Mc. Stordal et Ga. Gill, DETERMINATION OF MERCURY METHYLATION RATES USING A 203-HG RADIOTRACERTECHNIQUE, Water, air and soil pollution, 80(1-4), 1995, pp. 725-734
A radiotracer method for the determination of mercury (Hg) methylation
rates in bulk water and water overlying intact sediment cores has bee
n developed. A sediment core with overlying water is collected in a co
re tube, the overlying water is spiked with high specific activity 203
-Hg radiotracer, and the core is incubated at ambient temperature. Ali
quots of the overlying water are removed, the Hg is extracted from the
sample, and the activity in the extract is measured. A 10-25 fold sam
ple preconcentration is achieved using a dithizone-chloroform extracti
on technique and a sodium nitrite back extraction step to separate ino
rganic Hg(II) from monomethylmercury (MMHg). The use of this technique
, in conjunction with high specific activity 203-Hg and has allowed fo
r spiking concentrations in the overlying water of approximately 1 ng
Hg/L. This spiking level is about the same concentration as the ambien
t water overlying the core, thus not significantly perturbing the syst
em. Our technique is a significant improvement over previous methodolo
gies which used 203-Hg spike additions of 1 mu g Hg/L or higher. The t
echnique was used to measure Hg methylation rates at the Experimental
Lakes Area (ELA) in Ontario, Canada during August of 1983 and at an ex
tensively studied estuarine site in Gulf Breeze, Florida, USA during S
eptember, 1993 and June, 1994. Multiple cores were collected and spike
d with a range of 1 to 11,800 ng Hg (as 203-Hg) into the overlying wat
er. MMHg production at the ELA site indicated rates of 0.25 to 3.7 pg/
cm(2)/day (0.08 to 2.5% methylation/day). Results from Gulf Breeze wer
e significantly higher at 1.5 to 425 pg/cm(2)/day or 0.06 to 18% methy
lation/day. These rates are one to three orders of magnitude greater t
han previously measured ''specific rates'' in bulk water samples and s
ediments. A direct comparison of rates with previous sediment methylat
ion assay techniques is not possible, however, because of the signific
ant differences between our methodology and previous assay protocols.