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Interaction between glycine and Na-, Caand Cu-rich smectites

Published online by Cambridge University Press:  09 July 2018

E. Benincasa
Affiliation:
Department of Earth Sciences, University of Modena and Reggio Emilia, Via S. Eufemia 19, I 41100, Modena, Italy
M. F. Brigatti*
Affiliation:
Department of Earth Sciences, University of Modena and Reggio Emilia, Via S. Eufemia 19, I 41100, Modena, Italy
C. Lugli
Affiliation:
Department of Earth Sciences, University of Modena and Reggio Emilia, Via S. Eufemia 19, I 41100, Modena, Italy
L. Medici
Affiliation:
Department of Earth Sciences, University of Modena and Reggio Emilia, Via S. Eufemia 19, I 41100, Modena, Italy
L. Poppi
Affiliation:
Department of Earth Sciences, University of Modena and Reggio Emilia, Via S. Eufemia 19, I 41100, Modena, Italy
*

Abstract

The interactions between glycine and two Na-, Ca- and Cu-exchanged smectites with different layer-charge location were studied. The sorption of glycine depends on the nature of the interlayer cations (Ca < Na < Cu), and on the type of smectite. Sequential extraction procedures were carried out in order to test the possibility of removing metals and/or glycine from the smectite interlayer. By the end of the treatments, the release of the amino acid from the substrates, with the exception of Cu-rich smectite, was virtually complete. The thermal curves of glycine-smectites confirm the stronger bonding of the amino acid with Cu-exchanged samples, and FTIR spectra indicate that glycine is mainly sorbed in the zwitterionic form. The data obtained suggest that in investigations into mechanisms of the binding of metals by minerals and their subsequent mobilization, amino acids merit close attention.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2000

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References

Bodenheimer, W. & Heller, L. (1967) Sorption of aamino- acids by copper montmorillonite. Clay Miner. 7, 167176.Google Scholar
Boyd, S.A. & Jaynes, W.F. (1994) Role of layer charge in organic contaminant sorption by organo-clays. Pp. 4777.in. Layer Charge Characteristics of 2:1 Silicate Clay Minerals (Mermut, A.R., editor). CMS Workshop lectures, 6. Clay Minerals Society, Boulder, CO, USA.Google Scholar
Brigatti, M.F., Campana, G., Medici, L. & Poppi, L. (1996) The influence of layer charge on Zn2+ and Pb2+ sorption by smectites. Clay Miner. 31, 477483.Google Scholar
Brigatti, M.F., Franchini, G.C., Lugli, C., Pinetti, A. & Vaccari, G. (1998) Amino acid as a factor controlling distribution of heavy metals in soils and groundwater. Ann. Chim. 88, 783792.Google Scholar
Brigatti, M.F., Lugli, C., Montorsi, S. & Poppi, L. (1999) Effects of exchange cations and layer charge location on cysteine retention by smectites. Clays Clay Miner. 47, 664671.Google Scholar
Greenland, D.J., Laby, R.H. & Quirk, J.P. (1962) Adsorption of glycine and its di-, tri-, and tetrapeptides by montmorillonite. Trans. Faraday Soc. 58, 829841.CrossRefGoogle Scholar
Greenland, D.J., Laby, R.H. & Quirk, J.P. (1965) Adsorption of amino-acids and peptides by montmorillonite and illite. Trans. Faraday Soc. 61, 20132023.CrossRefGoogle Scholar
Gupta, A., Loew, G.H. & Lawless, J. (1983) Interaction of metal ions and amino acids: possible mechanisms for the adsorption of amino acids on homoionic smectite clays. Inorg. Chem. 22, 111120.Google Scholar
Jang, S.D. & Condrate, R.A. (1972) The IR spectra of lysine adsorbed on several cation-substituted montmorillonites. Clays Clay Miner. 20, 7982.Google Scholar
Jaynes, W.F. & Boyd, S.A. (1991) Hydrophobicity of siloxane surfaces in smectites as revealed by aromatic hydrocarbon adsorption from water. Clays Clay Miner. 19, 428436.CrossRefGoogle Scholar
Johnston, C.T. (1996) Sorption of organic compounds on clay minerals: a surface functional group approach. Pp. 244.in. Organic Pollutants in the Environment (Sawhney, B.L., editor). CMS Workshop lectures, 8. Clay Minerals Society, Boulder.Google Scholar
Kunze, G.W. & Dixon, J.B. (1986) Pretreatments for mineralogical analysis. Pp. 91100.in: Methods of Soil Analysis. Part 1: Physical and Mineralogical Methods, 2nd edition (Klute, A., editor). Soil Science Society of America, Madison, WI, USA.Google Scholar
Laird, D.A. (1996) Interaction between atrazine and smectite surfaces. Pp. 86100.in. Chemistry of Herbicide Metabolites in Surface and Groundwater (Mayer, M.T. & Thurman, E.M., editors). American Chemical Soc iety Symposium Series 630. Washington D.C., USA.Google Scholar
Lilley, T.H. (1985) Physical properties of amino acid solutions. Pp. 591625.in: Chemist ry and Biochemistry of the Amino Acids (Barret, G.C., editor). Oxford Polytechnic, Oxford, UK.CrossRefGoogle Scholar
Mackenzie, R.C. (1973) Oxides and hydroxides of monovalent and divalent metals. Pp. 237270.in: Differential Thermal Analysis, Vol. 1: Fundamental Aspects. Academic Press, London, UK.Google Scholar
Mosser, C., Michot, L.J., Villieras, F. & Romeo, M. (1997) Migration of cations in copper(II)-exchanged montmorillonite and laponite upon heating. Clays Clay Miner. 45, 789802.Google Scholar
Porter, T.L., Eastman, M.P., Hagerman, M.E., Price, L.B. & Shand, R.F. (1998) Site-specific prebiotic oligomerization reactions of glycine on the surface of hectorite. J. Molecular Evol. 47, 373377.CrossRefGoogle ScholarPubMed
Russell, J.D. & Fraser, A.R. (1996) Infrared methods. Pp. 1167.in: Clay Mineralogy: Spectroscopic and Chemical Determinative Methods (Wilson, M.J., editor). Chapman & Hall, London, UK.Google Scholar
Sawhney, B.L. (1996) Sorption and desorption of organic contaminants by clays and soils. Pp. 4569.in. Organic Pollutants in the Environment (Sawhney, B.L., editor). CMS Workshop lectures, 8. Clay Minerals Society, Boulder, CO, USA.Google Scholar
Sawhney, B.L. & Singh, S.S. (1997) Sorption of atrazine by Al- and Ca-saturated smectite. Clays Clay Miner. 45, 333338.CrossRefGoogle Scholar
Tan, X.S., Fujii, Y., Sato, T., Nakano, Y. & Yashiro, M. (1999) The crystal structures of glycylglycine and glycine complexes of cis,cis-1,3,5-triaminocyclohexane- copper (II) as reaction intermediates of metalpromoted peptide hydrolysis. Chem. Commun. 21, 881882.Google Scholar
Van Olphen, H. & Fripiat, J.J. (1979) Data Handbook for Clay Minerals and other Non-metallic Minerals (Van Olphen, H. & Fripiat, J.J., editors). Pergamon Press, New York.Google Scholar
Zamaraev, K.I. , Romannikov, V.N., Salganik, R.I. , Wlassoff, W.A. & Khramtsov, V.V. (1997) Modelling of the prebiotic synthesis of oligopeptides: silicate catalysts help to overcome the critical stage. Orig. Life Evol. Bios. 27, 325337.CrossRefGoogle ScholarPubMed