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2010 | 45 |

Tytuł artykułu

Erozja gleb pod różnymi systemami upraw w klimacie monsunowym Wyżyny Meghalaya (Indie) i zapis jej skutków w pokrywach stokowych

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Warianty tytułu

EN
Soil erosion under different cultivation systems in the monsoonal climate of the Meghalaya Plateau (India) and record of its effects in slope deposits

Języki publikacji

PL

Abstrakty

EN
The Meghalaya Plateau, located in NE India, forms hilly horst block elevated to about 2000 m a.s.l. In the subtropical monsoonal climate, with strong mean annual rainfall gradient from 11,000 mm in Cherrapunji to 2,200 mm in Shillong and 1,600 mm in Gauhati were developed several cultivation systems. The shifting cultivation is the oldest and predominant system at lower elevations (such near Gauhati). It induces soil loss of about 40 t ha⁻¹ yr⁻¹ under cereals and perennial cropping on slopes up to 25-40°. As long as this system has long a cycle which permits forest regrowth on the abandoned fields, the effect of agricultural activity is not visible in the soil profiles. Intensive human activity (near Shillong), resulted in development of the sedentary agriculture, where soil erosion rates of about 55 t ha⁻¹ y⁻¹ are observed under potato cultivation. Radiocarbon dates of colluvial deposits in this area indicate intensification of agricultural human activity from at least 200-300 years. Closer to the southern margin of the plateau (near Cherrapunji), high monsoonal rainfall combined with cultivation in the past caused transformation of forest to grassland. The erosion below 2 t ha⁻¹ yr⁻¹ indicates that compact pavement of soil and root grass system has exerted a greater control over the sediment transfer than the energy impact of the rainfall and overland flow. Only wet rice cultivation in populated valleys and creation of terraces does not threat the environment. Various forms of agriculture and accelerated soil erosion lead to the gradual retreat of cultivated fields from high to low rainfall areas on the Meghalaya Plateau.

Wydawca

-

Rocznik

Tom

45

Opis fizyczny

s.49-66,tab.,wykr.,bibliogr.

Twórcy

autor
  • Zakład Geomorfologii i Hydrologii Gór i Wyżyn, Instytut Geografii i Przestrzennego Zagospodarowania - Polska Akademia Nauk, Kraków

