- Art Gallery - |
Bilinite (Fe2+Fe23+(SO4)·22H2O) is an iron sulfate mineral. It is a product of the oxidation of pyrite in water. It is an acidic mineral that has a pH of less than 3 and is harmful to the environment when it comes from acid rock drainage (Keith et. al., 2001). Bilinite was first discovered near Bilina, Czech Republic which is why the mineral was named 'bilinite' (Palache, et al., 1969). This mineral possibly occurs on Mars. Composition The weight percent oxide is as follows:[1]
Related minerals Related minerals to bilinite include jarosite, which is an iron sulfate salt, lepidocrocite, schwetmannite, ferricopiapite, and copiapite (Marion, et. al., 2008). Special characteristics Boulder Creek is a stream at Iron Mountain in Shasta County, California. The stream drains into the Sacramento River and San Francisco Bay. The water in this stream is contaminated from the mixture of the groundwater and surface streams due to mining. The pH is low and acidic due to the oxidation of pyrite in water. This results in the formation of sulfuric acid and bilinite (Keith, et al., 2001). References 1. ^ a b http://rruff.geo.arizona.edu/doclib/hom/bilinite.pdf Handbook of Mineralogy * Keith, David C., Runnells, Donald D., Esposito, Kenneth J., Chermak, John A., Levy, David B., Haaula, Steven R., Watts, Malcolm, Hall, Larry. (2001) Geochemical models of the impact of acidic groundwater and evaporative sulfate salts on Boulder Creek at Iron Mountain, California. Applied Geochemistry 16, 947-961. Retrieved from "http://en.wikipedia.org/"
|
|