid molecule. For example, phosphoric acid, H3PO4, has sometimes been called orthophosphoric acid, in order to distinguish it from metaphosphoric acid, HPO3.[8] However, according to IUPAC's current rules, the prefix ortho- should only be used in names of orthotelluric acid and orthoperiodic acid, and their corresponding anions and salts.[10]

Examples

In the following table, the formula and the name of the anion refer to what remains of the acid when it loses all its hydrogen atoms as protons. Many of these acids, however, are polyprotic, and in such cases, there also exists one or more intermediate anions. In name of such anions, the prefix hydrogen- (in older nomenclature bi-) is added, with numeral prefixes if needed. For example, SO2−
4
is the sulfate anion, and HSO
4
, the hydrogensulfate (or bisulfate) anion. Similarly, PO3−
4
is phosphate, HPO2−
4
is hydrogenphosphate, and H
2
PO
4
is dihydrogenphosphate.

Oxyacids and their corresponding anions
Element groupElement (central atom)Oxidation stateAcid formulaAcid name[8][9]Anion formulaAnion name
6Chromium+6H
2
CrO
4
Chromic acidCrO2−
4
Chromate
H
2
Cr
2
O
7
Dichromic acidCr
2
O2−
7
Dichromate
7Manganese+7HMnO
4
Permanganic acidMnO
4
Permanganate
+6H
2
MnO
4
Manganic acidMnO2−
4
Manganate
Technetium+7HTcO
4
Pertechnetic acidTcO
4
Pertechnetate
+6H
2
TcO
4
Technetic acidTcO2−
4
Technetate
Rhenium+7HReO
4
Perrhenic acidReO
4
Perrhenate
+6H
2
ReO
4
Tetraoxorhenic(VI) acidReO2−
4
Rhenate(VI)
+5HReO
3
Trioxorhenic(V) acidReO
3
Trioxorhenate(V)
H
3
ReO
4
Tetraoxorhenic(V) acidReO3−
4
Tetraoxorhenate(V)
H
4
Re
2
O
7
Heptaoxodirhenic(V) acidRe
2
O4−
7
Dirhenate(V)
8 Iron +6 H2FeO4 Ferric acid FeO42– Ferrate
Ruthenium +6 H2RuO4 Ruthenic acid RuO42– Ruthenate
+7 HRuO4 Perruthenic acid RuO4 Perruthenate (note difference in usage compared to osmium)
+8 H2RuO5 Hyperruthenic acid HRuO5 Hyperruthenate[11]
Osmium +6 H6OsO6 Osmic acid H4OsO62– Osmate
+8 H4OsO6 Perosmic acid H2OsO62– Perosmate (note difference in usage compared to ruthenium)
13Boron+3H
3
BO
3
Boric acid
(formerly orthoboric acid)[10]
BO3−
3
Borate
(formerly orthoborate)
(HBO
2
)
n
Metaboric acidBO
2
Metaborate
14Carbon+4H
2
CO
3
Carbonic acidCO2−
3
Carbonate
Silicon+4H
4
SiO
4
Silicic acid
(formerly orthosilicic acid)[10]
SiO4−
4
Silicate (formerly orthosilicate)
H
2
SiO
3
Metasilicic acidSiO2−
3
Metasilicate
14, 15Carbon, nitrogen+4, −3HOCNCyanic acidOCN
Cyanate
15Nitrogen+5HNO
3
Nitric acidNO
3
Nitrate
HNO
4
Peroxynitric acidNO
4
Peroxynitrate
H
3
NO
4
Orthonitric acidNO3−
4
Orthonitrate
+3HNO
2
Nitrous acidNO
2
Nitrite
HOONOPeroxynitrous acidOONO
Peroxynitrite
+2H
2
NO
2
Nitroxylic acidNO2−
2
Nitroxylate
+1H
2
N
2
O
2
Hyponitrous acidN
2
O2−
2
Hyponitrite
Phosphorus+5H
3
PO
4
Phosphoric acid
(formerly orthophosphoric acid)[10]
PO3−
4
Phosphate
(orthophosphate)
HPO
3
Metaphosphoric acidPO
3
Metaphosphate
H
4
P
2
O
7
Pyrophosphoric acid
(diphosphoric acid)
P
2
O4−
7
Pyrophosphate
(diphosphate)
H
3
PO
5
Peroxomonophosphoric acidPO3−
3
Peroxomonophosphate
+5, +3(HO)
2
POPO(OH)
2
Diphosphoric(III,V) acidO
2
POPOO2−
2
Diphosphate(III,V)
+4(HO)
2
OPPO(OH)
2
Hypophosphoric acid
(diphosphoric(IV) acid)
O
2
OPPOO4−
2
Hypophosphate
(diphosphate(IV))
+3H
2
PHO
3
Phosphonic acidPHO2−
3
Phosphonate
H
2
P
2
H
2
O
5
Diphosphonic acidP
2
H
2
O5−
3
Diphosphonate
+1HPH
2
O
2
Phosphinic acid (hypophosphorous acid)PH
2
O
2
Phosphinate (hypophosphite)
Arsenic+5H
3
AsO
4
Arsenic acidAsO3−
4
Arsenate
+3H
3
AsO
3
Arsenous acidAsO3−
3
Arsenite
16Sulfur+6H
2
SO
4
Sulfuric acidSO2−
4
Sulfate
H
2
S
2
O
7
Disulfuric acidS
2
O2−
7
Disulfate
H
2
SO
5
Peroxomonosulfuric acidSO2−
5
Peroxomonosulfate
H
2
S
2
O
8
Peroxodisulfuric acidS
2
O2−
8
Peroxodisulfate
+5H
2
S
2
O
6
Dithionic acidS
2
O2−
6
Dithionate
+5, 0H
2
S
x
O
6
Polythionic acids
(x = 3, 4...)
S
x
O2−
6
Polythionates
+4H
2
SO
3
Sulfurous acidSO2−
3
Sulfite
H
2
S
2
O
5
Disulfurous acidS
2
O2−
5
Disulfite
+4, 0H
2
S
2
O
3
Thiosulfuric acidS
2
O2−
3
Thiosulfate
+3H
2
S
2
O
4
Dithionous acidS
2
O2−
4
Dithionite
+3, −1H
2
S
2
O
2
Thiosulfurous acidS
2
O2−
2
Thiosulfite
+2H
2
SO
2
Sulfoxylic acid (hyposulfurous acid)SO2−
2
Sulfoxylate (hyposulfite)
+1H
2
S
2
O
2
DihydroxydisulfaneS
2
O2−
2
0HSOHSulfenic acidHSO
Sulfinite
Selenium+6H
2
SeO
4
Selenic acidSeO2−
4
Selenate
+4H
2
SeO
3
Selenous acidSeO2−
3
Selenite
Tellurium+6H
2
TeO
4
Telluric acidTeO2−
4
Tellurate
H
6
TeO
6
Orthotelluric acidTeO6−
6
Orthotellurate
+4H
2
TeO
3
Tellurous acidTeO2−
3
Tellurite
17Chlorine+7HClO
4
Perchloric acidClO
4
Perchlorate
+5HClO
3
Chloric acidClO
3
Chlorate
+3HClO
2
Chlorous acidClO
2
Chlorite
+1HClOHypochlorous acidClO
Hypochlorite
Bromine+7HBrO
4
Perbromic acidBrO
4
Perbromate
+5HBrO
3
Bromic acidBrO
3
Bromate
+3HBrO
2
Bromous acidBrO
2
Bromite
+1HBrOHypobromous acidBrO
Hypobromite
Iodine+7HIO
4
Periodic acidIO
4
Periodate
H
5
IO
6
Orthoperiodic acidIO5−
6
Orthoperiodate
+5HIO
3
Iodic acidIO
3
Iodate
+1HIOHypoiodous acidIO
Hypoiodite
18 Xenon +6 H2XeO4 Xenic acid HXeO4 Hydrogenxenate (dibasic xenate is unknown)
+8 H4XeO6 Perxenic acid XeO64– Perxenate

