In chemistry, the oxidation state, or oxidation number, is the hypothetical charge of an atom if all of its bonds to other atoms were fully ionic. It describes the degree of oxidation (loss of electrons) of an atom in a chemical compound. Conceptually, the oxidation state may be positive, negative or zero. Beside nearly-pure ionic bonding, many covalent bonds exhibit a strong ionicity, making oxidation state a useful predictor of charge.
The oxidation state of an atom does not represent the "real" charge on that atom, or any other actual atomic property. This is particularly true of high oxidation states, where the ionization energy required to produce a multiply positive ion is far greater than the energies available in chemical reactions. Additionally, the oxidation states of atoms in a given compound may vary depending on the choice of electronegativity scale used in their calculation. Thus, the oxidation state of an atom in a compound is purely a formalism. It is nevertheless important in understanding the nomenclature conventions of inorganic compounds. Also, several observations regarding chemical reactions may be explained at a basic level in terms of oxidation states.
Oxidation states are typically represented by integers which may be positive, zero, or negative. In some cases, the average oxidation state of an element is a fraction, such as 8/3 for iron in magnetite Fe3O4 (see below). The highest known oxidation state is reported to be +9, displayed by iridium in the tetroxoiridium(IX) cation (IrO+4). [1] It is predicted that even a +10 oxidation state may be achieved by platinum in tetroxoplatinum(X), PtO2+4. [2] The lowest oxidation state is −5, as for boron in Al3BC [3] and gallium in pentamagnesium digallide (Mg5Ga2).
In Stock nomenclature, which is commonly used for inorganic compounds, the oxidation state is represented by a Roman numeral placed after the element name inside parentheses or as a superscript after the element symbol, e.g. Iron(III) oxide.
The term oxidation was first used by Antoine Lavoisier to signify the reaction of a substance with oxygen. Much later, it was realized that the substance, upon being oxidized, loses electrons, and the meaning was extended to include other reactions in which electrons are lost, regardless of whether oxygen was involved. The increase in the oxidation state of an atom, through a chemical reaction, is known as oxidation; a decrease in oxidation state is known as a reduction. Such reactions involve the formal transfer of electrons: a net gain in electrons being a reduction, and a net loss of electrons being oxidation. For pure elements, the oxidation state is zero.
Oxidation numbers are assigned to elements in a molecule such that the overall sum is zero in a neutral molecule. The number indicates the degree of oxidation of each element caused by molecular bonding. In ionic molecules, the oxidation numbers are the same as the element's ionic charge. Thus for KCl, potassium is assigned +1 and chlorine is assigned -1. [4] The complete set of rules for assigning oxidation numbers are discussed in the following sections.
Oxidation numbers are fundamental the chemical nomenclature of ionic compounds. For example, Cu compounds with Cu oxidation state +2 are call cupric and those with state +1 are cuprous. [4] : 172 The oxidation numbers of elements allow predictions of chemical formula and reactions, especially oxidation-reduction reactions. The oxidation numbers of the most stable chemical compounds follow trends in the periodic table. [5] : 140
International Union of Pure and Applied Chemistry (IUPAC) has published a "Comprehensive definition of oxidation state (IUPAC Recommendations 2016)". [6] It is a distillation of an IUPAC technical report "Toward a comprehensive definition of oxidation state" from 2014. [7] The current IUPAC Gold Book definition of oxidation state is:
The oxidation state of an atom is the charge of this atom after ionic approximation of its heteronuclear bonds.
— IUPAC [8]
and the term oxidation number is nearly synonymous. [9]
The ionic approximation means extrapolating bonds to ionic. Several criteria [10] were considered for the ionic approximation:
In a bond between two different elements, the bond's electrons are assigned to its main atomic contributor typically of higher electronegativity; in a bond between two atoms of the same element, the electrons are divided equally. This is because most electronegativity scales depend on the atom's bonding state, which makes the assignment of the oxidation state a somewhat circular argument. For example, some scales may turn out unusual oxidation states, such as −6 for platinum in PtH2−4, for Pauling and Mulliken scales. [7] The dipole moments would, sometimes, also turn out abnormal oxidation numbers, such as in CO and NO, which are oriented with their positive end towards oxygen. Therefore, this leaves the atom's contribution to the bonding MO, the atomic-orbital energy, and from quantum-chemical calculations of charges, as the only viable criteria with cogent values for ionic approximation. However, for a simple estimate for the ionic approximation, we can use Allen electronegativities, [7] as only that electronegativity scale is truly independent of the oxidation state, as it relates to the average valence‐electron energy of the free atom:
Group → | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 | 15 | 16 | 17 | 18 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
↓ Period | ||||||||||||||||||
1 | H 2.300 | He 4.160 | ||||||||||||||||
2 | Li 0.912 | Be 1.576 | B 2.051 | C 2.544 | N 3.066 | O 3.610 | F 4.193 | Ne 4.787 | ||||||||||
3 | Na 0.869 | Mg 1.293 | Al 1.613 | Si 1.916 | P 2.253 | S 2.589 | Cl 2.869 | Ar 3.242 | ||||||||||
4 | K 0.734 | Ca 1.034 | Sc 1.19 | Ti 1.38 | V 1.53 | Cr 1.65 | Mn 1.75 | Fe 1.80 | Co 1.84 | Ni 1.88 | Cu 1.85 | Zn 1.588 | Ga 1.756 | Ge 1.994 | As 2.211 | Se 2.424 | Br 2.685 | Kr 2.966 |
5 | Rb 0.706 | Sr 0.963 | Y 1.12 | Zr 1.32 | Nb 1.41 | Mo 1.47 | Tc 1.51 | Ru 1.54 | Rh 1.56 | Pd 1.58 | Ag 1.87 | Cd 1.521 | In 1.656 | Sn 1.824 | Sb 1.984 | Te 2.158 | I 2.359 | Xe 2.582 |
6 | Cs 0.659 | Ba 0.881 | Lu 1.09 | Hf 1.16 | Ta 1.34 | W 1.47 | Re 1.60 | Os 1.65 | Ir 1.68 | Pt 1.72 | Au 1.92 | Hg 1.765 | Tl 1.789 | Pb 1.854 | Bi 2.01 | Po 2.19 | At 2.39 | Rn 2.60 |
7 | Fr 0.67 | Ra 0.89 | ||||||||||||||||
See also: Electronegativities of the elements (data page) |
While introductory levels of chemistry teaching use postulated oxidation states, the IUPAC recommendation [6] and the Gold Book entry [8] list two entirely general algorithms for the calculation of the oxidation states of elements in chemical compounds.
