FATE OF MERCURY IN THE ARCTIC Michael Evan ... - COGCI
FATE OF MERCURY IN THE ARCTIC Michael Evan ... - COGCI
FATE OF MERCURY IN THE ARCTIC Michael Evan ... - COGCI
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F. Roos-Barraclough et al. / The Science of the Total Environment 292 (2002) 129–139<br />
2.1. Determination of a suitable peat analysis<br />
program for Hg analysis using the Leco AMA 254<br />
The Leco AMA 254 is fully compliant with<br />
EPA (1998) method 7473.Samples contained in<br />
nickel sample holders enter a sealed drying and<br />
combustion furnace, where they are dried in a<br />
stream of oxygen before being thermally decomposed.Gases<br />
from the thermally decomposed sample<br />
are swept in the stream of oxygen through a<br />
catalyst furnace at 750 8C, which fully decomposes<br />
the gases and traps NO 2, SO2 and halogens.Mercury<br />
is trapped on a gold amalgamator situated at<br />
the end of the furnace.Waste gases are removed<br />
from the system by the gas stream.The amalgamator<br />
is then heated to 500 8C to release the<br />
mercury, which is measured by atomic absorption<br />
spectrometry.The detection limit of the instrument<br />
is 0.01 ng Hg and the working range is 0.05–600<br />
ng Hg, with repeatability being -1.5%.<br />
The instrument was calibrated using liquid standards<br />
prepared from Merck mercury standard solu-<br />
y1<br />
tion, 1000 mg l .Solutions of concentration 10<br />
y1<br />
and 1000 ng ml were used to dose the instru-<br />
ment.A 10-point calibration was made from 0.00<br />
to 29 ng Hg.The equation used to calculate the<br />
calibration curve is:<br />
1<br />
kŽ NST. s µ AjiŽ NST. ymji∂<br />
8ji n<br />
Where k is the constant of proportionality, NST is<br />
the relative non-absorbable radiation flux, A is the<br />
corrected absorbance and m is the quantity of<br />
mercury in the cell.For the calibration obtained,<br />
slope (k)s42.64"0.62 ng.<br />
To test the effect of increased drying time (and<br />
therefore increased Hg passing through the apparatus<br />
from oxygen supply), blanks were run on<br />
the Leco AMA 254 using drying times of 9 and<br />
500 s (other parameters being kept constant:<br />
decomposition time 150 s, waiting time 45 s).<br />
The validity of the recommended drying time<br />
was also tested w0.7=vol.water (ml)x s.Ten<br />
samples of the in-house peat standard OGS 1878<br />
P were moistened (made up to 95% water,<br />
RH OG18<br />
V) and analysed using the recommend-<br />
2<br />
ed drying time.Ten dry samples were also analysed<br />
using a drying time of 20 s.<br />
131<br />
A suitable decomposition time was established<br />
by measuring Hg in nine samples of OGS 1878 P<br />
at 100, 125, 150 and 175 s decomposition time<br />
(drying and waiting time being constant at 30 and<br />
45 s, respectively).One coal and five plant-derived<br />
certified standard reference materials (SRMs) were<br />
analysed using this program.<br />
2.2. Effects of sample preparation: drying times<br />
and temperatures<br />
Homogenisation of the sample is difficult if the<br />
peat is wet but can easily be carried out by hand<br />
using dry peat.However, drying peat, particularly<br />
samples from cold regions, could results in a loss<br />
of Hg by volatilisation.For this reason, tests of<br />
the effect of air-drying peat at room temperature<br />
on Hg content were carried out.The Hg profile of<br />
an Arctic peat core was measured twice; once<br />
using samples which had been kept frozen since<br />
collection and once using samples which had been<br />
air-dried overnight in a class 100 clean-air cabinet.<br />
All samples were measured in duplicate using the<br />
Leco AMA 254 program recommended here.Bulk<br />
density was determined for each sample as<br />
described below and from this, the volumetric<br />
y3<br />
concentrations (ng cm ) were calculated.<br />
To investigate the effect of prolonged drying at<br />
high temperatures and the effect of fertilisation<br />
upon Hg losses upon drying, bulk samples of peat<br />
from the ombrotrophic, pre-anthropogenic section<br />
(88–234 cm) of the EGR2A core was homogenised<br />
using a food mixer.The mixture was divided<br />
into five sections of 150 g each.Three sections<br />
were artificially fertilised with NH NO (1 mM),<br />
4 3<br />
Ca (PO ) (1mM), KCO (1 mM), respectively,<br />
3 4 2 2 3<br />
and a fourth was fertilised with a mixture of the<br />
three above additives (1 mM each).The fifth<br />
section was left unfertilised.These sections were<br />
then subsampled into five parts, which were dried<br />
at the following temperatures; RT, 30, 60, 90 and<br />
105 8C for the following times; 0, 19, 24, 48, 120,<br />
168 and 336 h.The drying was carried out in<br />
acid-cleaned, Teflon bowls, each containing 3.5 g<br />
of peat slurry.After drying, the samples were<br />
stored frozen, sealed in air-tight plastic bags until<br />
AAS Hg analysis using the Leco AMA 254.