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2018 | 29 | 4 |

Tytuł artykułu

The mechanical degradation of land surface and the present state of the loess “islands” plant cover of Chernihiv Polesie (Ukraine)

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
The causes of the mechanical degradation of the loess lands of Chernihiv Polesie have been determined, in particular, the ability of the loess to be washed out and subside easily, deforestation (the end of the 13th – the beginning of the 14th centuries) and the excessive increase of the anthropogenic pressure on the agricultural lands (the end of the 19th – the beginning of the 21st centuries). It has been cleared that the degradation of the loess “islands” soils of Chernihiv Polesie is manifested in the form of erosion and suffusion. The areas at the fifth stage of erosion prevail. The largest percentage of the eroded areas is on the Mykhailo-Kotsiubynsk and Ripky-Chernihiv loess “islands”. The lands with suffusion forms dominate on the Berezna-Mena-Sosnytsia loess “island”. Long-term use of the arable lands contributed to the increase of erosion and suffusion forms of the relief. The potential places of the beginning of the mechanical degradation are post-sowing, neglected lands, which were repeatedly violated mechanically. The plant communities, which are the indicators of different stages of mechanical degradation of the lands, have been identified. The plant communities of Digitario sanguinalis-Eragrostietea minoris Mucina, Lososová et Šilc 2016 and Bidentetea Tx. et al. ex von Rochow 1951 are the indicators of eroded lands at the stages of formation, expansion and deepening of washouts. The phytocenoses of Bidentetea tripartiti are the indicators of the initial stages of suffusion, and the complexes of Magnocaricetalia are the indicators of suffusion increase and deepening. Over the past 120 years, there has been a slight increase in the area occupied by plant communities other than agrocenoses on the loess “islands” due to the anti-erosion planting of Pinus sylvestris and Robinia pseudoacacia. The agronomic, fitomeliorative and prohibitive measures that can slow down the pace of the mechanical degradation of the loess lands of Chernihiv Polesie have been suggested.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

29

Numer

4

Opis fizyczny

p.23-34,fig.,ref.

Twórcy

autor
  • Department of Ecology and Nature Conservation, T. Shevchenko National University “Chernihiv Collegium”, Hetman Polubotko 53 St, 14013 Chernihiv, Ukraine
autor
  • Department of Ecology and Nature Conservation, T. Shevchenko National University “Chernihiv Collegium”, Hetman Polubotko 53 St, 14013 Chernihiv, Ukraine
autor
  • Department of Languages and Methodology, T. Shevchenko National University “Chernihiv Collegium”, Hetman Polubotko 53 St, 14013 Chernihiv, Ukraine

Bibliografia

  • Akhromeiev L.M., 2008, The nature, genesis, history of the development and landscape structure of the high plains of Central Russia. Publishing house of BSU, Briansk.
  • Atlas of environmental conditions and natural resources of Ukrainian SSR, Main administration of geodesy and cartography at Council of ministers of the USSR, Moscow: 74-75.
  • Baliuk S.A. & Tovazhnianskyi L.L., 2010, Scientific and Applied Bases of Soil Protection from Erosion in Ukraine. Publishing house of National Technical University of KhPI, Kharkiv.
  • Bezdukhov O.A., 2013, Influence of agricultural land use of Chernihiv region on the development of crisis ecological and geomorphological situations. Physical Geography and Geomorphology 4(11): 72-81. [http://nbuv.gov.ua/UJRN/fiz_geo_2013_4_11].
  • Budko O.S., 2009, The loess “islands” of Zhytomyr and Volyn Polesie : regional problems of landscape science and geomorphology. Physical Geography and Geomorphology 56: 178-184.
  • Lanko A.I., 1958, On some geomorphological pequliarities of the Left Bank Polesie of the Ukrainian SSR. Bulletin of Kiev University: a series of geology and geography 1 (1): 93-102.
  • Korchahin A.A., 2012, Field geobotany. Methodical guidance. E.M. Lavrenko (ed.), PH Ozon.ru, Moscow.
  • Marynych A.M., Parkhomenko H.O., Petrenko O.M. & Shyshenko P.H., 2003, Improved scheme of physico-geographical zoning of Ukraine. Ukrainian Geographic Journal 1(41): 21-32.
  • Milkov F.N., 1964, On the nature of the high plains on the Russian plain. Questions of Regional Landscape Science and Geomorphology of the USSR 8: 20-27.
  • Matuszkiewicz W., 2001, Przewodnik do oznaczania zbiorowisk roślinnych Polski [Guide for determination of Polish plant communities]. Wydawnictwo Naukowe PWN, Warszawa.
  • Mucina L., Bültmann H., Dierssen K., Theurillat J.-P., Raus T., Čarni A., Šumberová K., Willner W., Dengler J., García R.G., Chytrý M., Hájek M., Di Pietro R., Iakushenko D., Pallas J. Daniëls F.J.A., Bergmeier E., Guerra A.S., Ermakov N., Valachovič M., Schaminée J.H.J., Lysenko T., Didukh Y.P., Pignatti S., Rodwell J.S., Capelo J., Weber H.E., Solomeshch A., Dimopoulos P., Aguiar C., Hennekens S.M. & Tichý L., 2016, Vegetation of Europe: hierarchical floristic classification system of vascular plant, bryophyte, lichen, and algal communities. Applied Vegetation Science 19(S1): 3-264. (https://onlinelibrary.wiley.com/doi/epdf/10.1111/avsc.12257).
  • Pashkevych H.A., 1971, The history of vegetation of Chernigov Polesie in the late- and post-glacial time by the data of the spore-pollen analysis, Problems of palynology, International palynolongical conference. Academy of Sciences of the Ukrainian SSR, Kiev: 188-199.
  • Schubert F.F. & Tuchkov P.A., 1916, Military-topographic map of Russian Empire, Row XX, Moscow: 9-10. (htpp: //www.clubclad.ru/maps/) [Accessed 20 April 2016].
  • Solomakha V.A., Kostylov O.V. & Sheliah-Sosonko Yu.R., 1992, Synanthropic vegetation of Ukraine. Scientific thought, Kyiv.
  • Veremeichyk O.M., 2010, Results and prospects of archaeological researches of village settlements of Chernihiv Polesie. Archeology and Ancient History of Ukraine 1(3): 209-215.
  • Zhekulin V.S., 1982, Historical geography: object and methods. PH Science, Leningrad.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

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