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Arsenic and Old Lakes. / ppb. / ppb. / ppb. / ppb. / ppb. > 200 ppb. USEPA/WHO = 10 ppb. RISK = One in a million probability of death. As. As (V). As (III). Jeromite As(S, Se) 2. Plutonic Relationship. 100 ppb. Sinagua Peoples. Ground water arsenic
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Arsenic and Old Lakes
/ ppb / ppb / ppb / ppb / ppb > 200 ppb USEPA/WHO = 10 ppb
As (V) As (III)
100 ppb Sinagua Peoples
Ground water arsenic in the Verde Valley in central Arizona, USA. R.D. Foust Jr., et al Northern Arizona Univ. Applied Geochemistry 19 (2004) 251-255 www.elsevier.com Geology Rules!
Clarkdale mine tailings / ground water trough 210 ppb 400 – 500 ppb
Supai Formation – 280/300 MYA Verde Formation – 5/2 MYA Supai Formation ~ ground level near Sedona
Arsenopyrite FeAsS
40 Fine-grained deposits Big Chino Valley Schwab(1995), USGS 89 Open File Report 2005-1154
Oxidation Rust…………..
Reduction (anaerobic) methane swamp gas
Anoxic Depositional Setting high organic content
Oxidation of Arsenopyrite: 4 FeAsS + 13 O2 + 6 H2O 4FeSO4 + 4H3AsO4 Add Oxygen and water – Lower the water table in an Arsenopyrite-rich aquifer – Arsenic will be mobilized
Microbial processes mediate the release of arsenic into ground water under reducing conditions
Ground Water Arsenic Concentrations INCREASED When landfill covered! Slower ground water velocity allows more time to strip the water of oxygen, resulting in geochemically reducing conditions. In reducing conditions, microbial processes release arsenic.
Arsenic mobilization Geochemical evolution of ground water to high pH, alkaline conditions, can induce transport of arsenic
Ground water flow from limestone (alkaline pH) into arsenic-rich aquifer, will mobilize arsenic.
As (III) Reduction pH Oxidation As (V)
Options: • well construction – • no method to predict • optimal design / depth • treatment dependent • on arsenic species • present – water softener • + Fe-based resin filter • geochemistry rules • test your well water