Stoner J C, Whanger P D, Weswig P H
Environ Health Perspect. 1977 Aug;19:139-43. doi: 10.1289/ehp.7719139.
The arsenic content of well water in certain areas of Oregon can range up to 30 to 40 times the U.S.P.H.S. Drinking Water Standard of 1962, where concentrations in excess of 50 ppb are grounds for rejection. The elevated arsenic levels in water are postulated to be due to volcanic deposits. Wells in central Lane County, Oregon, that are known to contain arsenic rich water are in an area underlain by a particular group of sedimentary and volcanic rocks, which geologists have named the Fischer formation. The arsenic levels in water from wells ranged from no detectable amounts to 2,000 ppb. In general the deeper wells contained higher arsenic water. The high arsenic waters are characterized by the small amounts of calcium and magnesium in relation to that of sodium, a high content of boron, and a high pH. Water from some hot springs in other areas of Oregon was found to range as high as 900 ppb arsenic. Arsenic blood levels ranged from 32 ppb for people living in areas where water is low in arsenic to 250 ppb for those living in areas where water is known to contain high levels of arsenic. Some health problems associated with consumption of arsenic-rich water are discussed.
俄勒冈州某些地区的井水砷含量可能高达1962年美国公共卫生署饮用水标准的30至40倍,该标准规定超过50 ppb的浓度就不符合要求。水中砷含量升高据推测是由于火山沉积物所致。俄勒冈州莱恩县中部已知含有富含砷水的水井位于一个特定的沉积岩和火山岩群之下,地质学家将其命名为费舍尔地层。井水的砷含量从检测不到到2000 ppb不等。一般来说,较深的水井含有砷含量更高的水。高砷水的特点是钙和镁的含量相对于钠较少、硼含量高且pH值高。在俄勒冈州其他地区,一些温泉水的砷含量高达900 ppb。砷的血液含量范围从生活在砷含量低的地区的人的32 ppb到生活在已知水砷含量高的地区的人的250 ppb。文中讨论了一些与饮用富含砷的水相关的健康问题。