Introductory chemistry uses postulates: the oxidation state for an element in a chemical formula is calculated from the overall charge and postulated oxidation states for all the other atoms.
A simple example is based on two postulates,
where OS stands for oxidation state. This approach yields correct oxidation states in oxides and hydroxides of any single element, and in acids such as sulfuric acid (H2SO4) or dichromic acid (H2Cr2O7). Its coverage can be extended either by a list of exceptions or by assigning priority to the postulates. The latter works for hydrogen peroxide (H2O2) where the priority of rule 1 leaves both oxygens with oxidation state −1.
Additional postulates and their ranking may expand the range of compounds to fit a textbook's scope. As an example, one postulatory algorithm from many possible; in a sequence of decreasing priority:
This set of postulates covers oxidation states of fluorides, chlorides, bromides, oxides, hydroxides, and hydrides of any single element. It covers all oxoacids of any central atom (and all their fluoro-, chloro-, and bromo-relatives), as well as salts of such acids with group 1 and 2 metals. It also covers iodides, sulfides, and similar simple salts of these metals.
This algorithm is performed on a Lewis structure (a diagram that shows all valence electrons). Oxidation state equals the charge of an atom after each of its heteronuclear bonds has been assigned to the more electronegative partner of the bond (except when that partner is a reversibly bonded Lewis-acid ligand) and homonuclear bonds have been divided equally:
where each "—" represents an electron pair (either shared between two atoms or solely on one atom), and "OS" is the oxidation state as a numerical variable.
After the electrons have been assigned according to the vertical red lines on the formula, the total number of valence electrons that now "belong" to each atom is subtracted from the number N of valence electrons of the neutral atom (such as 5 for nitrogen in group 15) to yield that atom's oxidation state.
This example shows the importance of describing the bonding. Its summary formula, HNO3, corresponds to two structural isomers; the peroxynitrous acid in the above figure and the more stable nitric acid. With the formula HNO3, the simple approach without bonding considerations yields −2 for all three oxygens and +5 for nitrogen, which is correct for nitric acid. For the peroxynitrous acid, however, both oxygens in the O–O bond have OS = −1, and the nitrogen has OS = +3, which requires a structure to understand.
Organic compounds are treated in a similar manner; exemplified here on functional groups occurring in between methane (CH4) and carbon dioxide (CO2):
Analogously for transition-metal compounds; CrO(O2)2 on the left has a total of 36 valence electrons (18 pairs to be distributed), and hexacarbonylchromium (Cr(CO)6) on the right has 66 valence electrons (33 pairs):
A key step is drawing the Lewis structure of the molecule (neutral, cationic, anionic): Atom symbols are arranged so that pairs of atoms can be joined by single two-electron bonds as in the molecule (a sort of "skeletal" structure), and the remaining valence electrons are distributed such that sp atoms obtain an octet (duet for hydrogen) with a priority that increases in proportion with electronegativity. In some cases, this leads to alternative formulae that differ in bond orders (the full set of which is called the resonance formulas). Consider the sulfate anion (SO2−4) with 32 valence electrons; 24 from oxygens, 6 from sulfur, 2 of the anion charge obtained from the implied cation. The bond orders to the terminal oxygens do not affect the oxidation state so long as the oxygens have octets. Already the skeletal structure, top left, yields the correct oxidation states, as does the Lewis structure, top right (one of the resonance formulas):
The bond-order formula at the bottom is closest to the reality of four equivalent oxygens each having a total bond order of 2. That total includes the bond of order 1/2 to the implied cation and follows the 8 − N rule [7] requiring that the main-group atom's bond-order total equals 8 − N valence electrons of the neutral atom, enforced with a priority that proportionately increases with electronegativity.
This algorithm works equally for molecular cations composed of several atoms. An example is the ammonium cation of 8 valence electrons (5 from nitrogen, 4 from hydrogens, minus 1 electron for the cation's positive charge):
Drawing Lewis structures with electron pairs as dashes emphasizes the essential equivalence of bond pairs and lone pairs when counting electrons and moving bonds onto atoms. Structures drawn with electron dot pairs are of course identical in every way:
The algorithm contains a caveat, which concerns rare cases of transition-metal complexes with a type of ligand that is reversibly bonded as a Lewis acid (as an acceptor of the electron pair from the transition metal); termed a "Z-type" ligand in Green's covalent bond classification method. The caveat originates from the simplifying use of electronegativity instead of the MO-based electron allegiance to decide the ionic sign. [6] One early example is the O2S−RhCl(CO)(PPh3)2 complex [13] with sulfur dioxide (SO2) as the reversibly-bonded acceptor ligand (released upon heating). The Rh−S bond is therefore extrapolated ionic against Allen electronegativities of rhodium and sulfur, yielding oxidation state +1 for rhodium:
This algorithm works on Lewis structures and bond graphs of extended (non-molecular) solids:
Oxidation state is obtained by summing the heteronuclear-bond orders at the atom as positive if that atom is the electropositive partner in a particular bond and as negative if not, and the atom’s formal charge (if any) is added to that sum. The same caveat as above applies.
