Diffusion of H, C, and O Components in Silicate Melts

Research Article| January 01, 2010 Diffusion of H, C, and O Components in Silicate Melts Youxue Zhang; Youxue Zhang Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109-1005, U.S.A., youxue@umich.edu Search for other works by this author on: GSW Google Scholar Huaiwei Ni Huaiwei Ni Bayerisches Geoinstitut, University of Bayreuth, D-95440 Bayreuth, Germany Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2010) 72 (1): 171–225. https://doi.org/10.2138/rmg.2010.72.5 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Youxue Zhang, Huaiwei Ni; Diffusion of H, C, and O Components in Silicate Melts. Reviews in Mineralogy and Geochemistry 2010;; 72 (1): 171–225. doi: https://doi.org/10.2138/rmg.2010.72.5 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Silicate melts are complicated in structure and composition. Hence, diffusion in a melt (in this chapter, a melt includes both liquid and glass) can be very complicated due to the presence of many components, each of which can be present in different species, as well as various kinds of diffusion, such as self-diffusion, tracer diffusion, interdiffusion, effective binary diffusion and multi-component diffusion. In this chapter, the diffusion of H, C and O components is reviewed. H may be in the form of H2O molecules (hereafter referred to as H2Om), OH groups (hereafter referred to... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.