Stefana Babović1, Miodrag Zlatić2, Stanimir Kostadinov2

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Presentation transcript:

Stefana Babović1, Miodrag Zlatić2, Stanimir Kostadinov2 SOCIO-ECONOMIC INFLUENCE ON THE SOIL EROSION INTENSITY IN THE PANEVLJANSKA RIVER WATERSHED Stefana Babović1, Miodrag Zlatić2, Stanimir Kostadinov2 1Geographical Institute “Jovan Cvijić” Serbian Academy of Sciences and Arts, s.babovic@gi.sanu.ac.rs 2Department of Ecological Engineering for Soil and Water Resources Protection, Faculty of Forestry, University of Belgrade miodrag.zlatic@sfb.bg.ac.rs, stanimir.kostadinov@sfb.bg.sc.rs  

Introduction Soil erosion is one of the major natural hazards in the world, causing soil degradation (Mircea et al. 2015). Every year, 75 billion tons, of mainly arable land in the world, are being taken away due to erosion. Viewed spatially, this represents a loss of 20 million hectares in total (Ananda and Herath 2003).

Introduction On average, each kilometer of the Grdelica Gorge is threatened by five torrential flows and there are 143 of them (Gavrilovic, 1957; Kostadinov and Markovic, 1957).

The aim is… men illegal forest cutting on steep slopes depopulation trimming of leafy branches for winter cattle forage tillage down the slope depopulation erosion and torrent control works soil erosion intensity

Study Area the average annual temperature is 11.1 oC the lowest average monthly temperature is in January 0.1 oC the highest average monthly temperature is in August 21.6 oC the average annual precipitation is 567.7 mm the month of minimum precipitation is January 35.4 mm maximum precipitation is July 63.2 mm Main characteristics of the Panevljanska River watershed Perimeter(km) 11.2 Watershed area(km2) 3.82 Main stream length (km) 5.04 Stream bed slope (%) 9.82 Watershed length (km) 4.74

Land use Present state 1. broad-leaved forest (53.6%) Institute for Agricultural Economics in Belgrade carried out a research in the Grdelica Gorge and Vranjska valley, in the time period 1956-1959. Agriculture was undeveloped at that time, poor technically equipped; in the hilly and mountainous areas people were engaged in farming, at the expense of forests (Zlatić 2010). During the period 1959-1983 orchards and vineyards areas increased. The similar situation is with meadows – these areas increased from 3.5% to 14.8% in 24 years’ time period. Present state 1. broad-leaved forest (53.6%) 2. complex cultivation patterns (38%), 3. land principally occupied by agriculture with significant areas of natural vegetation (8.4%).

agricultural inhabitants % active inhabitants agricultural inhabitants

Municipality Vranjska Banja 43 of age 52 of age average population age The number of cattle and pigs decreased until 2002, and then increased in the last inter-census period, especially increased the number of pigs.

Methods Average annual sediment transport (total sediment) is calculated by the Polyakov-Kostadinov method: Population and agriculture data were taken from publications of the Statistical Office of the Republic of Serbia. Statistical data analysis was performed by program Statgraphics XVII.

1531 m3/km2/year One of the main causes for the current state of soil erosion is derived biological works in the watershed. Prior to afforestation in 1959, mainly degraded forests occupied 23.2% of the total area. After afforestation, the forests occupied 39.4% of the total areas. 555 413 Causes of the emigration are: low income, then life conditions such as small houses made of bad material, missing sewerage system, bad traffic connection to local municipalities, changes in socio-economic issues regarding to rural – urban relation, etc. (Zlatić 1985; Dragićević et al. 2014).  

Statistical analysis agricultural inhabitants number of livestock arable land number of livestock agricultural inhabitants Statistical analysis average annual sediment transport inhabitants active inhabitants Gyear = 600.87 + 0.42*AgI + 0.12*NL – 2.88*AL Where are: Gyear – average annual sediment transport AgI – agricultural inhabitants NL – Number of livestock AL – arable land

Conclusion The Panevljanska River watershed was characteristic for occurrence of all erosion phenomena, with the state of accelerated erosion in mid-fifties of the twenty century, endangering roads and railway, villages, human lives. The population was constantly decreasing in recent decades, which led to the abandonment of agricultural land, so they are today largely unused. These processes, together with a number of erosion and torrent control works contributed to the reduction of erosion. Average annual sediment transport reduced from 1,531 m3*km-2*year-1 (1953) to 413 m3*km-2*year-1 (2015) and intensity of erosion reduced from excessive to weak.