An example of a Lewis structure with no formal charge,
illustrates that, in this algorithm, homonuclear bonds are simply ignored (the bond orders are in blue).
Carbon monoxide exemplifies a Lewis structure with formal charges:
To obtain the oxidation states, the formal charges are summed with the bond-order value taken positively at the carbon and negatively at the oxygen.
Applied to molecular ions, this algorithm considers the actual location of the formal (ionic) charge, as drawn in the Lewis structure. As an example, summing bond orders in the ammonium cation yields −4 at the nitrogen of formal charge +1, with the two numbers adding to the oxidation state of −3:
The sum of oxidation states in the ion equals its charge (as it equals zero for a neutral molecule).
Also in anions, the formal (ionic) charges have to be considered when nonzero. For sulfate this is exemplified with the skeletal or Lewis structures (top), compared with the bond-order formula of all oxygens equivalent and fulfilling the octet and 8 − N rules (bottom):
A bond graph in solid-state chemistry is a chemical formula of an extended structure, in which direct bonding connectivities are shown. An example is the AuORb3 perovskite, the unit cell of which is drawn on the left and the bond graph (with added numerical values) on the right:
We see that the oxygen atom bonds to the six nearest rubidium cations, each of which has 4 bonds to the auride anion. The bond graph summarizes these connectivities. The bond orders (also called bond valences) sum up to oxidation states according to the attached sign of the bond's ionic approximation (there are no formal charges in bond graphs).
Determination of oxidation states from a bond graph can be illustrated on ilmenite, FeTiO3. We may ask whether the mineral contains Fe2+ and Ti4+, or Fe3+ and Ti3+. Its crystal structure has each metal atom bonded to six oxygens and each of the equivalent oxygens to two irons and two titaniums, as in the bond graph below. Experimental data show that three metal-oxygen bonds in the octahedron are short and three are long (the metals are off-center). The bond orders (valences), obtained from the bond lengths by the bond valence method, sum up to 2.01 at Fe and 3.99 at Ti; which can be rounded off to oxidation states +2 and +4, respectively:
Oxidation states can be useful for balancing chemical equations for oxidation-reduction (or redox) reactions, because the changes in the oxidized atoms have to be balanced by the changes in the reduced atoms. For example, in the reaction of acetaldehyde with Tollens' reagent to form acetic acid (shown below), the carbonyl carbon atom changes its oxidation state from +1 to +3 (loses two electrons). This oxidation is balanced by reducing two Ag+ cations to Ag0 (gaining two electrons in total).
An inorganic example is the Bettendorf reaction using tin dichloride (SnCl2) to prove the presence of arsenite ions in a concentrated HCl extract. When arsenic(III) is present, a brown coloration appears forming a dark precipitate of arsenic, according to the following simplified reaction:
Here three tin atoms are oxidized from oxidation state +2 to +4, yielding six electrons that reduce two arsenic atoms from oxidation state +3 to 0. The simple one-line balancing goes as follows: the two redox couples are written down as they react;
One tin is oxidized from oxidation state +2 to +4, a two-electron step, hence 2 is written in front of the two arsenic partners. One arsenic is reduced from +3 to 0, a three-electron step, hence 3 goes in front of the two tin partners. An alternative three-line procedure is to write separately the half-reactions for oxidation and reduction, each balanced with electrons, and then to sum them up such that the electrons cross out. In general, these redox balances (the one-line balance or each half-reaction) need to be checked for the ionic and electron charge sums on both sides of the equation being indeed equal. If they are not equal, suitable ions are added to balance the charges and the non-redox elemental balance.
A nominal oxidation state is a general term with two different definitions:
Lewis formulae are rule-based approximations of chemical reality, as are Allen electronegativities. Still, oxidation states may seem ambiguous when their determination is not straightforward. If only an experiment can determine the oxidation state, the rule-based determination is ambiguous (insufficient). There are also truly dichotomous values that are decided arbitrarily.
Seemingly ambiguous oxidation states are derived from a set of resonance formulas of equal weights for a molecule having heteronuclear bonds where the atom connectivity does not correspond to the number of two-electron bonds dictated by the 8 − N rule. [7] : 1027 An example is S2N2 where four resonance formulas featuring one S=N double bond have oxidation states +2 and +4 for the two sulfur atoms, which average to +3 because the two sulfur atoms are equivalent in this square-shaped molecule.
Fractional oxidation states are often used to represent the average oxidation state of several atoms of the same element in a structure. For example, the formula of magnetite is Fe
3O
4, implying an average oxidation state for iron of +8/3. [17] : 81–82 However, this average value may not be representative if the atoms are not equivalent. In a Fe
3O
4 crystal below 120 K (−153 °C), two-thirds of the cations are Fe3+
and one-third are Fe2+
, and the formula may be more clearly represented as FeO·Fe
2O
3. [18]
Likewise, propane, C
3H
8, has been described as having a carbon oxidation state of −8/3. [19] Again, this is an average value since the structure of the molecule is H
3C−CH
2−CH
3, with the first and third carbon atoms each having an oxidation state of −3 and the central one −2.
