Hostname: page-component-586b7cd67f-rdxmf Total loading time: 0 Render date: 2024-11-24T10:55:11.289Z Has data issue: false hasContentIssue false
  • English
  • Français

Influence of Mn(III) availability on the phase transformation from layered buserite to tunnel-structured todorokite

Published online by Cambridge University Press:  01 January 2024

Haojie Cui ,
Xiangwen Liu ,
Wenfeng Tan ,
Xionghan Feng ,
Fan Liu  and
Huada Daniel Ruan
Haojie Cui
Affiliation:
Key Laboratory of Subtropical Agricultural Resources and Environment, Ministry of Agriculture, Huazhong Agricultural University, Wuhan 430070, People's, Republic of China
Xiangwen Liu
Affiliation:
China University of Geosciences, Wuhan 430074, People's, Republic of China
Wenfeng Tan
Affiliation:
Key Laboratory of Subtropical Agricultural Resources and Environment, Ministry of Agriculture, Huazhong Agricultural University, Wuhan 430070, People's, Republic of China
Xionghan Feng*
Affiliation:
Key Laboratory of Subtropical Agricultural Resources and Environment, Ministry of Agriculture, Huazhong Agricultural University, Wuhan 430070, People's, Republic of China
Fan Liu
Affiliation:
Key Laboratory of Subtropical Agricultural Resources and Environment, Ministry of Agriculture, Huazhong Agricultural University, Wuhan 430070, People's, Republic of China
Huada Daniel Ruan
Affiliation:
Environmental Science Program, Division of Science and Technology, United International College, Beijing Normal University-Hong Kong Baptist University, Zhuhai 519085, People's, Republic of China
*
* E-mail address of corresponding author: [email protected]
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Todorokite is a common Mn oxide mineral in terrestrial and ocean-floor environments, and it is commonly synthesized from layered Na-buserite. Pyrophosphate, which is known to form strong complexes with Mn(III) at a pH range of 1–8, was added to a suspension of Na-buserite in order to sequester the available Mn(III) in Na-buserite. No Mn(III)-pyrophosphate complex was formed in solution at pH 10, and the treated Na-buserites were converted completely to todorokite. Significant transformation reductions were observed when Na-buserite was treated with pyrophosphate solution at pH 7. The presence of Mn(III) within the MnO6 octahedral sheets of Na-buserite is critical for the transformation from layered buserite to tunnel-structured todorokite at atmospheric pressure. At lower pH, two effects are combined to reduce the amount of Mn(III) in the layers: (1) the complexing power of pyrophosphate is increased; and (2) the transformation from Na-buserite to H-birnessite, which is concomitant with the migration of Mn(III) from layers to the interlayer, and the partial disproportionation of Mn(III). The results showed that Mn(III) played a key role in the transformation of layered Na-buserite to tunnel-structured todorokite at atmospheric pressure.

Keywords

BuseriteMn OxideTodorokiteTransformationRefluxing
Type
Article
Information
Clays and Clay Minerals , Volume 56 , Issue 4 , August 2008 , pp. 397 - 403
Copyright
Copyright © 2008, The Clay Minerals Society

