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2001 | 50 |

Tytuł artykułu

Characteristics of humic substances in humid subalpine forest soils in Central Taiwan

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Języki publikacji

EN

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EN
The study site, 2700 m a.s.l., is located in the central Taiwan. A globally rare combination of the mean temperature (ca. 9.5 °C) and total annual precipitation (ca. 4100 mm) makes studies on pedogenic and edaphic processes of the moist soils in this area worthwhile. The study was undertaken to investigate distribution and characteristics of humic substances in this subalpine forest ecosystem. Fulvic acids comprised a higher total organic carbon fraction (1.8 to 25%) than humic acids (1.1 to 13.4%). Fulvic acids were more mobile and migrated downwards to deeper horizons. Comparatively, humic acids were distributed more in the surface horizons. The hu- mification index, based on E4/E6, showed that humification varied in different horizons even in the same profile. The AlogK and RF values indicate that the types of humic acids extracted from Tsuga forest soil are grouped as P or A types, whereas Rp or B types are in Picea forest soil, suggesting a high degree of humification of humic acids in such soils. Features of the absorption spectra were consistent with the classification of humic acids with A logK and RF values. Humification indices and humic acid types in these subalpine soils indicate that they are similar to acidic soils elsewhere with abundant rainfall and cold climate.

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Rocznik

Tom

50

Opis fizyczny

p.41-47,fig.

Twórcy

autor
  • Academia Sinica, Nangking, Taipei 11529, Taiwan
autor

Bibliografia

  • 1. Chen J.S., Chiu C.Y.: Spectral features of humic substances in a perhumid subtropical montane forest ecosystem, Taiwan. Soil Sci. Plant Nutr., 1999.
  • 2. Chen Y., Senesi N., Schnitzer M.: Information provided on humic substances by E4/E6 ratios. Soil Sci. Soc. Am. J., 41,352-358, 1977.
  • 3. Drijber R.A., Lowe L.E.: Nature of humus in andosols under differing vegetation in Sierra Nevada, Mexico. Geoderma, 47, 221-231, 1990.
  • 4. Huang W.H., Keller W.D.: Dissolution of rock-forming silicate mineral in organic acids: simulated first-stage weathering of fresh mineral surfaces. Am. Mineral., 55, 2076-2083, 1970.
  • 5. Kononova M.M.: Soil Organic Matter. Pergamon Press, 1966.
  • 6. Kumada K.: Humus composition of some podzols in Great Britain. Pedologist, 11,71-80, 1967.
  • 7. Kumada K. Elementary composition and absorption spectra of humic and fulvic acids. Soil Sci. Plant Nutr., 31, 437-448, 1985.
  • 8. Kumada K.: Chemistry of Soil Organic Matter. Jpn. Sci. Soc. Press, Tokyo, 1987.
  • 9. Lowe L,F„: Humus fraction ratios as a means of discriminating between horizon types. Can. J. Soil Sci., 60, 219-229, 1980.
  • 10.Soil Survey Staff: Key to Soil Taxonomy (4th ed.), SMSS Technical Monograph No. 6, Blacksburg, Virginia, 1990,
  • 11.Stevenson F.J.: Humus Chemistry: Genesis, Composition and Reaction. Wiley, New York, 1982.
  • 12. Tan K.H.: Scanning electron microscopy of humic matter as influenced by methods of preparation. Soil Sci. Soc. Am J., 49, 1185-1191, 1985.
  • 13. Theng B.K.G., Tate K.R., Sollins P., Moris N., Nadkarni N., Tate R. T.: III. Constituents of organic matter in temperate and tropical soils. [In:] Dynamics of Soil Organic Matter in Tropical Ecosystem (Eds. DC. Coleman, J.M. Oafdes, G. Uehara). University of Hawaii Press, Honolulu, 1989.
  • 14 Tsutsuki K., Suzuki C., Kuwatsuka S., Becker-Heidemann P., Scharpenseel H.W.: Investigation on the stabilization of the humus in Mollisols. Z. Pflanzenemahr Bodenk,, 151, 87-90, 1988.
  • 15. Zhao L., Yang X., Inouce K.: Morphological, chemical, and humus characteristics of volcanic ash soils in Changbaishan and Wudalianchi, Northeast China. Soil Sci. Plant Nutr., 39, 339-350,

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Bibliografia

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