An example with true fractional oxidation states for equivalent atoms is potassium superoxide, KO
2. The diatomic superoxide ion O−
2 has an overall charge of −1, so each of its two equivalent oxygen atoms is assigned an oxidation state of −1/2. This ion can be described as a resonance hybrid of two Lewis structures, where each oxygen has an oxidation state of 0 in one structure and −1 in the other.
For the cyclopentadienyl anion C
5H−
5, the oxidation state of C is −1 + −1/5 = −6/5. The −1 occurs because each carbon is bonded to one hydrogen atom (a less electronegative element), and the −1/5 because the total ionic charge of −1 is divided among five equivalent carbons. Again this can be described as a resonance hybrid of five equivalent structures, each having four carbons with oxidation state −1 and one with −2.
Oxidation state | Example species |
---|---|
−6/5 | C 5H− 5 |
−6/7 | C 7H+ 7 |
+3/2 | C 4O2− 4 |
Finally, fractional oxidation numbers are not used in the chemical nomenclature. [20] : 66 For example the red lead Pb
3O
4 is represented as lead(II,IV) oxide, showing the oxidation states of the two nonequivalent lead atoms.
Most elements have more than one possible oxidation state. For example, carbon has nine possible integer oxidation states from −4 to +4:
Many compounds with luster and electrical conductivity maintain a simple stoichiometric formula, such as the golden TiO, blue-black RuO2 or coppery ReO3, all of obvious oxidation state. Ultimately, assigning the free metallic electrons to one of the bonded atoms is not comprehensive and can yield unusual oxidation states. Examples are the LiPb and Cu
3Au ordered alloys, the composition and structure of which are largely determined by atomic size and packing factors. Should oxidation state be needed for redox balancing, it is best set to 0 for all atoms of such an alloy.
This is a list of known oxidation states of the chemical elements, excluding nonintegral values. The most common states appear in bold. The table is based on that of Greenwood and Earnshaw, [21] with additions noted. Every element exists in oxidation state 0 when it is the pure non-ionized element in any phase, whether monatomic or polyatomic allotrope. The column for oxidation state 0 only shows elements known to exist in oxidation state 0 in compounds.
Element | Negative states | Positive states | Group | Notes | |||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
−5 | −4 | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | +8 | +9 | |||||
Z | |||||||||||||||||||
1 | hydrogen | H | −1 | +1 | 1 | ||||||||||||||
2 | helium | He | 0 | 18 | 0 [22] | ||||||||||||||
3 | lithium | Li | −1 | +1 | 1 | [23] | |||||||||||||
4 | beryllium | Be | 0 | +1 | +2 | 2 | [24] [25] | ||||||||||||
5 | boron | B | −5 | −1 | 0 | +1 | +2 | +3 | 13 | [26] [27] [28] [29] [30] [29] | |||||||||
6 | carbon | C | −4 | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 14 | |||||||
7 | nitrogen | N | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 15 | [29] [29] [31] [29] [29] [29] | ||||||
8 | oxygen | O | −2 | −1 | 0 | +1 | +2 | 16 | [29] [29] [29] | ||||||||||
9 | fluorine | F | −1 | 17 | |||||||||||||||
10 | neon | Ne | 0 | 18 | 0 [32] | ||||||||||||||
11 | sodium | Na | −1 | 0 | +1 | 1 | [29] [33] | ||||||||||||
12 | magnesium | Mg | 0 | +1 | +2 | 2 | [34] [35] | ||||||||||||
13 | aluminium | Al | −2 | −1 | 0 | +1 | +2 | +3 | 13 | [36] [37] [38] [29] [39] [40] | |||||||||
14 | silicon | Si | −4 | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 14 | [29] [29] [29] [41] [29] [42] [29] [29] | ||||||
15 | phosphorus | P | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 15 | [29] [29] [43] [29] [44] [29] [29] | ||||||
16 | sulfur | S | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 16 | [29] [29] [29] [29] | ||||||
17 | chlorine | Cl | −1 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 17 | [29] [29] [29] | |||||||
18 | argon | Ar | 0 | 18 | 0 [45] | ||||||||||||||
19 | potassium | K | −1 | +1 | 1 | [46] | |||||||||||||
20 | calcium | Ca | +1 | +2 | 2 | [47] | |||||||||||||
21 | scandium | Sc | 0 | +1 | +2 | +3 | 3 | [48] [49] [50] | |||||||||||
22 | titanium | Ti | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 4 | [51] [29] [52] [53] [29] [29] | ||||||||
23 | vanadium | V | −3 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 5 | [54] [29] [55] [29] [29] [29] [29] | |||||||
24 | chromium | Cr | −4 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 6 | [56] [29] [29] [57] [29] [29] [29] [29] | |||||
25 | manganese | Mn | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 7 | [29] [58] [29] [29] [29] [29] [29] [29] [29] | ||||
