Hostname: page-component-cd9895bd7-gvvz8 Total loading time: 0 Render date: 2024-12-26T04:35:11.005Z Has data issue: false hasContentIssue false
  • English
  • Français

How kaolinite plays an essential role in remediating oil-polluted seawater

Published online by Cambridge University Press:  09 July 2018

S. K. Chaerun  and
K. Tazaki
S. K. Chaerun*
Affiliation:
Indonesia Agrogeology Development Center, Jenderal Soedirman University, Jl. Dr. Bunjamin No. 708, Grendeng, Purwokerto 53122, Central Java, Indonesia Graduate School of Natural Science and Technology, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan
K. Tazaki
Affiliation:
Department of Earth Sciences, Faculty of Science, Kanazawa University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan
*
E-mail: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

An investigation was carried out on the bioavailability of kaolinite and the role it plays in remediating oil-polluted seawater, since kaolinite is known to enable hydrocarbon-degrading bacteria to grow well. Experimental results revealed that significant amounts of Al and Si dissolved from kaolinite were not observed ((P > 0.05) in comparison with a control sample which contained no kaolinite) in the aqueous phase during the ~24 day experimental period. Transmission electron microscope observations and energy-dispersive spectroscope data revealed that some altered kaolinite particles appeared, connected to intact kaolinite and bacterial cells. Bacterial cells were associated and encrusted with intact and/or altered kaolinite clay particles, where mixed (C, O, Na and Si)-precipitates of kaolinite clays were formed on the surface of hydrocarbon-degrading bacterial cells. However, the uptake of Si (from kaolinite) by bacterial cells appeared to be more prevalent than Al, and there were no significant changes in basal spacings of kaolinite due to these altered kaolinite particles. Separate studies showed that hydrocarbon-degrading bacteria have a high resistance to Si. Thus, the present data suggest that Si from kaolinite may facilitate hydrocarbon-degrading bacterial growth as shown in our previous study (Chaerun et al., 2005), and the C-O-Na-Si complexes on the surfaces of bacterial cell walls may be the stimulator for hydrocarbon-degrading bacterial growth in seawater contaminated with oil spill.

Keywords

kaoliniteC-O-Na-Si complexesoil spillmarine environmenthydrocarbon-degrading bacteriaTEM-EDS
Type
Research Article
Information
Clay Minerals , Volume 40 , Issue 4 , December 2005 , pp. 481 - 491
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2005