Sources

  • Kivinen, Antti; Mäkitie, Osmo (1988). Kemia (in Finnish). Helsinki, Finland: Otava. ISBN 951-1-10136-6.
  • Nomenclature of Inorganic Compounds, IUPAC Recommendations 2005 (Red Book 2005). International Union of Pure and Applied Chemistry. 2005. ISBN 0-85404-438-8.
  • Otavan suuri ensyklopedia, volume 2 (Cid-Harvey) (in Finnish). Helsinki, Finland: Otava. 1977. ISBN 951-1-04170-3.
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See also

References

  1. Chemistry, International Union of Pure and Applied. IUPAC Compendium of Chemical Terminology. iupac.org. IUPAC. doi:10.1351/goldbook.O04374.
  2. Chemistry, International Union of Pure and Applied. IUPAC Compendium of Chemical Terminology. iupac.org. IUPAC. doi:10.1351/goldbook.I02949.
  3. Kivinen, Mäkitie: Kemia, p. 202-203, chapter=Happihapot
  4. "Hapot". Otavan iso Fokus, Part 2 (El-Io). Otava. 1973. p. 990. ISBN 951-1-00272-4.
  5. Otavan suuri Ensyklopedia, s. 1606, art. Happi
  6. Otavan suuri Ensyklopedia, s. 1605, art. Hapot ja emäxet
  7. Red Book 2005, s. 124, chapter IR-8: Inorganic Acids and Derivatives
  8. Kivinen, Mäkitie: Kemia, p. 459-461, chapter Kemian nimistö: Hapot
  9. Red Book 2005, p. 129-132, table IR-8-1
  10. Red Book 2005, p. 132, note a
  11. Encyclopedia of electrochemical power sources. Garche, Jürgen., Dyer, Chris K. Amsterdam: Academic Press. 2009. p. 854. ISBN 978-0444527455. OCLC 656362152.CS1 maint: others (link)
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