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2006 | 37 |

Tytuł artykułu

Nebki - formy wymuszonej akumulacji eolicznej wschodniego obrzeżenia szottu Dżerid

Treść / Zawartość

Warianty tytułu

EN
Nebkas - forms of forced aeolian accumulation of the eastern margin of the Chott Jerid

Języki publikacji

PL

Abstrakty

EN
The article includes description of nebkas - the smallest accumulation forms of aeolian origin. They originate from accumulation of wind-blown material accumulated on a lee side of a vegetation obstacle. The research was undertaken in the eastern part of the Chott Jerid, within its Holocene floor. Such forms are thought to indicate erosion of arid regions. Their appearance is usually linked to lowering of ground water table and related change in vegetation density. The researched was focused on two selected fields of nekbas. Morphometry and sedimentological features of building material were analysed. It was found that the shape of nebkas depends on a type of vegetation which constitutes the transport obstacles and forces accumulation. Lower forms (up to 0,5 m high) are created on a lee side of arfej species and are characterised by a high to length ratio 1:7 and so they have a typical shape of nebkas. Higher forms (up to 1 m) are created on a lee side of tamarix species and their high to length ratio is 1:4. Such a shape is due to a width of the plant and intensive erosion of a distal part of the form because wind frequently changes direction in this field. Sedimentological features of the forms show that material building the higher forms is better sorted comparing with lower forms and therefore it was probably transported for a longer distance. Mineral-lithological composition of the forms show a high share of quartz as well as relatively high share of gypsum (not resistant for abrasion). High content of gypsum in nebkas, seasonal capillarity with intensive evaporation lead to crusting of especially lower forms. Such a crusting strengthens the forms, protects from erosion of their distal parts and therefore explains differences in shapes of nebkas.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

37

Opis fizyczny

s.69-79,rys.,tab.,wykr.,fot.,bibliogr.

Twórcy

autor
  • Zakład Geomorfologii, Wydział Geografii i Studiów Regionalnych, Uniwersytet Warszawski w Warszawie, Warszawa
autor
  • Zakład Geografii Stosowanej i Kartografii, Wydział Geografii, Uniwersystet im.Iwana Franka we Lwowie, Lwów

Bibliografia

  • Coque R., 1962. La tunisie présaharienne. Etude géomorphologique. Armand Colin, Paris.
  • Dłużewski M., Dubis L., Woronko B. 2003., Nebki - formy wymuszonej akumulacji eolicznej N-części obniżenia Khargi. [w:] Warsztaty geomorfologiczne, Egipt, 5-22.04.2002, WGiSR, SGP, Mat. Konf. Warszawa.
  • Dłużewski M., Woronko B., 2000. Genesis of forced forms of aeolian accumulation - nebkhas in the area of Shott El Jerid (S Tunisia). [w:] Dulias R., Pełka-Gościniak J. (red.) Aeolian processes in diferent landscape zones. Procesy eoliczne w różnych strefach klimatycznych, WNoZ UŚl, SGP, Sosnowiec.
  • Dougill A.J., Thomas A.D., 2002. Nebkha dunes in the Molopo Basin, South Africa and Bostwana: formation control and their validity as indicators of soil degradation. Jurnal of Arid Environmental 50.
  • Gile L.H., 1957. Holocene soil and soli geomorphic relations in arid region of southern New Maxico. Quarter. Res. 5.
  • Gunatilaka A., Mwango S., 1987. Continental sebkhas pans and associated nebkhas in southern Kuwait, Arabian Gulf. [w:] Froctick L., Reid I. (red.), Desert Sediments: Ancient and Modern. Geolog. Soc. Spec. Publ. 35, 187-203.
  • Hesp P.A., 1981. Formation of shadow dunes. J. Sediment. Petrol. 51.
  • Kosmowska-Suffczyńska D., 1980. Formy wydmowe na sebhce Sabhet El-Muh w okolicy Palmyry. Prace i St. Geog. 9.
  • Langberg P.R. 2000., Nabkha (coppice dune) field of south-central New Mexico, U.S.A. Jurnal of Arid Environmental 46.
  • Mycielska-Dowgiałło E., 2001. Eolizacja osadów jako wskaźnik stratygraficzny czwartorzędu. Prac. Sedyment, WGiSR UW Warszawa.
  • Nickling W.G., Wolfe A.S., 1994. The morphology and origin of nabkhas, region of Mopti, Mali, West Africa. Jurnal of Arid Environmental 28.
  • Piertow M.P., 1976. Pustynie kuli ziemskiej. PWN. Warszawa.
  • Pietrow M. P., 1962. Types de deserts de l'Asia centrale. Ann de Geog. 10, 131-155.
  • Pye K., Tsoar H., 1990. Aeolian Sand and Sand Dunes. London. Unwin Hyman.
  • Rango A., Chopping M., Ritchie J., Havstad K., Kustas W., Schmugge W. 2000. Morphological
  • Characteristics of Shrub Coppice Dunes I Desert Grasslands of Southern New Mexico derived from Scanning LIDAR. Remote Sens. Environmental 74.
  • Szczypek T. 1994. Inicjalne kopczyki piaszczyste typu „nebkha”. [w:] Nowaczyk B., Szczypek T. (red.) Vistuliańsko-holoceńskie zjawiska i procesy eoliczne (wybrane zagadnienia). Poznań.
  • Tengberg A. 1994. Nebkhas - their spatial distribution, morphology, composition and age - in the Sidi Bouzid area, central Tunesia. Ziet. fur Geomorph. 38.
  • Tengberg A., Chen D. 1998. A comparitive analysis of nebhkas in central Tunisia and northen Burkina Faso. Geomorphology 22.
  • Thomas D.S.G., Tsoar H. 1990. The geomorphological role of vegetation in desert dune system. [w:] Thornes J.B. (red.) Vegetation and Erosion. Londyn, John Wiley.
  • Thomas D.S.G. 1997. Sand seas and Aeolian bedforms. [w:] Thomas D.S.G. (red.) Arid Zone Geomorphology: Process, Form and Change of Drylands. Londyn, John Wiley.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

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