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Lanthanides & Actinides
Actinide Aqueous Chemistry
Frost Diagrams for Actinides

Latimer & Frost Diagrams for elements in acid & alkaline (aq) indicate

  • actinides are quite electropositive
  • Pa - Pu show significant redox chemistry
    e.g. all 4 oxidation states of Pu can co-exist in appropriate conditions in (aq)
  • stability of high oxidation states peaks at U (Np)
  • An3+ is the maximum oxidation state for (Cf)Es - Lr
  • No2+(aq) is especially stable ~ most stable state for No in (aq)
  • redox potentials show strong dependence on pH (data for Ac - Cm)
    • high oxidation states are more stable in basic conditions
    • even at low pH hydrolysis occurs Æ formation of polymeric ions
      when hydrolysis leads to precipitation measurement of potentials is difficult!

      e.g. Pa5+ hydrolyses easily; potentials that indicate it to be the most stable oxidation state are recorded in presence of F- or C2O42-

    • tendency to disproportionation is particularly dependent on pH
      e.g. at high pH 3Pu4+ + 2H2O PuO22+ + 2Pu3+ + 4H+
  • early actinides have a tendency to form complexes
    • ~ complex formation influences reduction potentials
      e.g. Am4+(aq) only exists when complexed by fluoride (15 M NH4F(aq))
  • radiation-induced solvent decomposition produces H and OH radicals
    which lead to reduction of higher oxidation states e.g. PuV/VI, AmIV/VI

Stability of Actinide ions in aqueous solution:

Ion

Colour

Stability

Preparation

Md2+

easy to oxidize, but stable to water

Zn or Cr2+ on Md3+

No2+

stable

normal oxdn state in acid

Ac3+

colourless

stable

normal oxdn state in acid

U3+

claret

evolves H2 on standing; easily oxidized by air

Na or Zn/Hg on UO22+

Np3+

blue-purple

stable to water; easily oxidized by air

Zn/Hg or H2(Pt) reduction

Pu3+

blue-violet

stable to water & air; readily oxidized

SO2 or NH2OH reduction

Am3+

pink

stable; difficult to oxidize

I, SO2 , etc... on higher states

Cm3+

pale yellow

stable; chemical oxidation not possible

normal oxdn state in acid

Bk3+

green

stable; can be oxidized to Bk4+

normal oxdn state in acid

Cf3+

green

stable

normal oxdn state in acid

Es3+

stable

normal oxdn state in acid

Fm3+

stable

normal oxdn state in acid

Md3+

stable, but easily reduced to Md2+

normal oxdn state in acid

No3+

easily reduced to No2+

CeIV or BrO3 on No2+

Lr3+

stable

normal oxdn state in acid

Th4+

colourless

stable

normal oxdn state in acid

Pa4+

colourless

stable to water; easily oxidized

Zn/Hg on PaV(aq)

U4+

green

stable to water; easily oxidized by air to UO22+

Zn/Hg on UO22+

Np4+

yellow-green

stable to water; slowly oxidized by air to NpO2+

SO2 on NpO2+ in H2SO4

Pu4+

tan-brown

stable in 6M acid, disproportionates at higher pH

SO2 or NO2 on PuO22+

Am4+

pink?

only stable as fluoride complex; easily reduced

Am(OH)4 in 15 M NH4F

Cm4+

pale yellow

only as fluoride complex; stable only 1 hr at 25°C

CmF4 in 15 M CsF

Bk4+

yellow

marginally stable; easily reduced

Pa5+

colourless

stable; readily hydrolyzed

normal oxdn state in acid

UO2+

unstable to disproportionation (least at pH 2-4)

a transient species

NpO2+

green

stable; disproportionates at high acidity

hot HNO3 on Np4+

PuO2+

pink-purple

tends to disproportionate (least at low pH)

NH2OH on PuO22+

AmO2+

yellow

disproportionates in acid; reduced by its a-decay

ClO or cold S2O82-on Am3+

UO22+

yellow

stable; difficult to reduce

oxidation by air in HNO3

NpO22+

pink-red

stable; easy to reduce

oxidation by CeIV, MnO4, BrO3 , etc.

PuO22+

orange-pink

stable; easy to reduce; reduced by its a -decay

oxidation by CeIV, MnO4, BrO3 , etc.

AmO22+

rum-brown

easy to reduce; rapidly reduced by its a -decay

oxidation by CeIV, MnO4, BrO3 , etc.

NpO53-

deep green

only in alkaline solution

O3 or S2O82- on NpO22+ + alkali

PuO53-

deep green

only in alkaline solution; oxidizes water

O3 or S2O82- on PuO22+ + alkali

 Colour omission Þ concentrated enough solution to tell colour has not been obtained


--Info & DownloadsBibliography  [textbook & online resources]

Source: Dr. S.J. Heyes; University of Oxford
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