PURIFICATION, RECOVERY, AND LASER-DRIVEN FLUORINATION OF SILICON FROMDISSOLVED AND PARTICULATE SILICA FOR THE MEASUREMENT OF NATURAL STABLE-ISOTOPE ABUNDANCES
Cl. Delarocha et al., PURIFICATION, RECOVERY, AND LASER-DRIVEN FLUORINATION OF SILICON FROMDISSOLVED AND PARTICULATE SILICA FOR THE MEASUREMENT OF NATURAL STABLE-ISOTOPE ABUNDANCES, Analytical chemistry, 68(21), 1996, pp. 3746-3750
A procedure for the purification, recovery, and determination of isoto
pic abundances of silicon from biogenic and lithogenic particulate mat
ter and dissolved silicic acid is reported, Purification involves the
reaction of acid molybdate with dissolved silicon in natural waters or
that produced by the dissolution of particulate silica by hydrofluori
c acid. The resulting silicomolybdic acid is then quantitatively preci
pitated by reaction with triethylamine hydrochloride, The silicon is r
ecovered as silicon dioxide through stepwise combustion of the dried p
recipitate, Fluorination of the product for isotopic analysis is accom
plished by laser heating under pure fluorine generated by the decompos
ition of a fluorine-based salt, The resulting silicon tetrafluoride is
separated from hydrogen fluoride and other fluorination byproducts cr
yogenically using a variable-temperature cold trap, Yields for silicon
recovery are 99.9% for precipitation and greater than 95% for the pur
ification/fluorination procedure. Reproducibility of the isotopic comp
osition for pure quartz granules processed through the procedure is +/
-0.1 parts per thousand for delta(30)Si.