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Effect of different fractions of weathered pumice in the formation of humic-like substances

Published online by Cambridge University Press:  09 July 2018

A. Miura
Affiliation:
Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan
S. Fukuchi
Affiliation:
Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan
R. Okabe
Affiliation:
Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan
M. Fukushima*
Affiliation:
Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan
M. Sasaki
Affiliation:
National Institute of Advanced Industrial Science and Technology (AIST), 2-17-2 Tsukisamu-Higashi, Toyohira-ku, Sapporo 062-8517, Japan
T. Sato
Affiliation:
Division of Sustainable Resources Engineering, Graduate School of Engineering, Hokkaido University, Sapporo 060-8628, Japan
*

Abstract

Polycondensation reactions between amino acids and phenols are one of the pathways for the formation of humic substances, and clay minerals are able to catalyse these reactions. To investigate the catalytic power of allophane, an allophane fraction (ALF) was separated from weathered pumice (WP) that contained imogolite as an impurity by taking advantage of differences in sedimentation velocity. The iron content in the separated ALF was increased by up to 3.0% compared to that in the starting WP (1.3%), and the ALF was further treated with sodium dithionate and citric acid (ALF-DC) to remove the iron. The catalytic powers of WP, ALF and ALF-DC were evaluated, based on the degree of darkening of reaction mixtures from polycondensation reactions between catechol and tryptophan, model compounds for precursors of humic substances. The catalytic power for ALF was significantly higher than the corresponding values for WP and ALF-DC. This can be attributed to the high iron content of the ALF, which serves as a Lewis acid that can enhance nucleophilic reactions which occur during the polycondensation reactions.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2011