Bibliografia

  • Budek A., Prokop P., 2005, Mikromorfologiczne cechy pokryw glebowych obszaru o najwyższych opadach na świecie - Cherrapunji, Wyżyna Meghalaya, Indie, Przegl. Geol. 53, 4, 293- 298.
  • El-Swaify S.A., 1997, Factors affecting soil erosion hazards and conservation needs for tropical steeplands, Soil Technology 11, 3- 16
  • Froehlich W., 2004a, Soil erosion in experimental catchment, [w:] L. Starkel, S. Singh (red.), Rainfall, runoff and soil erosion in the globally extreme humid area, Cherrapunji region, India, Prace Geogr. 191, 81-89.
  • Froehlich W., 2004b, Soil erosion, suspended sediment sources and deposition in the Maw-Ki-Syiem drainage basin, Cherrapunji, northeastern India, [w:] V. Golosov, V. Belyaev, D.E. Walling (red.), Sediment transfer through the fluvial system, IAHS Publication 288, 138-146
  • Gafur A., Jensen J.R., Borggaard O.K., Petersen L., 2003, Runoff and losses of soil and nutrients from small watersheds under shifting cultivation (jhum) in the Chittagong Hill Tracts of Bangladesh, Journal of Hydrology 274, 30-46.
  • GSI, 1974, Geology and mineral resources of the states of India, part IV, Meghalaya, Geological Survey of India, Miscelaneous Publication 30, 69-90.
  • Hudson N. W. , 1982, Soil Conservation, London, Batsford.
  • Khiewtam R.S., 1986, Ecosystem function of protected forests of Cherrapunji and adjoining areas, Praca doktorska, North-Eastem Hill University, Shillong.
  • Kostrowicki J., 1973, Zarys geografii rolnictwa, PWN, Warszawa.
  • Migoń P., Traczyk A., 1998, Pokrywy stokowe - środowisko powstawania i cechy diagnostyczne, [w:] E. Mycielska-Dowgiałło (red.), Struktury sedymentacyjne i postsedymentacyjne w osadach czwartorzędowych i ich wartość interepretacyjna, WGiSR UW, Warszawa, 285-301.
  • Mishra B.K., Ramakrishnan P.S., 1983, Slash and burn agriculture at higher elevations in north-eastern India, I. Sediment, water and nutrient losses, Agriculture, Ecosystems and Environment 9, 69- 82.
  • Morgan R. P.C., 1995, Soil Erosion and Conservation, Longman.
  • Murata F., Hayashi T., Matsumoto J., Asada H., 2007, Rainfall on the Meghalaya plateau in northeastern India - one of the rainiest places in the world, Natural Hazards 42, 2, 391 - 399.
  • Parthasarathy B., 1984, Interannual and long-term variability of Indian summer monsoon rainfall, Proc. Indian Acad. Sci. (Earth Planetary Science) 93, 371-385.
  • Prokop P., 2005a, Modelowanie erozji wodnej w klimacie monsunowym o najwyższych na świecie opadach (zlewnia UMIEW, Wyżyna Meghalaya, Indie), Acta Agrophysica 5, 1, 121 -128.
  • Prokop P., 2005b, Natural hazards and anthropogenic impact on environment in a tropical mountain catchment, Meghalaya Hills, India, St. Geomorph. Carpatho-Balcanica 39, 95-113.
  • Prokop P. , 2007, Degradacja środowiska przyrodniczego południowego skłonu Wyżyny Meghalaya, Indie, Prace Geogr. IGiPZ PAN, 210.
  • Prokop P., Walanus A., 2003, Trend and periodicity in the longest instrumental rainfall series for the area of most extreme rainfall in the world, northeast India, Geographia Polonica 76, 2, 25- 35.
  • Ram S.C., 1986, Ecosystem structure and function of seral communities of degraded environment at Cherrapunji and adjoining areas. Praca doktorska, North-Eastern Hill University, Shillong.
  • Singh R.S., 2005, Soil Series of Meghalaya, Technical Bulletin, 121, NBSS&LUP, Nagpur.
  • Singh G., Babu R., Chandra S., 1981, Soil Loss Predictions in India, CS& WCRTI, Bulletin No 12/D9, Dehra Dun India.
  • Soja R. , Starkel L., 2007, Extreme rainfalls in Eastern Himalaya and southern slope of Meghalaya Plateau and their geomorphologic impacts, Geomorphology 84, 170-180.
  • Starkel L., Singh S. (red.), 2004, Rainfall, runoff and soil erosion in the globally extreme humid area, Cherrapunji region. India, Prace Geogr. IGiPZ PAN 191.
  • Toky O.P., Ramakrishnan P.S., 1981, Cropping and yields in agricultural systems of the North-Eastern hill region of India, Agro-Ecosystems 7, 11 - 25.
  • Toky O.P., Ramakrishnan P.S., 1983, Secondary succession following slash and burn agriculture in North-Eastern India, 1, Biomass, litterfall and productivity, Journal of Ecology 71 , 735- 745.
  • Whitlock C., Larsen C., 2001, Charcoal as a fire proxy, [w:] J.P. Smol, H.J. Birks, W.M. Last (red.), Tracking environmental change using lake sediments, vol. 3, Terrestrial, algal and siliceous indicators, Kluwer Academic Publisher, Dordrecht, The Netherlands.
  • Whitmore T.C. , 1975, Tropical Rain Forests of the Far East, Clarendon Press, Oxford.
  • Wischmeier W.H., Smith D.D., 1978, Predicting Rainfall Erosion Losses, USDA Agricultural Research Service Handbook, 537, Washington.
  • Xie Y., Liu B., Nearing M.A., 2002, Practical thresholds for separating erosive and nonerosive storms, Transactions of American Society of Agricultural Engineers 45, 6, 1843- 1847.

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Bibliografia

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