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Arsenic cycle

The arsenic (As) cycle is the biogeochemical cycle of natural and anthropogenic exchanges of arsenic with the environment. The cycle is of interest because arsenic is detrimental to human health. The World Health Organization recognizes that inorganic arsenic is extremely toxic for humans and detrimental to aquatic life. Arsenic toxicity can harm nearly every organ system within the human body, as well as causing lung and skin cancer. While treatment for arsenic toxicity is possible, prevention or water treatment tends to be the safest solution.

Reservoirs and fluxes
(FeAsS) and tennantite. The principal problematic mineral-sourced arsenic comes from smelting of ores that contain traces of arsenic. Sedimentary rocks bearing coal and shale may also contain high As. Major fluxes of As from the lithosphere to the atmosphere are volcanic emissions. Major sinks include sedimentation and subduction. As is also present in many industrial and agricultural sources such as herbicides, fertilizers, and pesticides. Some As is emitted from steel and glass production, and forest and grassland burning. Major locations that contribute significantly to As pollution are South Asia, West-central Africa, Western Europe, and Latin America. == Arsenic toxicity ==
Arsenic toxicity
The toxicity of As is well known. File:Arsenopyrite.jpg|Arsenopyrite (AsFeS) is the most abundant As mineral File:Arsenic Poisoning.jpg|Signs of arsenic poisoning include changes in skin pigmentation. This person experienced As poisoning due to contaminated water. == See also ==
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