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References

Chiavari, G. & Galletti, G.C. (1992) Pyrolysis-gas chromatography/mass spectrometry of amino acids. Journal of Analytical Applied Pyrolysis, 24, 123137.Google Scholar
Farner, V.C., Palmieri, F., Violante, A. & Violante, P. (1991) Amorphous hydroxyaluminum silicates formed under physiological saline conditions, and in CaCO3-buffered solutions-stability and significance for alzheimer plaque precipitates. Clay Minerals, 26, 281287.Google Scholar
Fukushima, M. & Tatsumi, K. (2007) Degradation of pentachlorophenol in contaminated soil suspensions by potassium monopersulfate catalyzed oxidation by a supramolecular complex between tetra(p-sulfophenyl) porphineiron(III) and hydroxypropyl-β-cyclodextrin. Journal of Hazardous Materials, 144, 222228.Google Scholar
Fukushima, M., Tanaka, S., Nakamura, H. & Ito, S. (1996) Acid-base characterization of molecular weight fractionated humic acid. Talanta, 43, 383390.CrossRefGoogle ScholarPubMed
Fukushima, M., Tatsumi, K. & Morimoto, K. (2000) Influence of iron(III) and humic acid on the photodegradation of pentachlorophenol. Environmental Toxicology and Chemistry, 19, 17111716.Google Scholar
Fukushima, M., Miura, A., Sasaki, M. & Izumo, K. (2009a) Effect of an allophanic soil on humification reactions between catechol and glycine: Spectroscopic investigations of reaction products. Journal of Molecular Structure, 917, 142147.Google Scholar
Fukushima, M., Yamamoto, M., Komai, T. & Yamamoto, K. (2009b) Studies of structural alterations of humic acids from conifer bark residue during composting by pyrolysis-gas chromatography/mass spectrometry using tetramethylammonium hydroxide (TMAH-py- GC/MS). Journal of Analytical and Applied Pyrolysis, 86, 200206.Google Scholar
He, H., Barr, T.L. & Klinowski, J. (1995) ESCA and solid-state NMR-studies of allophane. Clay Minerals, 30, 201209.Google Scholar
Hur, J., Williams, M.A. & Schlautman, M.A. (2006) Evaluating spectroscopic and chromatographic techniques to resolve dissolved organic matter via end member mixing analysis. Chemosphere, 63, 387402.Google Scholar
Jokic, A., Wang, M.C., Liu, C., Frenkel, A.I. & Huang, P.M. (2004) Integration of the polyphenol and Maillard reactions into a unified abiotic pathway for humification in nature: the role of δ-MnO2 . Organic Geochemistry, 35, 747762.Google Scholar
Kelleher, B.P. & Simpson, A.J. (2006) Humic substances in soils: Are they really chemically distinct. Environmental Science & Technology, 40, 46054611.CrossRefGoogle ScholarPubMed
Miura, A., Okabe, R., Izumo, K. & Fukushima, M. (2009) Influence of the physicochemical properties of clay minerals on the degree of darkening via polycondensation reactions between catechol and glycine. Applied Clay Science, 46, 277282.Google Scholar
Nanzyo, M., Yamasaki, S., Honna, T., Yamada, I., Shoji, S. & Takahashi, T. (2007) Changes in element concentrations during Andosol formation on tephra in Japan. European Journal of Soil Science, 58, 465477.CrossRefGoogle Scholar
Parfitt, R.L. (2009) Allophane and imogolite: role in soil biogeochemical processes. Clay Minerals, 44, 135155.Google Scholar
Sharami, S.M., Forghani, A., Akbarzadeh, A. & Ramezanpour, H. (2010) Mineralogical characteristics and related surface charge functions of some selected soils of temperate regions of northern Iran. Clay Minerals, 45, 327348.Google Scholar
Shindo, H. & Huang, P.M. (1982) Role of Mn(IV) oxide in abiotic formation of humic substances in the environment. Nature, 298, 363365.Google Scholar
Shindo, H. & Huang, P.M. (1984a) Catalytic effects of manganese(IV), iron(III), aluminum and siliconoxides on the formation of phenolic polymers. Soil Sciences Society of America Journal, 48, 927934.Google Scholar
Shindo, H. & Huang, P.M. (1984b) Significance of Mn(IV) oxide in abiotic formation of organic nitrogen complexes in natural environments. Nature, 298, 363365.Google Scholar
Smeulders, D.E., Wilson, M.A. & Kamalikannangara, G.S. (2001) Host-guest interactions in humic materials. Organic Geochemistry, 32, 13571371.Google Scholar
Stevenson, F.J. & Goh, K.M. (1971) Infrared spectra of humic acids and related substances. Geochimica et Cosmochimica Ada, 35, 471483.Google Scholar
Tan, K.H. (2003) Humic Matter in Soil and the Environment: Principles and Controversies, Chapter 2, Dekker, New York.Google Scholar
Theng, B.K.G. & Yuan, G. (2008) Nanoparticles in the soil environmen. Elements, 4, 395399.Google Scholar
Tsutsuki, K. & Kuwatsuka, S. (1978) Chemical studies on soil humic acids. Ill Nitrogen distribution in humic acids. Soil Science and Plant Nutrition, 24, 561570.Google Scholar
Varma, R.S. (2002) Clay and clay-supported reagents in organic synthesis. Tetrahedron, 58, 1235-1255.CrossRefGoogle Scholar
Wada, K. & Yoshinaga, N. (1969) The structure of “imogolite”. American Mineralogist. 54, 5071.Google Scholar
Wang, M.C. & Huang, P.M. (2000) Ring cleavage and oxidative transformation of pyrogallol catalyzed by Mn, Fe, Al, Si oxides. Soil Science, 165, 934942.Google Scholar
Wang, M.C. & Huang, P.M. (2003) Cleavage and polycondensation of pyrogallol and glycine catalyzed by natural soil clays. Geoderma, 112, 3150.Google Scholar
Wang, M.C. & Huang, P.M. (2005) Cleavage of 14C-labeled glycine and its polycondensation with pyrogallol as catalyzed by birnessite. Geoderma, 124, 415426.Google Scholar
Yabuta, H., Fukushima, M., Kawasaki, M., Tanaka, F., Kobayashi, T. & Tatsumi, K. (2008) Multiple polar components in poorly-humified humic acids stabilizing free radicals: Carboxyl and nitrogen-containing carbons. Organic Geochemistry, 39, 13191335 Google Scholar