J. Gaillardet et al., Evaporation and sublimation of boric acid: Application for boron purification from organic rich solutions, GEOSTAND N, 25(1), 2001, pp. 67-75
Citations number
11
Categorie Soggetti
Earth Sciences
Journal title
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS
We report in this paper a series of experiments whose purpose is to test th
e long held idea of boron volatility when neutral to acidic solutions conta
ining traces of boron are evaporated. Boron recoveries have been measured p
recisely by isotopic dilution and boron isotopic ratios have also been dete
rmined. Most of the evaporations have been conducted at 60-65 degreesC. It
was found that no loss of boric acid occurs when c. 1 mug of B is evaporate
d in water, HCl, HF and acetone solutions. At the same time, we did not obs
erve any associated B isotopic fractionation. In contrast to previous studi
es on B volatilisation, it was not found necessary to use mannitol to preve
nt B losses during the evaporation of acidic solutions. Important losses of
boron were observed from solutions of methanol, ethanol and organic-rich n
atural solutions. In the presence of methanol and ethanol, a volatile methy
l (or ethyl) borate is likely to be formed. In contrast to these studies, w
e show that boron is highly volatile when the dried residues of an evaporat
ion are heated further. The sublimation of boron that then occurs can be mo
derated by the use of mannitol, but a slight increase of the temperature al
lows B volatilisation. Despite the substantial losses of B by sublimation,
no B isotopic fractionation was observed at 60-65 degreesC. The property of
boron to sublime was used to separate B from on organic matrix. A miniatur
ized sublimation apparatus, comprising a 5 ml Teflon beaker, and the associ
ated "microsublimation" technique are described. The 100% boron recovery an
d the absence of B isotopic fractionation make this method suitable for ext
racting B from organic-rich samples.