Uranium is a ubiquitous trace component in rocks ranging from 1.2 to 1.3 µg g-1 in sedimentary rocks, 2.2 to 15 µg g-1 in granites, and 20 to 120 µg g-1 in phosphates (Langmuir, 1997; Plant et al., 1999). Uranium (U) is released to natural waters in dilute concentrations (generally
Revised: May 14, 2015 |
Published: May 16, 2013
Citation
Zachara J.M., E.S. Ilton, and C. Liu. 2013.Reactive Transport of the Uranyl Ion in Soils, Sediments, and Groundwater Systems. In Uranium - Cradle to Grave. Short Course Series, edited by PC Burns and GE Sigmon. 255-299. Quebec, :Mineralogical Association of Canada.PNNL-SA-94443.