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Asada, R. & Tazaki, K. (2001) Silica biomineralization of unicellular microbes under strongly acidic conditions. The Canadian Mineralogist, 39, 1–16.Google Scholar
Asada, R., Okuno, M. & Tazaki, K. (2002) Structural anisotropy of biogenic silica in pinnate diatoms under Fourier transform polarized infrared microspectroscopy. Journal of Mineralogical and Petrological Sciences, 97, 219–226.Google Scholar
Chaerun, S.K., Tazaki, K., Asada, R. & Kogure, K. (2004a) Bioremediation of coastal areas 5 years after the Nakhodka oil spill in the Sea of Japan: isolation and characterization of hydrocarbon-degrading bacteria. Environment International, 30, 911–922.CrossRefGoogle ScholarPubMed
Chaerun, S.K., Tazaki, K., Asada, R. & Kogure, K. (2004b) Alkane-degrading bacteria and heavy metals from the Nakhodka oil spill-polluted seashores in the Sea of Japan after five years of bioremediation. The Science Reports of Kanazawa University, 49, 25–46.Google Scholar
Chaerun, S.K., Tazaki, K., Asada, R. & Kogure, K. (2005) Interaction between clay minerals and hydrocarbon-utilizing indigenous microorganisms in high concentration of heavy oil: Implications for bioremediation. Clay Minerals, 40, 105–114.Google Scholar
Coale, K.H., Johnson, K.S., Chavez, F.P., Buesseler, K.O., Barber, R.T., Brzezinski, M.A., plus 42 others (2004) Southern ocean iron enrichment experiment: carbon cycling in high- and low-Si waters. Science, 304, 408–414.Google Scholar
Coles, C.A. & Yong, R.N. (2002) Aspects of kaolinite characterization and retention of Pb and Cd. Applied Clay Science, 22, 39–45.CrossRefGoogle Scholar
Cook, T.L. & Stakes, D.S. (1995) Biogeological mineralization in deep-sea hydrothermal deposits. Science, 267, 1975–1979.CrossRefGoogle ScholarPubMed
Ferris, F.G., Beveridge, T.J. & Fyfe, W.S. (1986) Iron- silica crystallite nucleation by bacteria in a geothermal sediment. Nature, 320, 609–611.Google Scholar
Fialips, C.I. (2003) Kaolinite properties and conditions of formation or transformation. Newsletter of the Mineralogical Association of Canada, 71, 12–14.Google Scholar
Ichikuni, M. (1970) Incorporation of aluminium and iron into siliceous sinters. Chemical Geology, 6, 273–276.Google Scholar
Inagaki, F., Motomura, Y. & Ogata, S. (2003) Microbial silica deposition in geothermal hot waters. Applied Microbiology and Biotechnology, 60, 605–611.Google Scholar
Kastner, M. (1981) Authigenic silicates in deep-sea sediments: formation and diagenesis. Pp. 915–980 in: The Sea: The Oceanic Lithosphere (Emiliani, C., editor). Wiley, New York, USA.Google Scholar
Konhauser, K.O. & Ferris, F.G. (1996) Diversity of iron and silica precipitation by microbial mats in hydrothermal waters, Iceland: implications for Precambrian iron formations. Geology, 24, 323–326.Google Scholar
Kostka, J.E., Haefele, E., Viehweger, R. & Stucki, J.W. (1999) Respiration and dissolution of Fe(III)-containing clay minerals by bacteria. Environmental Science and Technology, 33, 3127–3133.Google Scholar
Kostka, J.E., Dalton, D.D., Skelton, H., Dollhopf, S. & Stucki, J.W. (2002) Growth of iron(III)-reducing bacteria on clay minerals as the sole electron acceptor and comparison of growth yields on a variety of oxidized iron forms. Applied and Environmental Microbiology, 68, 6256–6262.CrossRefGoogle ScholarPubMed
Little, B.J., Wagner, P.A. & Lewandowski, Z. (1997) Spatial relationships between bacteria and mineral surfaces. Pp. 123–159 in: Geomicrobiology: Interactions between Microbes and Minerals (Banfield, J.F. and, K.H. Nealson, , editors). Reviews in Mineralogy, 35. Mineralogical Society of America, Washington, D.C.Google Scholar
Maurice, P.A., Lee, Y.J. & Hersman, L.E. (2000) Dissolution of Al-substitute goethites by an aerobic Pseudomonas mendocina var. bacteria. Geochimica et Cosmochimica Acta, 64, 1363–1374.Google Scholar
Moat, A.G. & Foster, J.W. (1988) Microbial Physiology. John Wiley & Sons, Inc., New York, USA, pp. 86–92.Google Scholar
Shelobolina, E.S., Anderson, R.T., Vodyanitskii, Y.N., Sivtsov, A.V., Yuretich, R. & Lovley, D.R. (2004) Importance of clay size minerals for Fe (III) respiration in a petroleum-contaminated aquifer. Geobiology, 2, 67–76.Google Scholar
Shuler, M.L. & Kargi, F. (1992) Bioprocess Engineering Basic Concepts, pp. 10–57. Prentice Hall International, New Jersey, USA.Google Scholar
Urrutia, M.M. & Beveridge, T.J. (1994) Formation of fine-grained metal and silicate precipitations on a bacterial surface (Bacillus subtilis). Chemical Geology, 116, 261–280.CrossRefGoogle Scholar