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FATE OF MERCURY IN THE ARCTIC Michael Evan ... - COGCI

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Fate of Mercury in the Arctic 90<br />

The annular denuders are subjected to numerous analytical steps to inspect, clean and coat<br />

them, expose them and afterwards analyse them. The physical principle of these denuders is so<br />

simple, that it should make them ideal for use. However, in practice they are so difficult to employ<br />

that of the measurements for GEM, particulate mercury and RGM; RGM is the one that scientists<br />

working with atmospheric mercury in the Arctic have least confidence in (Schroeder et al., 2003).<br />

Why is this? As shown in Figure 6., page 64, in general, parallel measurements in these<br />

experiments are reproducible within the 15% documented by Landis et al., 2002, except for the first<br />

measured replicate. In Lindberg et al., 2002, Appendix C., manual denuders were compared with<br />

the automated system and 5 of 6 replicates gave excellent results. However, a single outlier is<br />

enough to document the need for continued improvement. Especially since the only proper<br />

validation so far, is to make multiple replicate measurements, as there is at present no standard<br />

method of the calibrating the annular denuders prior to use. This is especially important since only<br />

two denuders are used as accumulators in the REA RGM system. In principle, if these two denuders<br />

cannot measure the same amount of RGM, then they will necessarily produce a measurement<br />

artefact that will result in an erroneous flux measurement. For example if the two denuders in the<br />

first parallel measurement shown in Figure 6., page 64, represented denuders that were hung on the<br />

up and down channel, then this would show as a significant difference in concentration, and thus a<br />

difference in flux. This single observation reinforces the need for a calibration system, especially if<br />

the system is to be deployed for further REA flux measurements.<br />

Figure 7., page 65 confirms that the physical geometry of the denuder sampling train as well as<br />

the fact that the parts are made out of quartz make the sampling train only negligibly exposed to<br />

passive uptake. Thus fulfilling a pre-requisite for using the annular denuders as RGM REA<br />

accumulators. With the passive uptake rate found for the observed total concentration, this means<br />

that over a typical 4 hour REA sampling period that the RGM due to passive uptake does not

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