Clerici solution
Clerici solution is an aqueous solution of equal parts of thallium formate (Tl(HCO2)) and thallium malonate (Tl(C3H3O4)). It is freely flowing and odorless. Its color fades from yellowish to colorless upon decreasing the concentration of the thallium salts. At 4.25 g/cm3 at 20 °C, the density of saturated Clerici solution is one of the highest known. The solution was invented in 1907 by the Italian chemist Enrico Clerici (1862–1938).[1] Its value in mineralogy and gemology was reported in 1930s. It allows the separation of minerals by density with a traditional flotation method. Its advantages include transparency and an easily controllable density in the range 1–5 g/cm3.[2][3][4]
Clerici solution is more dense than spinel, garnet, diamond, and corundum as well as many other minerals.[3] The density of the saturated solution (thallium formate plus thallium malonate in water) increases from 4.25 to 5.0 g/cm3 upon heating from 20 to 90 °C (194 °F).[4] (Note that density of water decreases from 1.0 to 0.96 g/cm3 in the same temperature range.[5]) It can be reduced by diluting the solution with water down to 1 g/cm3. The refractive index shows significant, linear and well reproducible variation with the density; it changes from 1.44 for 2 g/cm3 to 1.70 for 4.28 g/cm3. Thus the density can be easily measured by optical techniques.[2]
The color of the Clerici solution changes significantly upon minor dilution. In particular, at room temperature the concentrated solution with the density of 4.25 g/cm3 is amber-yellow. However, a minor dilution with water to the density of 4.0 g/cm3 makes it as transparent as glass or water (absorption threshold 350 nm).[6]
Procedure for determining mineral density using the Clerici solution are available.[2]
One drawback of the Clerici solution is its high toxicity and corrosiveness.[2][3] Today sodium polytungstate has been introduced as a replacement, but its solutions will not reach as high in density as the Clerici solution.
References
- ↑ E. Clerici (1907). "Preparazione di liquidi per la separazione dei minerali". Atti della Reale Accademia Nazionale dei Lincei: Memorie della Classe di Scienze Fisiche, Matematiche e Naturale (in Italian). 16: 187.
- 1 2 3 4 R. H. Jahns (1939). "Clerici solution for the specific gravity determination of small mineral grains" (PDF). American Mineralogist. 24: 116.
- 1 2 3 Peter G. Read (1999). Gemmology. Butterworth-Heinemann. pp. 63–64. ISBN 0-7506-4411-7.
- 1 2 B. A. Wills, T. Napier-Munn (2006). Wills' mineral processing technology: an introduction to the practical aspects of ore treatment and mineral recovery. Butterworth-Heinemann. p. 247. ISBN 0-7506-4450-8.
- ↑ Lide, D. R. (Ed.) (1990). CRC Handbook of Chemistry and Physics (70th Edn.). Boca Raton (FL):CRC Press.
- ↑ A. Kusumegi (1982). "Total Absorption Counter and Viewing Shield by The Use of Heavy Liquidst". Bull. Inst. Chem. Res., Kyoto Univ. 60 (2): 234. hdl:2433/76969.