Other| February 01, 1998 Aqueous Pb sorption by hydroxylapatite; applications of atomic force microscopy to dissolution, nucleation, and growth studies Steven K. Lower; Steven K. Lower Kent State University, Department of Geology, Kent, OH, United States Search for other works by this author on: GSW Google Scholar Patricia A. Maurice; Patricia A. Maurice Search for other works by this author on: GSW Google Scholar Samuel J. Traina; Samuel J. Traina Search for other works by this author on: GSW Google Scholar Ernest H. Carlson Ernest H. Carlson Search for other works by this author on: GSW Google Scholar Author and Article Information Steven K. Lower Kent State University, Department of Geology, Kent, OH, United States Patricia A. Maurice Samuel J. Traina Ernest H. Carlson Publisher: Mineralogical Society of America First Online: 02 Mar 2017 Online Issn: 1945-3027 Print Issn: 0003-004X GeoRef, Copyright 2004, American Geological Institute. American Mineralogist (1998) 83 (1-2): 147–158. https://doi.org/10.2138/am-1998-1-215 Article history First Online: 02 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 Steven K. Lower, Patricia A. Maurice, Samuel J. Traina, Ernest H. Carlson; Aqueous Pb sorption by hydroxylapatite; applications of atomic force microscopy to dissolution, nucleation, and growth studies. American Mineralogist 1998;; 83 (1-2): 147–158. doi: https://doi.org/10.2138/am-1998-1-215 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 SocietyAmerican Mineralogist Search Advanced Search Abstract A combination of atomic force microscopy, scanning election microscopy, transmission electron microscopy, energy dispersive spectroscopy, electron diffraction, and X-ray diffraction were used to study reactions of 0.5-500 mg/L aqueous Pb with Ca 5 (PO 4 ) 3 OH, hydroxylapatite (HAP), at pH 6 and 22 degrees C. Following 2 h reaction time, concentrations of Pb aq ([Pb aq ]) decreased from 500 mg/L to <100 mg/L, and from 0.5-100 mg/L to <15 mu g/L. This loss of Pb aq from solution (i.e., sorption) resulted partially from simultaneous dissolution of HAP and precipitation of Pb 5 (PO 4 ) 3 OH, hydroxypyromorphite (HPY), or another solid Pb phase. The initial saturation state with respect to HPY (defined as the ratio of the ion activity product to equilibrium solubility product) influenced strongly precipitation processes. At a high degree of saturation (initial [Pb aq ]>100 mg/L), small nuclei or aggregates of poorly crystalline HPY precipitated homogeneously in solution. At intermediate saturation (initial [Pb aq ] approximately 10-100 mg/L), large, euhedral needles of HPY precipitated homogeneously in solution. At a low degree of saturation (initial [Pb aq ]<10 mg/L), a needle-like Pb-containing phase grew heterogeneously on HAP. These results agree well with concepts derived from nucleation and growth theories and demonstrate that initial saturation state influences strongly the sorption process. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.