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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.

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