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

Title: Zinc surface complexes on birnessite: A density functional theory study

Journal Article · · Geochimica et Cosmochimica Acta

Biogeochemical cycling of zinc is strongly influenced by sorption on birnessite minerals (layer-type MnO2), which are found in diverse terrestrial and aquatic environments. Zinc has been observed to form both tetrahedral (Zn{sup IV}) and octahedral (Zn{sup VI}) triple-corner-sharing surface complexes (TCS) at Mn(IV) vacancy sites in hexagonal birnessite. The octahedral complex is expected to be similar to that of Zn in the Mn oxide mineral, chalcophanite (ZnMn{sub 3}O{sub 7} {center_dot} 3H{sub 2}O), but the reason for the occurrence of the four-coordinate Zn surface species remains unclear. We address this issue computationally using spin-polarized Density Functional Theory (DFT) to examine the Zn{sub IV}-TCS and Zn{sup VI}-TCS species. Structural parameters obtained by DFT geometry optimization were in excellent agreement with available experimental data on Zn-birnessites. Total energy, magnetic moments, and electron-overlap populations obtained by DFT for isolated Zn{sup IV}-TCS revealed that this species is stable in birnessite without a need for Mn(III) substitution in the octahedral sheet and that it is more effective in reducing undersaturation of surface O at a Mn vacancy than is Zn{sub VI}-TCS. Comparison between geometry-optimized ZnMn{sub 3}O{sub 7} {center_dot} 3H{sub 2}O (chalcophanite) and the hypothetical monohydrate mineral, ZnMn{sub 3}O{sub 7} {center_dot} H{sub 2}O, which contains only tetrahedral Zn, showed that the hydration state of Zn significantly affects birnessite structural stability. Finally, our study also revealed that, relative to their positions in an ideal vacancy-free MnO{sub 2}, Mn nearest to Zn in a TCS surface complex move toward the vacancy by 0.08-0.11 {angstrom}, while surface O bordering the vacancy move away from it by 0.16-0.21 {angstrom}, in agreement with recent X-ray absorption spectroscopic analyses.

Research Organization:
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
Earth Sciences Division
DOE Contract Number:
DE-AC02-05CH11231
OSTI ID:
948576
Report Number(s):
LBNL-1553E; GCACAK; TRN: US200907%%118
Journal Information:
Geochimica et Cosmochimica Acta, Vol. 73; Related Information: Journal Publication Date: 2009; ISSN 0016-7037
Country of Publication:
United States
Language:
English

Similar Records

Surface complexation of Pb(II) by hexagonal birnessite nanoparticles
Journal Article · Fri Oct 15 00:00:00 EDT 2010 · Geochimica et Cosmochica Acta · OSTI ID:948576

Changes in Zinc Speciation with Mine Tailings Acidification in a Semiarid Weathering Environment
Journal Article · Tue Oct 09 00:00:00 EDT 2012 · Environ. Sci. Technol. · OSTI ID:948576

Water in the Interlayer Region of Birnessite: Importance in Cation Exchange and Structural Stability
Journal Article · Sun Jan 01 00:00:00 EST 2006 · American Mineralogist · OSTI ID:948576