References

Al-Sagheer, F.A. and Zaki, M.L., 2004 Synthesis and surface characterization of todorokite-type microporous manganese oxides: implications for shape-selective oxidation catalysts Microporous and Mesoporous Materials> 67 43–52 10.1016/j.micromeso.2003.10.005.CrossRefGoogle Scholar
Bodeï, S. Manceau, A. Geoffroy, N. Baronnet, A. and Buatier, M., 2007 Formation of todorokite from vernadite in Ni-rich hemipelagic sediments Geochimica et Cosmochimica Acta> 71 5698–5716 10.1016/j.gca.2007.07.020.CrossRefGoogle Scholar
Cui, H.J. Feng, X.H. Liu, F. Tan, W.F. and He, J.Z., 2005 Factors governing formation of todorokite at atmospheric pressure Science in China Series D> 48 1678–1689 10.1360/01YD0550.CrossRefGoogle Scholar
Cui, H.J. Feng, X.H. He, J.Z. Tan, W.F. and Liu, F., 2006 Effects of reaction conditions on the formation of todorokite at atmospheric pressure Clays and Clay Minerals> 54 605–615 10.1346/CCMN.2006.0540507.CrossRefGoogle Scholar
Drits, V.A. Silvester, E. Gorshkov, A.I. and Manceau, A., 1997 Structure of synthetic monoclinic Na-rich birnessite and hexagonal birnessite: I. Results from X-ray diffraction and selected-area electron diffraction American Mineralogist> 82 946–961 10.2138/am-1997-9-1012.CrossRefGoogle Scholar
Feng, X.H. Tan, W.F. Liu, F. Wang, J.B. and Ruan, H.D., 2004 Synthesis of todorokite at atmospheric pressure Chemistry of Materials> 16 4330–4336 10.1021/cm0499545.CrossRefGoogle Scholar
Feng, X.H. Liu, F. Tan, W.F. and Liu, X.W., 2004 Synthesis of birnessite from the oxidation of Mn2+ by O2 in alkali medium: Effects of synthesis conditions Clays and Clay Minerals> 52 240–250 10.1346/CCMN.2004.0520210.CrossRefGoogle Scholar
Golden, D.C. Chen, C.C. and Dixon, J.B., 1986 Synthesis of todorokite Science> 231 717–719 10.1126/science.231.4739.717.CrossRefGoogle ScholarPubMed
Golden, D.C. Chen, C.C. and Dixon, J.B., 1987 Transformation of birnessite to buserite, todorokite, and manganite under mild hydrothermal treatment Clays and Clay Minerals> 35 271–280 10.1346/CCMN.1987.0350404.CrossRefGoogle Scholar
Klewicki, J.K. and Morgan, J.J., 1998 Kinetic behavior of Mn(III) complexes of pyrophosphate, EDTA, and citrate Environmental Science & Technology> 32 2916–2922 10.1021/es980308e.CrossRefGoogle Scholar
Kostka, J.E. Luther, G.W. III and Nealson, K.H., 1995 Chemical and biological reduction of Mn(III)-pyrophosphate complexes: Potential importance of dissolved Mn(III) as an environmental oxidant Geochimica et Cosmochimica Acta> 59 885–894.Google Scholar
Kumagai, N. Komaba, S. Abe, K. and Yashiro, H., 2005 Synthesis of metal-doped todorokite-type MnO2 and its cathode characteristics for rechargeable lithium batteries Journal of Power Sources> 146 310–314 10.1016/j.jpowsour.2005.03.145.CrossRefGoogle Scholar
Lanson, B. Drits, V.A. Silvester, E. and Manceau, A., 2000 Structure of H-exchanged hexagonal birnessite and its mechanism of formation from Na-rich monoclinic buserite at low pH American Mineralogist> 85 826–838 10.2138/am-2000-5-625.CrossRefGoogle Scholar
Lanson, B. Drits, V.A. Feng, Q. and Manceau, A., 2002 Structure of synthetic Na-birnessite: Evidence for a triclinic one-layer unit cell American Mineralogist> 87 1662–1671 10.2138/am-2002-11-1215.CrossRefGoogle Scholar
Lanson, B. Drits, V. Gaillot, A. Silvester, E. Plançon, A. and Manceau, A., 2002 Structure of heavy-metal sorbed birnessite: Part 1. Results from X-ray diffraction American Mineralogist> 87 1631–1645 10.2138/am-2002-11-1213.CrossRefGoogle Scholar
Liu, J. Cai, J. Son, Y. C. Gao, Q. Suib, S.L. and Aindow, M., 2002 Magnesium manganese oxide nanoribbons: Synthesis, characterization, and catalytic application Journal of Physical Chemistry B> 106 9761–9768 10.1021/jp0208586.CrossRefGoogle Scholar
Liu, Z. Kang, L. Ooi, K. Makita, Y. and Feng, Q., 2005 Studies on the formation of todorokite-type manganese oxide with different crystalline birnessites by Mg2+-templating reaction Journal of Colloid and Interface Science> 285 239–246 10.1016/j.jcis.2004.11.021.CrossRefGoogle ScholarPubMed
Luo, J. Zhang, Q. Huang, A. Giraldo, O. and Suib, S.L., 1999 Double-aging method for preparation of stabilized Na-buserite and transformations to todorokites incorporated with various metals Inorganic Chemistry> 38 6106–6113 10.1021/ic980675r.CrossRefGoogle ScholarPubMed
Manceau, A. Lanson, B. and Drits, V., 2002 Structure of heavy metal sorbed birnessite. Part III: Results from powder and polarized extended X-ray absorption fine structure spectroscopy Geochimica et Cosmochimica Acta> 66 2639–2663 10.1016/S0016-7037(02)00869-4.CrossRefGoogle Scholar
Nguyen, M. Quemard, A. Broussy, S. Bernadou, J. and Meunier, B., 2002 Mn(III) pyrophosphate as an efficient tool for studying the mode of action of Isoniazid on the InhA protein of Mycobacterium tuberculosis Antimicrobial Agents and Chemotherapy> 46 2137–2144 10.1128/AAC.46.7.2137-2144.2002.CrossRefGoogle ScholarPubMed
Post, J.E., 1999 Manganese oxide minerals: Crystal structures and economic and environmental significance Proceedings of the National Academy of Sciences of the United States of America> 96 3447–3454 10.1073/pnas.96.7.3447.CrossRefGoogle ScholarPubMed
Post, J.E. Heaney, P.J. and Hanson, J., 2003 Synchrotron X-ray diffraction study of the structure and dehydration behavior of todorokite American Mineralogist> 88 142–150 10.2138/am-2003-0117.CrossRefGoogle Scholar
Shen, Y.F. Zerger, R.P. DeGuzman, R.N. Suib, S.L. McCurdy, L. Potter, D.I. and O’Young, C.L., 1993 Manganese oxide octahedral molecular sieves: Preparation, characterization, and applications Science> 260 511–515 10.1126/science.260.5107.511.CrossRefGoogle ScholarPubMed
Shen, Y.F. Suib, S.L. and O’Young, C.L., 1994 Effects of inorganic cation templates on octahedral molecular sieves of manganese oxide Journal of the American Chemical Society> 116 11020–11029 10.1021/ja00103a018.CrossRefGoogle Scholar
Silvester, E. Manceau, A. and Drits, V.A., 1997 Structure of synthetic monoclinic Na-rich birnessite and hexagonal birnessite: II. Results from chemical studies and EXAFS spectroscopy American Mineralogist> 82 962–978 10.2138/am-1997-9-1013.CrossRefGoogle Scholar
Turner, S. Siegel, M.D. and Buseck, P.R., 1982 Structural features of todorokite intergrowths in manganese nodules Nature> 296 841–842 10.1038/296841a0.CrossRefGoogle Scholar
Webb, S.M. Dick, G.J. Bargar, J.R. and Tebo, B.M., 2005 Evidence for the presence of Mn(III) intermediates in the bacterial oxidation of Mn((II) Proceedings of the National Academy of Sciences of the United States of America> 102 5558–5563 10.1073/pnas.0409119102.CrossRefGoogle ScholarPubMed