The ruderal vegetation of the northwestern part of the Podunajská nížina lowland 5.Malvion neglectae

1987 ◽  
Vol 22 (1) ◽  
pp. 1-23 ◽  
Author(s):  
Ladislav Mucina
Keyword(s):  
Northwestern Part ◽  
Ruderal Vegetation

Ruderal vegetation of Baškiria II. Classes Artemisietea vulgaris, Agropyretea repentis, Plantaginetea majoris and Polygono-Artemisietea austriacae

1989 ◽  
Vol 100 (9-10) ◽  
pp. 493-529 ◽  
Author(s):  
B. M. Mirkin ◽  
A. I. Solomešč ◽  
A. R. Išbirdin ◽  
M. T. Sachapov
Keyword(s):  
Ruderal Vegetation

On communities of later succession stages of ruderal vegetation in urban territories of Kursk region

2012 ◽  
pp. 13-24 ◽  
Author(s):  
L. A. Arepieva
Keyword(s):  
Ruderal Vegetation ◽  
Urban Territories ◽  
Kursk Region

The article gives the results of the studies of ru­deral vegetation in urban territories of Kursk region. The characteristic of association Convolvulo arvensis–Elytrigietum repentis Felföldy 1943 is presented, 2 new subassociations are proposed. Communities of the association growing on the slopes of highways and railway embankments, as well as on barren lands are described.

SHORT-TERM DYNAMICS OF THE ANAPA BAY-BAR SHORELINE

2017 ◽  
Author(s):  
Marina Krylenko ◽  
Marina Krylenko ◽  
Alexandr Aleynikov ◽  
Alexandr Aleynikov ◽  
Viacheslav Krylenko ◽  
...  
Keyword(s):  
Black Sea ◽  
Satellite Images ◽  
The Black Sea ◽  
Northwestern Part ◽  
Short Term ◽  
Shoreline Position ◽  
Local Dynamics ◽  
Average Displacement ◽  
Local Erosion

The Anapa bay-bar is located in the northwestern part of the Black Sea. With the goal in mind to determine the short-term dynamics of the Anapa bay-bar we analyzed satellite images from 2003 to the present. Depending on the hydro-lithodynamical situation the shoreline configuration during storm can vary from a rectilinear to sinusoidal forms. There are regions of local erosion or accumulation whose formation is related to the alongshore motion of sediments and dynamics of underwater bars. Comparison of the data on 1965 and 1966 showed that in this period the amplitude of the shoreline position was more than 20 m but average displacement of the shoreline for 13 months was only 0.8 m. This study showed that for the analysis of changes in the shoreline position is necessary to consider the configuration of the coastline at the time of each observation and the local dynamics.

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