R. Juvonen et E. Kontas, Comparison of three analytical methods in the determination of gold in sixFinnish gold ores, including a study on sample preparation and sampling, J GEOCHEM E, 65(3), 1999, pp. 219-229
We used samples from six Finnish ore deposits to evaluate the efficiency of
sample pretreatment procedures - crushing, splining and grinding - and to
compare three analytical methods based on the atomic absorption determinati
on of gold following: (1) classical lead fire assay (FA); (2) the aqua regi
a leach (AR) followed by Hg coprecipitation of Au; and (3) the sodium cyani
de (NaCN) leach. Sample size used for the method comparison is 20 g. The Au
deposits and ore types were: Suurikuusikko and Osikonmaki, refractory ores
in which An is associated with arsenopyrite and pyrite; Pampalo and Kutema
jarvi ores with metallic Au and Au tellurides; and Jokisivu and Pahtavaara
ores containing coarse-grained metallic Au. After crushing, the samples wer
e split into three parts, one of which was put aside into storage. Two spli
ts were further divided into two subsamples which were ground to two grades
of fineness (<0.03 and <0.06 mm), The four subsamples thus obtained were a
nalysed for Au using the three analytical methods. Each determination was p
erformed five times on each of the four subsamples, According to t-tests on
the FA results of the two splits, crushing and splitting produced samples
of equal An content in all six cases. Grinding to a finer grain size gave a
significant difference in Au results only for the Pahtavaara ore sample. I
f the FA results are assumed to represent 100% recovery of Au, we obtained
greater than 95% recoveries for all but the Suurikuusikko sample (87% recov
ery) by the AR leach method. We also obtained recoveries of over 95% by the
NaCN leach method for the Pampalo, Kutemajarvi and Pahtavaara samples, whe
reas recoveries for the other three samples varied between 73 to 92%. The A
R leach was also performed on l-g samples and the NaCN leach on 250-g sampl
es. For three of the ore samples, decreasing sample size from 20 g to 1 g d
id not cause a significant difference in the variance of the Au results. In
creasing the sample size from 20 g to 250 g significantly improves the repr
esentativity of only the Pahtavaara sample. For the Kutemajarvi, Pahtavaara
and Jokisivu ores, a sample larger than 250 g is needed in order to obtain
a precision equivalent to that for reference samples. (C) 1999 Elsevier Sc
ience B.V. All rights reserved.