Polythionic acid

Polythionic acid is an oxoacid which has a straight chain of sulfur atoms and has the chemical formula Sn(SO3H)2 (n > 2). Trithionic acid (H2S3O6), tetrathionic acid (H2S4O6) are simple examples. They are the conjugate acids of polythionates. The compounds of n < 80 are expected to exist, and those of n < 20 have already been synthesized. Dithionic acid (H2S2O6) does not belong to the polythionic acids due to strongly different properties.

Skeletal formula of polythionic acid

Nomenclature

All polythionates anion contains chains of sulfur atoms attached to the terminal SO3H-groups. Names of polythionic acids are determined by the number of atoms in the chain of sulfur atoms:

History

Numerous acids and salts of this group have a venerable history, and chemistry systems, where they exist, dates back to the studies John Dalton devoted to the behavior of hydrogen sulfide in aqueous solutions of sulfur dioxide (1808). This solution now has the name of Heinrich Wilhelm Ferdinand Wackenroder, who conducted a systematic study (1846). Over the next 60–80 years, numerous studies have shown the presence of ions, in particular tetrathionate and pentathionate anion (S
4
O2−
6
and S
5
O2−
6
, respectively).

Preparation and properties

In the last few decades in the work of Schmidt and other scientists in Germany, a new idea formed: as H
2
S
can react with SO
3
or HSO
3
Cl
, forming thiosulfuric acid H
2
S
2
O
3
, as the analogous reaction with H
2
S
2
forms disulfonomonosulfonic acid HS
2
SO
3
H
; similarly polysulfanes H2Sn (n = 2–6) give HSnSO3H. Reactions from both ends of the polysulfane chain lead to the formation of polysulfonodisulfonic acid HO3SSnSO3H.

There are many known methods for the synthesis of these acids, but the reaction mechanism is unclear because of the large number of simultaneously occurring and competing reactions such as redox, chain transfer, and disproportionation. Typical examples are:

  • Interaction between hydrogen sulfide and sulfur dioxide in highly dilute aqueous solution. This yields a complex mixture of various oxyacids of sulfur of different structures, called Wackenroder solution. At temperatures above 20 °C solutes slowly decomposes with separation unit sulfur, sulfur dioxide, and sulfuric acid.[1]
H2S + H2SO3 H2S2O2 + H2O
H2S2O2 + 2 H2SO3 H2S4O6 + 2 H2O
H2S4O6 + H2SO3 H2S3O6 + H2S2O3
  • Reactions of sulfur halides with HSO
    3
    or HS
    2
    O
    3
    , for example :
SCl2 + 2 HSO
3
→ [O3SSSO 3]2− + 2 HCl
S2Cl2 + 2 HSO
3
→ [O3SS2SO3]2− + 2 HCl
SCl2 + 2 HS
2
O
3
→ [O3SS3SO3]2− + 2 HCl

Anhydrous polythionic acids can be formed in diethyl ether solution by the following three general ways:

HSnSO3H + SO3 → H2Sn+2O6 (n = 1, 2 … 8)
H2Sn + 2 SO3 → H2Sn+2O6 (n = 1, 2 … 8)
2 HSnSO3H + I2 → H2S2n+2O6 + 2 HI (n = 1, 2 … 6)

Polythionic acids with a small number of sulfur atoms in the chain (n = 3, 4, 5, 6) are the most stable. Polythionic acids are stable only in aqueous solutions, and are rapidly destroyed at higher concentrations with the release of sulfur, sulfur dioxide and - sometimes - sulfuric acid. Acid salts of polythionic acids do not exist. Polythionate ions are significantly more stable than the corresponding acids.

Under the action of oxidants (potassium permanganate, potassium dichromate) polythionic acids and their salts are oxidized to sulfate, and the interaction with strong reducing agents (amalgam of sodium) converts them into sulfites and dithionites.

Occurrence

Polythionic acids are often found in crater lakes. There are various kinds of ions containing sulfur atoms derived by hydrogen sulfide and they make the strongly acidic conditions. It is observed that polythionates in crater lakes are drastically decreased before an eruption occurs.[2] The phenomenon may be useful to predict volcanic activity.

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References

  1. Sarkar, Ramaprasad. General and inorganic chemistry. New Central Book Agency. p. 483. ISBN 9788173817274.
  2. Takano, B. (1987). "Correlation of Volcanic Activity with Sulfur Oxyanion Speciation in a Crater Lake". Science. 235 (4796): 1633–1635. doi:10.1126/science.235.4796.1633. PMID 17795598.
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