[Comparison of air/soil mercury exchange between warm and cold season in Hongfeng Reservoir region].
In July 2002 and March 2003, the mercury exchange flux between soil and air was measured using dynamic flux chamber method in Hongfeng Reservoir region. Mercury exchange flux is (27.4 +/- 40.1) ng x (m2 x h)(-1) (n = 255) and (5.6 +/- 19.4) ng x (m2 x h)(-1) (n = 192) in summer and winter respectively. The correlation coefficient between mercury flux and solar radiation, air temperature, soil temperature is 0.74, 0.83 and 0.80 in summer, and 0.88, 0.56 and 0.59 in winter. From the data, it was found that the mercury emission is stronger in summer than that in winter, and compared to winter, mercury exchange between soil and air depends more on meteorological conditions in summer.
Wang
Shao-feng
SF
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China. shf.wang@mail.gyig.ac.nc
Feng
Xin-bin
XB
Qiu
Guang-le
GL
Fu
Xue-wu
XW
D000388:Air / Q000032:analysis*; D000393:Air Pollutants / Q000032:analysis*; D002681:China; D008628:Mercury / Q000032:analysis*; D008685:Meteorological Concepts; D012621:Seasons; D012987:Soil / Q000032:analysis*; D012989:Soil Pollutants / Q000032:analysis*
D000393:Air Pollutants; D012987:Soil; D012989:Soil Pollutants; D008628:Mercury