skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: X-ray absorption spectroscopy of Co(II) sorption complexes on quartz ({alpha}-SiO{sub 2}) and rutile (TiO{sub 2})

Journal Article · · Geochimica et Cosmochimica Acta
 [1];  [2]; ; ;  [3]
  1. Arizona State Univ., Tempe, AZ (United States)
  2. Virginia Inst. of Marine Science, Gloucester Point, VA (United States)
  3. Stanford Univ., CA (United States)

The local molecular structure of Co(II) surface complexes sorbed to two pure mineral substrates, quartz ({alpha}-SiO{sub 2}) and rutile (TiO{sub 2}), was examined with X-ray absorption spectroscopy (XAS) are extended X-ray absorption fine structure (EXAFS) analysis. Absorption spectra were collected for samples equilibrated with Co solutions under- and over-saturated with respect to solid Co-hydroxide phases (0.15-3.00 mM) at Co surface coverages of 0.63-9.51 {mu}mol m{sup {minus}2} and for equilibration times of 23 h to 21 days. Quantitative analysis of the EXAFS spectra indicates no significant structural differences in the local atomic environment around Co sorbed to quartz, regardless of the surface coverage or the equilibration time. For all Co/quartz samples, the local Co environment is similar (but not identical) to that of Co in solid, crystalline cobalt hydroxide (Co(OH){sub 2}(s)). Cobalt is octahedrally coordinated by six O atoms at 2.06-2.11 {Angstrom}; second-neighbor Co backscatterers are found at 3.11-3.12 {Angstrom}, slightly contracted relative to the Co-Co distance in Co (OH){sub 2}(s) (3.173 {Angstrom}). Analysis of these high coverage Co/rutile samples indicates Ti backscatterers at distances near those expected for anatase, a TiO{sub 2} polymorph, suggesting a local geometry for Co and Ti octahedra at the rutile/water interface similar to that of the cation octahedra in anatase. We suggest that differences in Co sorption on quartz and rutile may be attributed to the availability of reactive surface sites on quartz and rutile which are structurally favorable for the sorption of octahedrally-coordinated Co{sup 2+}. 102 refs., 7 figs.

OSTI ID:
457469
Journal Information:
Geochimica et Cosmochimica Acta, Vol. 60, Issue 14; Other Information: PBD: Jul 1996
Country of Publication:
United States
Language:
English

Similar Records

X-ray absorption spectroscopy of cobalt(II) multinuclear surface complexes and surface precipitates on kaolinite
Journal Article · Fri Jul 01 00:00:00 EDT 1994 · Journal of Colloid and Interface Science; (United States) · OSTI ID:457469

Reaction sequence of nickel(II) with kaolinite: Mineral dissolution and surface complexation and precipitation
Journal Article · Tue Sep 01 00:00:00 EDT 1998 · Soil Science Society of America Journal · OSTI ID:457469

Evidence for the formation of trioctahedral clay upon sorption of Co{sup 2+} on quartz
Journal Article · Wed Dec 15 00:00:00 EST 1999 · Journal of Colloid and Interface Science · OSTI ID:457469