Micro-spectroscopic investigation of selenium-bearing minerals from the Western US Phosphate Resource Area

Amy L Ryser; Daniel G Strawn; Matthew A Marcus; Jodi L Johnson-Maynard; Mickey E Gunter; Gregory Möller

doi:10.1186/1467-4866-6-1

Micro-spectroscopic investigation of selenium-bearing minerals from the Western US Phosphate Resource Area

Geochem Trans. 2005 Jan 28;6(1):1. doi: 10.1186/1467-4866-6-1. eCollection 2005.

Authors

Amy L Ryser¹, Daniel G Strawn¹, Matthew A Marcus², Jodi L Johnson-Maynard¹, Mickey E Gunter¹, Gregory Möller¹

Affiliations

¹ University of Idaho, Moscow, Idaho 83844-2339.
² Lawrence Berkeley National Laboratory, Berkeley, California 94720.

Abstract

Mining activities in the US Western Phosphate Resource Area (WPRA) have released Se into the environment. Selenium has several different oxidation states and species, each having varying degrees of solubility, reactivity, and bioavailability. In this study we are investigating the speciation of Se in mine-waste rocks. Selenium speciation was determined using bulk and micro-x-ray absorption spectroscopy (XAS), as well as micro-x-ray fluorescence mapping. Rocks used for bulk-XAS were ground into fine powders. Shale used for micro-XAS was broken along depositional planes to expose unweathered surfaces. The near edge region of the XAS spectra (XANES) for the bulk rock samples revealed multiple oxidation states, with peaks indicative of Se(-II), Se(IV), and Se(+VI) species. Micro-XANES analysis of the shale indicated that three unique Se-bearing species were present. Using the XANES data together with ab initio fitting of the extended x-ray absorption fine structure region of the micro-XAS data (micro-EXAFS) the three Se-bearing species were identified as dzharkenite, a di-selenide carbon compound, and Se-substituted pyrite. Results from this research will allow for a better understanding of the biogeochemical cycling of Se in the WPRA.