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Distribution and development of gullies in Southern East Siberia (Russia)

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Języki publikacji
EN
Abstrakty
EN
Large catchment basins (the Yenisei, Angara, Lena, Selenga, and Amur) within southern East Siberia are characterized by weak gully dissection, and by a very uneven distribution of gullies.The varied natural conditions, combined with anthropogenic impacts, produce a highly mosaic pattern in the spatial distribution of gullies.For the last 230-300 years, four intensification stages of gully erosion were identified, which were associated with periods of abrupt changes in nature management.The growth rates of the gully heads in different areas of southern East Siberia vary from 0.1 to 26 m yr-1, the mean long-term linear growth rates of gullies are 0.5–2.5 m yr-1.Extreme meteorological phenomena: torrential rains (over 30 mm hr-1), abundant rains (over 50 mm day-1), and rapid snow thawing in the spring are responsible for gullying.
Czasopismo
Rocznik
Tom
Strony
155--159
Opis fizyczny
Bibliogr. 15 poz., rys.
Twórcy
autor
Bibliografia
  • Batuyev B.D., 1976. Formation and development of gullies on loessal rocks along the valleys of the Tarbagataika and Kuitunka rivers. Trudy geologicheskogo institute BF SO AN SSSR. 6 (14):101–108.
  • Bazhenova O.I., Lyubtsova E.M., Ryzhov Yu.V. & Makarov S.A., 1997.Spatio-temporal analysis of the dynamics of erosion processes in southern East Siberia. Nauka.Siberian Enterprise RAS Novosibirsk, 208 pp.
  • Golosov V.N., Kozlovskaya M.E. & Patsukevich Z.V., 1996. The specific character of the erosion processes in the Southwestern Transbaikalia. Vestnik Moskovskogo gosudarstvennogo universiteta. Seriya 5. Geografiya 4: 91–97.
  • Yurij V. Ryzhov, Dmitrij V. KobylkinIvanov A.D. & Budayev Kh.R., 1974. Gully erosion within the Lake Baikal watershed basin.In: Korobtsev, I.I. (ed.) Soils of the Lake Baikal watershed basin and the avenues for their rational utilization. Ulan-Ude: 171–183.
  • Kosov B.F. & Konstantinova G.S., 1972. Zoning of the USSR territory according to the density of the gully network. Vestnik Moskovskogo gosudarstvennogo universiteta. Seriya 5. Geografiya, 3: 32–38.
  • Kosov B.F. & Konstantinova G.S., 1972. Zoning of the USSR territory according to the gully density. Soil Erosion and Stream Channel Processes, Issue 4: 15–25.
  • Litvin L.F., 2002.The geography of soil erosion of agricultural lands of Russia. IKTs Akademkniga, Moscow, 255 pp.
  • Mironova E.A., 1971. Gullying of the USSR territory. Geomorfologiya 3: 25–35.
  • Nezhikhovsky R.A., 1971.The channel networkof the basin and the formation process of water runoff. Gidrometeoizdat, Leningrad: 476 pp.
  • Reimkhe V.V., 1986. Erosion processes in forest-steppe landscapes of the Transbaikalia (exemplified by the Kuitunka river basin). Nauka,Novosibirsk, 120 pp.
  • Ryzhov Yu.V., 2003. Assessing the current gully erosion in southern East Siberia. Izvestiya Russkogo geograficheskogo obshchestva 135: 70–77.
  • Ryzhov Yu.V., 2009. The occurrence of gullies in southern east siberia. Geomorfologiya 1: 5–93.
  • Salyukova R.I., 1976. Gullies of the Southern Minusinskaya depression. Sibirsky geografichesky sbornik 12: 183–222.
  • Vasiliev N.M., Tulokhonov A.K. & Voloshin A.L., 1988.The gullying dynamics in the Selenginskoye middle mountains (as deduced from historical-cartographic data). Geomorfologiya 4: 44–49.
  • Zulyar Yu.A., 2002.Studies on nature management in the Baikal region during the 20th century.Izdatelstvo Irkutskogo gosudartsvennogo universiteta, Irkutsk, 496 pp.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ5-0052-0006
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