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Role of smectites and Al-substituted goethites in the catalytic condensation of arginine and glucose

Published online by Cambridge University Press:  01 January 2024

Javier M. Gonzalez  and
David A. Laird
Javier M. Gonzalez*
Affiliation:
Department of Agronomy, Iowa State University, Ames, IA 50011, USA
David A. Laird
Affiliation:
USDA-ARS, National Soil Tilth Laboratory, 2150 Pammel Drive, Ames, IA 50011, USA
*
*E-mail address of corresponding author: [email protected]
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Abstract

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The polyphenol theory of humic-substance formation has been studied extensively; however, an alternative theory, that humic substances are formed through the condensation of amino acids and reducing sugars (Maillard reaction), has not been explored to the same extent. The general objectives of this study were to determine whether smectites and goethites catalyze the abiotic polymerization of arginine and glucose to form humic-like compounds. The effects of smectite type, saturating cation, and the degree of Al substitution in goethites on the polymerization reaction were also studied. Four cation-saturated smectites and four Al-substituted goethites were incubated abiotically with solutions containing a mixture of arginine + glucose for 21 days at 37°C. After the incubations, total C recovered ranged from 80.6 to 123.8% and from 100.5 to 105.1% for the smectite and goethite systems, respectively. At the end of the incubations, 21.4–50.3% of the added C and 16.5–90% of the added N were sorbed on the various smectites, and 6.2–9.0% of the added C and 2.3–4.6% of added N was sorbed on the goethites in a form that could not be desorbed by washing with 100 mM CaCl2. X-ray diffraction analysis indicated that some of the sorbed C was intercalated in the smectites and FTIR analysis provided evidence of new absorption bands at 1650 and 1668 cm−1, which are consistent with Maillard reaction products. Thus, it is concluded that smectites catalyze the condensation of arginine and glucose to form humic-like products. Goethites, however, have little or no ability to catalyze this reaction.

Keywords

ArginineCatalysisCondensationGlucoseGoethitesHumic SubstancesMaillard ReactionSmectites
Type
Research Article
Information
Clays and Clay Minerals , Volume 52 , Issue 4 , August 2004 , pp. 443 - 450
Copyright
Copyright © The Clay Minerals Society 2004

