Mercury flux measurements over air and water in Kejimkujik National Park, Nova Scotia

被引:49
作者
Boudala, FS [1 ]
Folkins, I
Beauchamp, S
Tordon, R
Neima, J
Johnson, B
机构
[1] Dalhousie Univ, Dept Oceanog, Halifax, NS B3H 4J1, Canada
[2] Environm Canada, Atmospher Environm Branch, Div Atmospher Sci, Dartmouth, NS B2Y 2N6, Canada
关键词
mercury; mercury fluxes; solar radiation;
D O I
10.1023/A:1005299411107
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Mercury flux measurements were conducted at two lakes and three soil sites in Kejimhujik National Park, located in the eastern Canadian province of Nova Scotia. One of the lakes had high levels of both mercury and Dissolved Organic Carbon (DOC). Two of the soil sites were located under the forest canopy, while the other was in a small clearing surrounded by forest. Flux measurements were pel formed using the dynamic chamber method. Mercury concentrations in the air were measured with a TEKRAN mercury analyzer. Mercury fluxes over the two lakes were most strongly correlated with solar radiation, although the flux was also significantly correlated with water temperature, air temperature, and negatively correlated with relative humidity. The flux from the high DOC lake (Big Dam West) was especially high when the conditions were both sunny and windy (wind speed greater than 1.3 m s(-1)) and the average flux measured was 5.4 ng m(-2) h(-1). The mercury Aux from this lake was well parameterized in terms of a simple expression involving solar radiation and a nonlinear dependence on wind speed. The flux measured from the low DOC lake (North Cranberry) tended to be lower than from the high DOC lake. The average flux measured was 1.1 ng m(-2) h(-1), but was again strongly correlated with solar radiation. The flux was low during windy conditions in the absence of sunlight, suggesting that wind enhances mercury evasion from lakes only in the presence of solar radiation. Mercury fluxes measured over the soil sites tended to be smaller than those over water (a range of -1.4-4.3 ng m(-2) h(-1)). At one of the forest sites, mercury flux was very strongly correlated with 0.5 cm soil temperature, and this dependence was well described by an Arrhenius-type expression with an activation energy of 14.6 kcal(-1) mole, quite close to the heat of vaporization of mercury (14.5 kcal(-1) mol(-1) at 20 degrees C). At the clearing, where there was direct exposure to the sun, the mercury flux was most strongly correlated with solar radiation.
引用
收藏
页码:183 / 202
页数:20
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