Mercury is an element emitted globally from both natural and man-made sources. As an element,
mercury cannot be created or destroyed. There are three primary forms of mercury found in the
environment: (1) elemental (quicksilver); (2) divalent (oxidized or “reactive” mercury); and (3)
organic (methylmercury). Elemental mercury is stable and can remain in the atmosphere between
six months and two years, during which time it can be globally distributed. In the atmosphere,
elemental mercury can be converted to the divalent form that can attach to solid particles
(“particle-bound” mercury, subject to dry and wet deposition) or aqueous droplets (subject to wet
deposition) and can be deposited on the ground and the surface of water bodies. Once divalent
mercury enters a water body, it can undergo chemical conversion to methylmercury, which is
retained in fish tissue and is the only form of mercury that accumulates in aquatic food webs.
Fish consumption is the primary source of methylmercury exposure in humans.
Human activity since the Industrial Revolution has increased the amount of mercury present
globally in the atmosphere. About half of global mercury emissions are natural—from oceans,
erosion, vegetation, vegetation burning, and volcanoes—while slightly less than half of mercury
emissions are the result of man-made sources. About three percent of total global mercury emissions originate from man-made sources in the U.S., with approximately one percent of the
global total from U.S. power plants. Asia contributes about half of the global emissions of mercury from man-made sources, while the U.S. contributes about six percent of emissions from
man-made sources.
This from the most worthless state agency ever. The TECQ.
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Member:
Steven F Austin's Old 300
Sons of Confederate Veterans
Sons of The Republic of Texas