References

Arfaioli, P. Pantani, O.L. Bosetto, M. and Ristori, G.G., (1999) Influence of clay minerals and exchangeable cations on the formation of humic-like substances (melanoidins) from D-glucose and L-tyrosine Clay Minerals 34 487–497 10.1180/000985599546271.CrossRefGoogle Scholar
Balogh, M. and Laszlo, P., (1993) Organic Chemistry using Clays New York Springer-Verlag.Google Scholar
Bosetto, M. Arfaioli, P. and Pantani, O.L., (2002) Study of the Maillard reaction products formed by glycine and D-glucose on different mineral substrates Clay Minerals 37 195–204 10.1180/0009855023710028.CrossRefGoogle Scholar
Dashman, T. and Stotzky, G., (1985) Physical properties of kaolinitic montmorillonite and kaolinite complexed with amino acids and peptides Soil Biology and Biochemistry 17 189–195 10.1016/0038-0717(85)90114-2.CrossRefGoogle Scholar
de Farias, R.F. Martínez, L. and Airoldi, C., (2002) A calorimetric investigation into copper-arginine and copper-alanine solid state interactions Transition Metal Chemistry 27 253–255 10.1023/A:1014842827521.CrossRefGoogle Scholar
Gogus, F. Bozkurt, H. and Eren, S., (1998) Nonenzymatic browning reactions in multi sugar and amino acid systems Journal of Food Processing and Preservation 22 81–90 10.1111/j.1745-4549.1998.tb00806.x.Google Scholar
Gonzalez, J.M., (2002) Role of clay minerals on soil organic matterstabilization and humification Ames, USA Iowa State University PhD thesis.Google Scholar
Hedges, J.I., (1978) The formation and clay mineral reactions of melanoidins Geochimica et Cosmochimica Acta 42 69–79 10.1016/0016-7037(78)90218-1.CrossRefGoogle Scholar
Hedges, J.I. and Hare, P.E., (1987) Amino acid adsorption by clay minerals in distilled water Geochimica et Cosmochimica Acta 51 255–259 10.1016/0016-7037(87)90237-7.CrossRefGoogle Scholar
Herbillon, A.J. et al. and Stucki, J.W. (1988) et al. , Introduction to the surface charge properties of iron oxides and oxidic soils Iron and Soils and Clay Minerals Dordrecht, The Netherlands D. Reidel Publishing Co. 251–266 10.1007/978-94-009-4007-9_10.CrossRefGoogle Scholar
Ikawa, M. and Snell, E.E., (1954) Oxidative deamination of amino acids by pyridoxal and metal salts Journal of the American Chemical Society 76 4900–4902 10.1021/ja01648a041.CrossRefGoogle Scholar
Laird, D.A. Martens, D.A. and Kingery, W.L., (2001) Nature of clay-humic complexes in an agricultural soil: I. Chemical, biochemical, and spectroscopic analyses Soil Science Society of America Journal 65 1413–1425 10.2136/sssaj2001.6551413x.CrossRefGoogle Scholar
Lehmann, R.G. Cheng, H.H. and Harsh, J.B., (1987) Oxidation of phenolic acids by soil iron and manganese oxides Soil Science Society of America Journal 51 352–356 10.2136/sssaj1987.03615995005100020017x.CrossRefGoogle Scholar
Naidja, A. and Siffert, B., (1989) Glutamic acid deamination in the presence of montmorillonite Clay Minerals 24 649–661 10.1180/claymin.1989.024.4.07.CrossRefGoogle Scholar
Phan, C.V. Tosi, L. and Garnier, A., (1975) Etude spectroscopique des complexes cuivre-L-arginine Journal of Inorganic and Nuclear Chemistry 37 2385–2388 10.1016/0022-1902(75)80761-5.CrossRefGoogle Scholar
Rengasamy, P. and Oades, J.M., (1977) Interaction of monomeric and polymeric species of metal ions with clay surfaces. I. Adsorption of iron (III) species Australian Journal of Soil Research 15 221–233 10.1071/SR9770221.CrossRefGoogle Scholar
Reyes, F.G.R. Poocharoen, B. and Wrolstand, R., (1982) Maillard reaction of sugar-glycine model systems: changes in sugar concentration, color and appearance Journal of Food Science 47 1376–1377 10.1111/j.1365-2621.1982.tb07690.x.CrossRefGoogle Scholar
Schwertmann, U. and Cornell, R.M., (2000) Iron Oxides in the Laboratory 2nd 10.1002/9783527613229 188 pp.CrossRefGoogle Scholar
Stevenson, F.J. and Cole, M.A., (1999) Cycles of Soil: Carbon, Nitrogen, Phosphorus, Sulfur, Micronutrients 2nd New York John Wiley & Sons, Inc. 427 pp.Google Scholar
Theander, O. and Nelson, D.A., (1978) Aqueous, high-temperature transformation of carbohydrates relative to utilization of biomass Advances of Carbohydrate Chemistry and Biochemistry 46 273–326 10.1016/S0065-2318(08)60169-9.CrossRefGoogle Scholar
Vazko, P.D. Blackwell, J. and Koenig, J.L., (1972) Infrared and raman spectroscopy of carbohydrates Carbohydrate Research 23 407–416 10.1016/S0008-6215(00)82690-7.CrossRefGoogle Scholar
Wang, M.C. and Huang, P.M., (1989) Pyrogallol transformations as catalyzed by nontronite, bentonite, and kaolinite Clays and Clay Minerals 37 525–531 10.1346/CCMN.1989.0370604.CrossRefGoogle Scholar
Yamamoto, S. and Ishiwatari, R., (1989) A study of the formation mechanism of sedimentary humic substances — II. Protein-based melanoidin model Organic Geochemistry 14 479–489 10.1016/0146-6380(89)90028-4.CrossRefGoogle Scholar
Yeomans, J.C. and Bremner, J.M., (1988) A rapid and precise method for routine determination of organic carbon in soil Communications in Soil Science and Plant Analysis 19 1467–1476 10.1080/00103628809368027.CrossRefGoogle Scholar