26 | iron | Fe | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 8 | [29] [29] [29] [59] [29] [60] [29] [61] | |||||
27 | cobalt | Co | −3 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 9 | [62] [29] [29] [29] [29] [63] | |||||||
28 | nickel | Ni | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 10 | [64] [29] [65] [66] [29] [67] | ||||||||
29 | copper | Cu | −2 | 0 | +1 | +2 | +3 | +4 | 11 | [68] [69] [29] [29] [29] | |||||||||
30 | zinc | Zn | −2 | 0 | +1 | +2 | 12 | [70] [71] ? | |||||||||||
31 | gallium | Ga | −5 | −4 | −3 | −2 | −1 | 0 | +1 | +2 | +3 | 13 | [72] [72] [73] [72] [74] [75] [29] [29] | ||||||
32 | germanium | Ge | −4 | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 14 | [76] [76] [76] [77] [29] [29] | ||||||
33 | arsenic | As | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 15 | [78] [79] [80] [81] [29] [82] | ||||||
34 | selenium | Se | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 16 | [83] [84] [85] [86] ? | ||||||
35 | bromine | Br | −1 | +1 | +2 | +3 | +4 | +5 | +7 | 17 | [87] [29] [29] | ||||||||
36 | krypton | Kr | +1 | +2 | 18 | ? | |||||||||||||
37 | rubidium | Rb | −1 | +1 | 1 | [88] | |||||||||||||
38 | strontium | Sr | +1 | +2 | 2 | [89] | |||||||||||||
39 | yttrium | Y | 0 | +1 | +2 | +3 | 3 | [90] [29] ? | |||||||||||
40 | zirconium | Zr | −2 | 0 | +1 | +2 | +3 | +4 | 4 | [91] [92] [29] [93] [94] [29] | |||||||||
41 | niobium | Nb | −3 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 5 | [95] [29] [96] [96] [29] [29] [29] | |||||||
42 | molybdenum | Mo | −4 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 6 | [97] [29] [29] [98] [29] [29] [29] [29] | |||||
43 | technetium | Tc | −1 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 7 | [29] [29] [29] [29] [29] [29] | |||||||
44 | ruthenium | Ru | −2 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | +8 | 8 | [29] [29] [29] [29] [29] [29] [29] | ||||||
45 | rhodium | Rh | −3 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 9 | [99] [29] [100] [29] [29] [29] [29] [29] [101] | |||||
46 | palladium | Pd | 0 | +1 | +2 | +3 | +4 | +5 | 10 | [102] [103] [104] | |||||||||
47 | silver | Ag | −2 | −1 | 0 | +1 | +2 | +3 | 11 | [105] [106] [107] [29] [29] | |||||||||
48 | cadmium | Cd | −2 | +1 | +2 | 12 | [108] [109] | ||||||||||||
49 | indium | In | −5 | −2 | −1 | 0 | +1 | +2 | +3 | 13 | [110] [111] [112] [113] [29] [29] | ||||||||
50 | tin | Sn | −4 | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 14 | [114] [115] [116] [117] [118] [119] | ||||||
51 | antimony | Sb | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 15 | [120] [120] [121] [122] [123] ? | ||||||
52 | tellurium | Te | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 16 | [29] ? | ||||||
53 | iodine | I | −1 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 17 | [124] ? | |||||||
54 | xenon | Xe | 0 | +2 | +4 | +6 | +8 | 18 | [125] [126] | ||||||||||
55 | caesium | Cs | −1 | +1 | 1 | [127] | |||||||||||||
56 | barium | Ba | +1 | +2 | 2 | [128] | |||||||||||||
57 | lanthanum | La | 0 | +1 | +2 | +3 | f-block groups | [90] [129] [29] | |||||||||||
58 | cerium | Ce | +2 | +3 | +4 | f-block groups | [29] | ||||||||||||
59 | praseodymium | Pr | 0 | +1 | +2 | +3 | +4 | +5 | f-block groups | [90] [130] [131] ? | |||||||||
60 | neodymium | Nd | 0 | +2 | +3 | +4 | f-block groups | [90] [29] | |||||||||||
61 | promethium | Pm | +2 | +3 | f-block groups | ? | |||||||||||||
62 | samarium | Sm | 0 | +1 | +2 | +3 | f-block groups | [90] [132] [29] | |||||||||||
63 | europium | Eu | 0 | +2 | +3 | f-block groups | 0 [90] | ||||||||||||
64 | gadolinium | Gd | 0 | +1 | +2 | +3 | f-block groups | [90] [29] [29] | |||||||||||
65 | terbium | Tb | 0 | +1 | +2 | +3 | +4 | f-block groups | [90] [129] [131] [29] | ||||||||||
66 | dysprosium | Dy | 0 | +2 | +3 | +4 | f-block groups | [90] [29] | |||||||||||
67 | holmium | Ho | 0 | +2 | +3 | f-block groups | [90] [131] | ||||||||||||
68 | erbium | Er | 0 | +2 | +3 | f-block groups | [90] [131] | ||||||||||||
69 | thulium | Tm | 0 | +1 | +2 | +3 | f-block groups | [90] [129] [29] | |||||||||||
70 | ytterbium | Yb | 0 | +1 | +2 | +3 | f-block groups | [90] [129] [29] | |||||||||||
71 | lutetium | Lu | 0 | +2 | +3 | 3 | [90] [131] | ||||||||||||
72 | hafnium | Hf | −2 | 0 | +1 | +2 | +3 | +4 | 4 | [133] [134] [135] [29] [29] | |||||||||
73 | tantalum | Ta | −3 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 5 | [136] [29] [137] [138] [29] [29] [29] | |||||||
74 | tungsten | W | −4 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 6 | [139] [29] [29] [140] [29] [29] [29] [29] | |||||
