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Tytuł artykułu

Mikromorfologiczne cechy pokryw glebowych obszaru o najwyższych opadach na świecie - Cherrapunji, Wyżyna Meghalaya, Indie

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
EN
Micromorphological features of the soil covers in the area of the highest rainfall in the world -Cherrapunji, Meghalaya Hills, India
Języki publikacji
PL
Abstrakty
EN
The paper presents the results of micromorphological analyses concerning soil covers near Cherrapunji with mean annual rainfall of 12 000 mm. Two soil profiles representing typical land use: grass formation (Cherrapunji–1) and natural evergreen forest (Cherrrapunji–2) have been choosen. Processes leading to formation of Dystric Cambisols predominate in both profiles. However they have different weathering features. Soil cover under grass has more weathered quartz and contains less feldspars compared to soil cover in the forest area. Soils are characterized also by a large volume of pores which is typical for the tropical humid areas. The rapid infiltration of large amounts of water protects forest soil from surficial erosion. In case of soils under grass vegetation, micropores are filled with fresh organic matter (fine roots and plants tissue). Since both profiles are located on similar substratum (Paleogene sandstones) and under the same climatic conditions, it is assumed that the micromorphological differences are due to long-term (several centuries) differences in local land use.
Rocznik
Strony
293--298
Opis fizyczny
Bibliogr. 31 poz., fot., tab., wykr.
Twórcy
autor
  • Instytut Geografii i Przestrzennego Zagospodarowania, Polska Akademia Nauk, ul. św. Jana 22, 31–018 Kraków
autor
  • Instytut Geografii i Przestrzennego Zagospodarowania, Polska Akademia Nauk, ul. św. Jana 22, 31–018 Kraków
Bibliografia
  • 1. Agriculture and Soil Division, Indian Institute of Remote Sensing
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  • 4. BOR N.L. 1942 - Relict vegetation of Shillong Plateau-Assam. Indian Forest Records, 3: 152-195.
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  • 6. BREMER H. 2002 - Tropical weathering, landforms and geomorphological processes: Field work and laboratory analysis. Zeitschrift fur Geomorphologie, 46: 273-291.
  • 7. BULLOCK P., FEDOROFF N., JONGERIUS A., STOOPS G. & TURSINA T. 1985 - Handbook for Soil Thin Section Description. Wane Research Publications, Wolverhampton.
  • 8. DELVIGNE J.E. 2001- Atlas of micromorphology of mineral alteration and weathering. The Canadian Mineralogist Special Publication, 3, Ottawa, Canada.
  • 9. FAO 1998 - World reference base for soil resources. 84 World soil resources report, Rome.
  • 10. FITZPATRICK E.A. 1990 - Soil Microscopy and Micromorphology. Wiley, London.
  • 11. Geological Survey of India 1974 - Geology and mineral resources of the states of India, part IV, Meghalaya. Geol. Surv. India, Miscellaneous Publications, 30: 69-90.
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  • 13. ISLAM M.R., STUART R., RISTO A. & VESA P. 2002 - Mineralogical changes during intensive chemical weathering of sedimentary rocks in Bangladesh. J. Earth Sci., 20: 889-901.
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  • 15. KUBINIOK J. 1992 - Soils and weathering as indicators of landform development in the mountains and basins of Northern Thailand. Zeit- schrift fur Geomorphologie N.F., Supplementband, 91: 67-78.
  • 16. LAUFENBERG M. 1992 - The different types of weathering of tropical soils in relation to source-rock material - examples from southern and western India. Zeitschrift fur Geomorphologie N.F., Supplement- band, 91: 23-27.
  • 17. MAZUMDAR S.K. 1986 - The Precambrian framework of part of the Khasi Hills, Meghalaya. Records of the Geological Survey of India, 117: 1-59.
  • 18. MULYANTO B. & STOOPS G. 2003 - Mineral neoformation in pore spaces during alteration and weathering of andesitic rocks in humid tropical Indonesia. Catena, 54, 385-391.
  • 19. NAG S. & PAL T. 1993 - Specialised thematic mapping for structural study of the tertiary belt of Meghalaya along road sections. Geol. Surv. India, 128: 13-15.
  • 20. NAG S., GAUR R.K.& PAL T. 2001 - Late Cretaceous-Tertiary Sediments and Assiociated Faults in Southern Meghalaya Plateau of India vis-a-vis South Tibet: Their Interrelationships and Regional Implications. J. Geol. Soc. India, 57: 327-338.
  • 21. NYE P. H. & TINKER P. B. 1977 - Solute movement in the soil-root system. Blackwell Scientific Publications, Oxford, UK.
  • 22. PAL D.K., SRIVASTAVA P., DURGE S.L. & BHATTACHARYYA T. 2003 - Role of microtopography in the formation of sodic soils in the semi-arid part of the Indo-Gangetic plains, India. Catena, 51: 3-31. Polski Komitet Normalizacyjny 1998a - PN-R-04032 Gleby i utwory mineralne. Pobieranie próbek i oznaczanie składu granulometrycznego. Warszawa.
  • 23. Polski Komitet Normalizacyjny 1998b - PN-R-04033 Gleby i utwory mineralne. Podział na frakcje i grupy granulometryczne. Warszawa.
  • 24. PROKOP P. 2004 - Vegetation and land use. [W:] Starkel L., Singh S. (red.) - Rainfall, runoff and soil erosion in the globally extreme humid area, Cherrapunji region, India. Pr. Geogr., 191: 33-36.
  • 25. RAM S.C. & RAMAKRISHNAN P.S. 1988 - Litter production and decomposition patterns in seral grasslands at Cherrapunji in north-eastern India. Pedobiologia, 32: 65-76.
  • 26. SANDER H. 2002 - The porosity of tropical soils and implications for geomorphological and pedogenetic processes and the movement of solutions within weathering cover. Catena, 49: 129-137.
  • 27. SCHNUTGEN A. 1992 - Spheroidal waethering, granular disintegration and loamification of compact rock under different climatic conditions. Zeitschrift fur Geomorphologie N.F., Supplementband, 91: 79-94. Soil Survey Staff 1998 - Taxonomy Keys. United States Department of Agriculture, Washington D.C.
  • 28. SRIVASTAVA P. & PARKASH B. 2002 - Polygenetic Soils of the North Central part of the Gangetic plains: A Micromorphological approach. Catena, 46: 243-259.
  • 29. STOOPS G. 2003 - Guidelines for analysis and description of soil and regolith thin section. Soil Science Society of America, INC, Madison Wisconsin.
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  • 31.World Meteorological Organisation 1995 - Guide to Hydrological Practices. 5th edn., 168, Geneva, Switzerland.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS2-0014-0060
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