A near edge X-ray absorption fine structure (NEXAFS) study of the response mechanism of the iron (III) chalcogenide glass membrane ion-selective electrode
Access Status
Fulltext not available
Authors
Maric, Mark
Sohail, M.
De Marco, Roland
Date
2014Type
Journal Article
Metadata
Show full item recordCitation
Maric, Mark and Sohail, Manzar and De Marco, Roland. 2014. A near edge X-ray absorption fine structure (NEXAFS) study of the response mechanism of the iron (III) chalcogenide glass membrane ion-selective electrode. Electrochemistry Communications. 41: pp. 27-30.
Source Title
Electrochemistry Communications
ISSN
Collection
Abstract
We have utilized synchrotron radiation-X-ray photoelectron spectroscopy (SR-XPS) and near edge X-ray absorption fine structure (NEXAFS) to demonstrate unequivocally that the modified surface layer (MSL) of the iron chalcogenide glass ion-selective electrode (ISE) comprises a mixture of iron(II) and iron(III) redox states, as proposed in previous theories to explain the mixed electron transfer and ion exchange response mechanism of this analytically important ISE.
Related items
Showing items related by title, author, creator and subject.
-
Bekker, A.; Planavsky, N.; Rasmussen, Birger; Krapez, Bryan; Hofmann, A.; Slack, J.; Rouxel, O.; Konhauser, K. (2014)Iron formations are economically significant, iron- and silica-rich sedimentary rocks that are restricted to Precambrian successions. There are no known modern or Phanerozoic analogues for these deposits that are comparable ...
-
Holman, R.; Olynyk, John; Kulkarni, H.; Ferrari, P. (2017)Background: Parenteral iron is integral in the treatment of anaemia of chronic kidney disease patients on haemodialysis (HD). However, increased liver iron concentration (LIC) can result from such treatment, and this ...
-
Rasmussen, Birger; Fletcher, Ian; Bekker, Andrey; Muhling, Janet; Gregory, Courtney; Thorne, Alan (2012)Iron formations are chemical sedimentary rocks comprising layers of iron-rich and silica-rich minerals whose deposition requires anoxic and iron-rich (ferruginous) sea water. Their demise after the rise in atmospheric ...