75 | rhenium | Re | −3 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | 7 | [29] [29] [141] [29] [29] [29] [29] [29] | |||||
76 | osmium | Os | −4 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | +8 | 8 | [29] [29] [29] [29] [29] [29] [29] [29] ? | |||
77 | iridium | Ir | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | +7 | +8 | +9 | 9 | [29] [29] [29] [29] [29] [142] ? | ||
78 | platinum | Pt | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | +6 | 10 | [29] [29] ? | |||||
79 | gold | Au | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +5 | 11 | [29] [143] [29] [29] ? | |||||||
80 | mercury | Hg | −2 | +1 | +2 | 12 | [144] | ||||||||||||
81 | thallium | Tl | −5 | −2 | −1 | +1 | +2 | +3 | 13 | [145] ? | |||||||||
82 | lead | Pb | −4 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | 14 | [29] [146] ? | |||||||
83 | bismuth | Bi | −3 | −2 | −1 | 0 | +1 | +2 | +3 | +4 | +5 | 15 | [29] [147] [29] ? | ||||||
84 | polonium | Po | −2 | +2 | +4 | +5 | +6 | 16 | [148] [29] | ||||||||||
85 | astatine | At | −1 | +1 | +3 | +5 | +7 | 17 | [29] [29] [29] | ||||||||||
86 | radon | Rn | +2 | +6 | 18 | ? | |||||||||||||
87 | francium | Fr | +1 | 1 | |||||||||||||||
88 | radium | Ra | +2 | 2 | |||||||||||||||
89 | actinium | Ac | +3 | f-block groups | |||||||||||||||
90 | thorium | Th | −1 | +1 | +2 | +3 | +4 | f-block groups | [149] [29] [29] ? | ||||||||||
91 | protactinium | Pa | +2 | +3 | +4 | +5 | f-block groups | [29] [29] ? | |||||||||||
92 | uranium | U | −1 | +1 | +2 | +3 | +4 | +5 | +6 | f-block groups | [149] [150] [29] [29] ? | ||||||||
93 | neptunium | Np | +2 | +3 | +4 | +5 | +6 | +7 | f-block groups | [29] [151] [29] [29] ? | |||||||||
94 | plutonium | Pu | +2 | +3 | +4 | +5 | +6 | +7 | +8 | f-block groups | [29] , [29] [29] [29] ? | ||||||||
95 | americium | Am | +2 | +3 | +4 | +5 | +6 | +7 | f-block groups | [29] [29] [29] [29] | |||||||||
96 | curium | Cm | +3 | +4 | +5 | +6 | f-block groups | [29] [152] [153] | |||||||||||
97 | berkelium | Bk | +2 | +3 | +4 | +5 | f-block groups | [29] [152] ? | |||||||||||
98 | californium | Cf | +2 | +3 | +4 | +5 | f-block groups | [29] [29] [154] [152] | |||||||||||
99 | einsteinium | Es | +2 | +3 | +4 | f-block groups | [29] | ||||||||||||
100 | fermium | Fm | +2 | +3 | f-block groups | [29] | |||||||||||||
101 | mendelevium | Md | +2 | +3 | f-block groups | [29] | |||||||||||||
102 | nobelium | No | +2 | +3 | f-block groups | [29] | |||||||||||||
103 | lawrencium | Lr | +3 | 3 | |||||||||||||||
104 | rutherfordium | Rf | +3 | +4 | 4 | [155] | |||||||||||||
105 | dubnium | Db | +3 | +4 | +5 | 5 | [155] | ||||||||||||
106 | seaborgium | Sg | +3 | +4 | +5 | +6 | 6 | [155] | |||||||||||
107 | bohrium | Bh | +3 | +4 | +5 | +7 | 7 | [155] | |||||||||||
108 | hassium | Hs | +3 | +4 | +6 | +8 | 8 | [155] | |||||||||||
109 | meitnerium | Mt | +1 | +3 | +6 | 9 | [155] | ||||||||||||
110 | darmstadtium | Ds | +2 | +4 | +6 | 10 | [155] | ||||||||||||
111 | roentgenium | Rg | −1 | +3 | +5 | 11 | [155] | ||||||||||||
112 | copernicium | Cn | +2 | +4 | 12 | [155] | |||||||||||||
113 | nihonium | Nh | 13 | ||||||||||||||||
114 | flerovium | Fl | 14 | ||||||||||||||||
115 | moscovium | Mc | 15 | ||||||||||||||||
116 | livermorium | Lv | −2 | +4 | 16 | [156] | |||||||||||||
117 | tennessine | Ts | −1 | +5 | 17 | ||||||||||||||
118 | oganesson | Og | −1 | +1 | +2 | +4 | +6 | 18 | [155] [157] [158] [158] [155] |
A figure with a similar format was used by Irving Langmuir in 1919 in one of the early papers about the octet rule. [159] The periodicity of the oxidation states was one of the pieces of evidence that led Langmuir to adopt the rule.
The oxidation state in compound naming for transition metals and lanthanides and actinides is placed either as a right superscript to the element symbol in a chemical formula, such as FeIII or in parentheses after the name of the element in chemical names, such as iron(III). For example, Fe
2(SO
4)
3 is named iron(III) sulfate and its formula can be shown as FeIII
2(SO
4)
3. This is because a sulfate ion has a charge of −2, so each iron atom takes a charge of +3.
Oxidation itself was first studied by Antoine Lavoisier, who defined it as the result of reactions with oxygen (hence the name). [160] [161] The term has since been generalized to imply a formal loss of electrons. Oxidation states, called oxidation grades by Friedrich Wöhler in 1835, [162] were one of the intellectual stepping stones that Dmitri Mendeleev used to derive the periodic table. [163] William B. Jensen [164] gives an overview of the history up to 1938.
