scholarly journals Chemical erosion intensity in the Nisava catchments

2002 ◽  
Vol 82 (1) ◽  
pp. 3-8 ◽  
Author(s):  
Predrag Manojlovic
Keyword(s):  
Water Erosion ◽  
Chemical Erosion ◽  
Geographical Characteristics ◽  
Erosion Intensity

The Nisava catchment comprehends the area of 4068 km2. There are differences in erosion intensity due to different physical-geographical characteristics of that area. Mechanical water erosion in the Nisava catchment is 302,4 m3/km2/yr and chemical erosion is 67,2 t/km2/yr. Space differences are large (47,1-115.5 t/km2/yr) and are mostly determined by hydrological and lithological characteristics of that area.

scholarly journals Contribution to the research of the chemical intensity erosion in the western Serbia

2003 ◽  
Vol 83 (1) ◽  
pp. 7-14 ◽  
Author(s):  
Slavoljub Dragicevic ◽  
Predrag Manojlovic ◽  
Sanja Mustafic
Keyword(s):  
Analytical Method ◽  
River Basins ◽  
Meteorological Conditions ◽  
The Other ◽  
Entry And Exit ◽  
Chemical Erosion ◽  
Time Period ◽  
Erosion Intensity

Based on the research of the chemical erosion intensity in the upper course of Tamnava, the appearance of its negative value has been found. Further researches, that enclose the lower course, confirmed this fact. This research opened the important question about the causes of this phenomena. Analytical method eliminated all expected causes and led to conclusion that the reason for this should be found by using the more precise research of the mineralisation of the precipitations. It was necessary to continue the measurings of the precipitation mineralisation in the greater number of locations and in the wider time period, as well as in the different meteorological conditions, and after that to establish the subordination between the amount of precipitations and the entered TDS. Only after these additive researches we could be able to find out the relation between ''entry'' and ''exit'' and to find out the intensity of the chemical erosion in this, and in the other river basins. For now, we are able only to find out the carrying of TDS, as well as the reduction of the chemical evacuation for the non - carbonated part of the basin (corrected value).

scholarly journals REVIEW AND COMPARISON OF WATER EROSION INTENSITY IN THE WESTERN BALKAN AND EU COUNTRIES

2017 ◽  
Vol 36 (1) ◽  
Author(s):  
Ivan Blinkov
Keyword(s):  
Methodological Approach ◽  
Secondary Data ◽  
Water Erosion ◽  
European Level ◽  
Recent Period ◽  
Erosion Risk ◽  
Balkan Countries ◽  
Gis Environment ◽  
National Databases ◽  
Erosion Intensity

The south and southeast region of Europe is significantly prone to water erosion. In parts of the region, erosion has reached a stage of irreversibility and in some places erosion has practically ceased because there is no soil left. In the recent period several models and approaches in a GIS environment were developed using available database for erosion factors on the European level on which data about water erosion in Western Balkan countries is missing. Sci-entists in the Western Balkan countries faced with the erosion problem for years, developed own models or prepared various erosion risk maps using national databases. The aim of this study is to compare results of water erosion inten-sity in the Western Balkan countries using models on wider level (European maps) and national researches. The basic methodological approach in this paper is an analysis of secondary data, using the method of "content analysis" of various data sources. Inductive and deductive qualitative analyses were used and finally the method of "comparative analysis" is applied, too. Through the analysis of national researches it was estimated that erosion intensity in the WB countries is 656 m3/ha (similar to 6.56 t/ha) and the total amount of annual produced erosive material is 373.8·106 m3. The most erosive countries in Europe are Albania and Montenegro where mean annual intensity of erosion is > 10 t/ha. Macedonia together with Italy, Portugal, Slovenia and Romania is in the second group of countries, where ero-sion intensity is 5–10 t/ha.

scholarly journals The Balkans - the most erosive part of Europe?

2015 ◽  
pp. 9-20 ◽  
Author(s):  
Ivan Blinkov
Keyword(s):  
Soil Erosion ◽  
Methodological Approach ◽  
Secondary Data ◽  
Water Erosion ◽  
Geological Time ◽  
The Balkans ◽  
Balkan Countries ◽  
The Mean ◽  
Soil Erosion By Water ◽  
Erosion Intensity

Soil erosion has been occurring over the geological time. Inappropriate human activities accelerate this process. Soil erosion by water is a widespread problem throughout Europe. The South and Southeast regions of Europe are significantly prone to water erosion. In parts of the region, erosion has reached a stage of irreversibility and in some places erosion has practically ceased because there is no soil left. Scientists from the Balkan countries faced with the erosion problem for years, paid significant attention to solving problems with erosion. The aim of this study is to compare the results of water erosion intensity in the Balkan countries with other European countries. The basic methodological approach in this paper is an analysis of secondary data, using the method of ?content analyses? of various data sources. Inductive and deductive qualitative analysis was used and finally the method of ?comparative analysis? is applied too. Through the analysis of national researches, it was estimated that erosion intensity in Balkan countries is 548 m3km-2 (similar to 5.48 tha-1) and the total amount of annual produced erosive material is 419.9 *106 m3. The mean European average annual erosion intensity is 3.13tha-1. The most erosive countries in Europe are the Balkan countries, Albania and Montenegro where the mean annual intensity of erosion is > 10 tha-1.

Biological and geographical characteristics Lavandula latifolia Medik.

2020 ◽  
Author(s):  
M.Yu. Cherednichenko M.Yu. ◽  
◽  
A.S. Elenchuk A.S.
Keyword(s):  
Geographical Distribution ◽  
Common Species ◽  
Flower Morphology ◽  
Lavandula Latifolia ◽  
Geographical Characteristics

The article presents the characteristics of the geographical distribution of broadleaved lavender, as well as the features of the flower morphology of this species in comparison with other common species of the genus.

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