SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Suetsugu, A.
Right arrow Articles by Nakano, M.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Suetsugu, A.
Right arrow Articles by Nakano, M.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Suetsugu, A.
Right arrow Articles by Nakano, M.
Related Collections
Right arrow Soil Biochemistry
Right arrow Soil Chemistry
Right arrow Soil Physics
Soil Science Society of America Journal 65:1129-1135 (2001)
© 2001 Soil Science Society of America


DIVISION S-2—SOIL CHEMISTRY

Effects of Amphiphilic Amines on Moisture Characteristics of Alluvial and Volcanic Soils

Atsushi Suetsugu*, Tsuyoshi Miyazaki and Masashi Nakano

Laboratory of Environmental Soil Physics and Soil Hydrology, Department of Biological and Environmental Engineering, The Graduate School of Agricultural and Life Sciences, The University of Tokyo, 1-1-1, Yayoi, Bunkyo-ku, Tokyo 113-8657, Japan

* Corresponding author (suetsugu{at}par.odn.ne.jp)

If organic matter (OM) has amphiphilicity, the properties of hydration of the OM-coated soil particles would vary drastically in dry conditions. Therefore, soil-moisture characteristics within the relatively low water potential should be understood in relation to the conformation of the sorbed amphiphilic OM. In the present study, the effects of amphiphilic behavior of OM on the moisture characteristics of alluvial soil (AS) and volcanic soil (VS) were investigated using three simple amphiphilic amines. The psychrometry of AS showed the decrease of sorbed water around 1.8 nm of statistical thickness because of the sorption of hexadecyltrimethyl ammonium (HDTMA). Fourier transform infrared spectroscopy (FTIR) of soils showed an increase in the wavenumber of the antisymmetric stretching of -OH and -CH2, suggesting the formation of hydrophobic outer surfaces by n–hexadecyl function. The peaks in the -CH2 rocking band suggest that the HDTMA sorbed at AS had the residual amorphous moieties. In the case of VS–HDTMA, the peak was hidden by a broad peak due to hydrated aluminosilicates in VS. These findings imply that the amorphous moieties of HDTMA sorbed at both soils were affected by residual water in the air dried samples. According to the clay mineralogy of the soils, the greater hydrophobicity in AS–HDTMA was attributed to intercalation of HDTMA into the expansible phyllosilicates in AS. In contrast, the relatively moderate hydrophobicity in VS–HDTMA indicated that the hydrophilic micropores (D < 2 nm) in VS restrict the sorption of HDTMA but enable it to exchange water.

Abbreviations: AS, alluvial soil • AA, amphiphilic amine • CEC, cation-exchange capacity • CMC, critical micelle concentration • ESR, electron spin resonance spectroscopy • FTIR, Fourier transform infrared spectroscopy • HDTMA, hexadecyltrimethyl ammonium • HDTMAC, hexadecyltrimethyl ammonium Cl • NMR, nuclear magnetic resonance spectroscopy • OM, organic matter • SOM, soil organic matter • TMA, tetramethyl ammonium • TMPA, trimethylphenyl ammonium • VS, volcanic soil




This article has been cited by other articles:


Home page
Soil Sci.Home page
D. Zhu, B. E. Herbert, and M. A. Schlautman
Sorption of Pyridine to Suspended Soil Particles Studied by Deuterium Nuclear Magnetic Resonance
Soil Sci. Soc. Am. J., September 1, 2003; 67(5): 1370 - 1377.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
D. Zhu, B. E. Herbert, and M. A. Schlautman
Molecular-Level Investigation of Monoaromatic Compound Sorption to Suspended Soil Particles by Deuterium Nuclear Magnetic Resonance
J. Environ. Qual., January 1, 2003; 32(1): 232 - 239.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2001 by the Soil Science Society of America.