When it was realized that some metals form two different binary compounds with the same nonmetal, the two compounds were often distinguished by using the ending -ic for the higher metal oxidation state and the ending -ous for the lower. For example, FeCl3 is ferric chloride and FeCl2 is ferrous chloride. This system is not very satisfactory (although sometimes still used) because different metals have different oxidation states which have to be learned: ferric and ferrous are +3 and +2 respectively, but cupric and cuprous are +2 and +1, and stannic and stannous are +4 and +2. Also, there was no allowance for metals with more than two oxidation states, such as vanadium with oxidation states +2, +3, +4, and +5. [17] : 84
This system has been largely replaced by one suggested by Alfred Stock in 1919 [165] and adopted [166] by IUPAC in 1940. Thus, FeCl2 was written as iron(II) chloride rather than ferrous chloride. The Roman numeral II at the central atom came to be called the "Stock number" (now an obsolete term), and its value was obtained as a charge at the central atom after removing its ligands along with the electron pairs they shared with it. [20] : 147
The term "oxidation state" in English chemical literature was popularized by Wendell Mitchell Latimer in his 1938 book about electrochemical potentials. [167] He used it for the value (synonymous with the German term Wertigkeit) previously termed "valence", "polar valence" or "polar number" [168] in English, or "oxidation stage" or indeed [169] [170] the "state of oxidation". Since 1938, the term "oxidation state" has been connected with electrochemical potentials and electrons exchanged in redox couples participating in redox reactions. By 1948, IUPAC used the 1940 nomenclature rules with the term "oxidation state", [171] [172] instead of the original [166] valency. In 1948 Linus Pauling proposed that oxidation number could be determined by extrapolating bonds to being completely ionic in the direction of electronegativity. [173] A full acceptance of this suggestion was complicated by the fact that the Pauling electronegativities as such depend on the oxidation state and that they may lead to unusual values of oxidation states for some transition metals. In 1990 IUPAC resorted to a postulatory (rule-based) method to determine the oxidation state. [174] This was complemented by the synonymous term oxidation number as a descendant of the Stock number introduced in 1940 into the nomenclature. However, the terminology using "ligands" [20] : 147 gave the impression that oxidation number might be something specific to coordination complexes. This situation and the lack of a real single definition generated numerous debates about the meaning of oxidation state, suggestions about methods to obtain it and definitions of it. To resolve the issue, an IUPAC project (2008-040-1-200) was started in 2008 on the "Comprehensive Definition of Oxidation State", and was concluded by two reports [7] [6] and by the revised entries "Oxidation State" [8] and "Oxidation Number" [9] in the IUPAC Gold Book. The outcomes were a single definition of oxidation state and two algorithms to calculate it in molecular and extended-solid compounds, guided by Allen electronegativities that are independent of oxidation state.
The alkali metals consist of the chemical elements lithium (Li), sodium (Na), potassium (K), rubidium (Rb), caesium (Cs), and francium (Fr). Together with hydrogen they constitute group 1, which lies in the s-block of the periodic table. All alkali metals have their outermost electron in an s-orbital: this shared electron configuration results in their having very similar characteristic properties. Indeed, the alkali metals provide the best example of group trends in properties in the periodic table, with elements exhibiting well-characterised homologous behaviour. This family of elements is also known as the lithium family after its leading element.
Electronegativity, symbolized as χ, is the tendency for an atom of a given chemical element to attract shared electrons when forming a chemical bond. An atom's electronegativity is affected by both its atomic number and the distance at which its valence electrons reside from the charged nucleus. The higher the associated electronegativity, the more an atom or a substituent group attracts electrons. Electronegativity serves as a simple way to quantitatively estimate the bond energy, and the sign and magnitude of a bond's chemical polarity, which characterizes a bond along the continuous scale from covalent to ionic bonding. The loosely defined term electropositivity is the opposite of electronegativity: it characterizes an element's tendency to donate valence electrons.
Ionic bonding is a type of chemical bonding that involves the electrostatic attraction between oppositely charged ions, or between two atoms with sharply different electronegativities, and is the primary interaction occurring in ionic compounds. It is one of the main types of bonding, along with covalent bonding and metallic bonding. Ions are atoms with an electrostatic charge. Atoms that gain electrons make negatively charged ions. Atoms that lose electrons make positively charged ions. This transfer of electrons is known as electrovalence in contrast to covalence. In the simplest case, the cation is a metal atom and the anion is a nonmetal atom, but these ions can be more complex, e.g. molecular ions like NH+
4 or SO2−
4. In simpler words, an ionic bond results from the transfer of electrons from a metal to a non-metal to obtain a full valence shell for both atoms.
A metallocene is a compound typically consisting of two cyclopentadienyl anions (C
5H−
5, abbreviated Cp) bound to a metal center (M) in the oxidation state II, with the resulting general formula (C5H5)2M. Closely related to the metallocenes are the metallocene derivatives, e.g. titanocene dichloride or vanadocene dichloride. Certain metallocenes and their derivatives exhibit catalytic properties, although metallocenes are rarely used industrially. Cationic group 4 metallocene derivatives related to [Cp2ZrCH3]+ catalyze olefin polymerization.
In chemistry, a hydride is formally the anion of hydrogen (H−), a hydrogen ion with two electrons. In modern usage, this is typically only used for ionic bonds, but it is sometimes (and more frequently in the past) been applied to all compounds containing covalently bound H atoms. In this broad and potentially archaic sense, water (H2O) is a hydride of oxygen, ammonia is a hydride of nitrogen, etc. In covalent compounds, it implies hydrogen is attached to a less electronegative element. In such cases, the H centre has nucleophilic character, which contrasts with the protic character of acids. The hydride anion is very rarely observed.
The octet rule is a chemical rule of thumb that reflects the theory that main-group elements tend to bond in such a way that each atom has eight electrons in its valence shell, giving it the same electronic configuration as a noble gas. The rule is especially applicable to carbon, nitrogen, oxygen, and the halogens; although more generally the rule is applicable for the s-block and p-block of the periodic table. Other rules exist for other elements, such as the duplet rule for hydrogen and helium, and the 18-electron rule for transition metals.
In chemistry, catenation is the bonding of atoms of the same element into a series, called a chain. A chain or a ring may be open if its ends are not bonded to each other, or closed if they are bonded in a ring. The words to catenate and catenation reflect the Latin root catena, "chain".
The inert-pair effect is the tendency of the two electrons in the outermost atomic s-orbital to remain unshared in compounds of post-transition metals. The term inert-pair effect is often used in relation to the increasing stability of oxidation states that are two less than the group valency for the heavier elements of groups 13, 14, 15 and 16. The term "inert pair" was first proposed by Nevil Sidgwick in 1927. The name suggests that the outermost s electron pairs are more tightly bound to the nucleus in these atoms, and therefore more difficult to ionize or share.
Valence shell electron pair repulsion (VSEPR) theory is a model used in chemistry to predict the geometry of individual molecules from the number of electron pairs surrounding their central atoms. It is also named the Gillespie-Nyholm theory after its two main developers, Ronald Gillespie and Ronald Nyholm.
The bond valencemethod or mean method is a popular method in coordination chemistry to estimate the oxidation states of atoms. It is derived from the bond valence model, which is a simple yet robust model for validating chemical structures with localized bonds or used to predict some of their properties. This model is a development of Pauling's rules.
Iron shows the characteristic chemical properties of the transition metals, namely the ability to form variable oxidation states differing by steps of one and a very large coordination and organometallic chemistry: indeed, it was the discovery of an iron compound, ferrocene, that revolutionalized the latter field in the 1950s. Iron is sometimes considered as a prototype for the entire block of transition metals, due to its abundance and the immense role it has played in the technological progress of humanity. Its 26 electrons are arranged in the configuration [Ar]3d64s2, of which the 3d and 4s electrons are relatively close in energy, and thus it can lose a variable number of electrons and there is no clear point where further ionization becomes unprofitable.
Metal nitrosyl complexes are complexes that contain nitric oxide, NO, bonded to a transition metal. Many kinds of nitrosyl complexes are known, which vary both in structure and coligand.
An alkalide is a chemical compound in which alkali metal atoms are anions with a charge or oxidation state of −1. Until the first discovery of alkalides in the 1970s, alkali metals were known to appear in salts only as cations with a charge or oxidation state of +1. These types of compounds are of theoretical interest due to their unusual stoichiometry and low ionization potentials. Alkalide compounds are chemically related to the electrides, salts in which trapped electrons are effectively the anions.
In chemistry, a Zintl phase is a product of a reaction between a group 1 or group 2 and main group metal or metalloid. It is characterized by intermediate metallic/ionic bonding. Zintl phases are a subgroup of brittle, high-melting intermetallic compounds that are diamagnetic or exhibit temperature-independent paramagnetism and are poor conductors or semiconductors.
The carbon–fluorine bond is a polar covalent bond between carbon and fluorine that is a component of all organofluorine compounds. It is one of the strongest single bonds in chemistry, and relatively short, due to its partial ionic character. The bond also strengthens and shortens as more fluorines are added to the same carbon on a chemical compound. As such, fluoroalkanes like tetrafluoromethane are some of the most unreactive organic compounds.
A hexafluoride is a chemical compound with the general formula QXnF6, QXnF6m−, or QXnF6m+. Many molecules fit this formula. An important hexafluoride is hexafluorosilicic acid (H2SiF6), which is a byproduct of the mining of phosphate rock. In the nuclear industry, uranium hexafluoride (UF6) is an important intermediate in the purification of this element.
A stannide can refer to an intermetallic compound containing tin combined with one or more other metals; an anion consisting solely of tin atoms or a compound containing such an anion, or, in the field of organometallic chemistry an ionic compound containing an organotin anion
Fluorine forms a great variety of chemical compounds, within which it always adopts an oxidation state of −1. With other atoms, fluorine forms either polar covalent bonds or ionic bonds. Most frequently, covalent bonds involving fluorine atoms are single bonds, although at least two examples of a higher order bond exist. Fluoride may act as a bridging ligand between two metals in some complex molecules. Molecules containing fluorine may also exhibit hydrogen bonding. Fluorine's chemistry includes inorganic compounds formed with hydrogen, metals, nonmetals, and even noble gases; as well as a diverse set of organic compounds. For many elements the highest known oxidation state can be achieved in a fluoride. For some elements this is achieved exclusively in a fluoride, for others exclusively in an oxide; and for still others the highest oxidation states of oxides and fluorides are always equal.
The phosphaethynolate anion, also referred to as PCO, is the phosphorus-containing analogue of the cyanate anion with the chemical formula [PCO]− or [OCP]−. The anion has a linear geometry and is commonly isolated as a salt. When used as a ligand, the phosphaethynolate anion is ambidentate in nature meaning it forms complexes by coordinating via either the phosphorus or oxygen atoms. This versatile character of the anion has allowed it to be incorporated into many transition metal and actinide complexes but now the focus of the research around phosphaethynolate has turned to utilising the anion as a synthetic building block to organophosphanes.
Aluminium(I) nucleophiles are a group of inorganic and organometallic nucleophilic compounds containing at least one aluminium metal center in the +1 oxidation state with a lone pair of electrons strongly localized on the aluminium(I) center.
MgHg then lends itself to an oxidation state of +2 for Mg and -2 for Hg because it consists entirely of these polar bonds with no evidence of electron unpairing. (translated)