The silt carrying in the upper part of Jerma river basin in amount of 82.3 t/km/year is relatively high, considering the situation in all Serbia. The specific silt carrying in the upper part of Crnica river basin is 23.9 t/km/year (Manojlović P.), while it is even lower in the basin of Crni Timok river (3.5 t/km/year; Manojlović P, Gavrilović Lj. 1991.). In the Kolubara river basin, the specific mechanical water erosion is between 4.6 t/km/year (Gradac) and 73.2 t/km/year in Tamnava basin (Dragicevic S. 2002). Greater erosion in the upper part of Jerma river basin is result of great part of metamorphic stones that intensively disintegrates and significant anthropogenic influence in Znepolje. The great slopes at the left side of the basin, under the Ruj mountain, should be considered, too. That doesn't mean that the erosion is strong, because, for example in the basin of Beli Timok, between Knjaževac and Zaječar, it is 186 t/km/year. Following regression, base on flow and silt concentra...tion values can calculate the silt carrying very precisely: t/day=6251+26875 - C+1058 - Q Based on beta coefficients (0.73 for silt and 0.31 for flow) it could be concluded that concentration of silt has greater influence on erosion, than flow. More interesting is the influence of seasonal factor on the carrying of suspended silt. Months with the highest amount of carried suspended material are March, April and May. During these months 50.5 % of average yearly value is evacuated from a basin. Similar excessivity has been noticed in the other basins (Dragicevic S. 2002), only in other months.
U slivu Jerme, do profila Trnski Odorovci, specifični pronos nanosa iznosi 82,3 t/km2/god. Pojedinih godina je izrazito visok (1969. godine iz sliva izneto 267.504 t silta ili 480,0 t/km2/god), dok je drugih godina veoma mali (1979. godine samo 10,4 t/km2/god). S druge strane, sezonska razlika kako u koncentraciji silta, tako i u iznosu erozije, veoma je izrazita. Dakle, kompleksni uticaj svih fizičko geografskih faktora, ima veliki uticaj na sezonski ritam pronosa i koncentracije silta. Najerodibliniji su zimski i prolećni meseci.
Keywords:
discharge / silt / erosion / Jerma / Serbia / proticaj / silt / erozija / Jerma / Srbija
Source:
Glasnik Srpskog geografskog društva, 2003, 83, 2, 3-10
TY - JOUR
AU - Manojlović, Predrag
AU - Mustafić, Sanja
AU - Dragićević, Slavoljub
PY - 2003
UR - https://gery.gef.bg.ac.rs/handle/123456789/64
AB - The silt carrying in the upper part of Jerma river basin in amount of 82.3 t/km/year is relatively high, considering the situation in all Serbia. The specific silt carrying in the upper part of Crnica river basin is 23.9 t/km/year (Manojlović P.), while it is even lower in the basin of Crni Timok river (3.5 t/km/year; Manojlović P, Gavrilović Lj. 1991.). In the Kolubara river basin, the specific mechanical water erosion is between 4.6 t/km/year (Gradac) and 73.2 t/km/year in Tamnava basin (Dragicevic S. 2002). Greater erosion in the upper part of Jerma river basin is result of great part of metamorphic stones that intensively disintegrates and significant anthropogenic influence in Znepolje. The great slopes at the left side of the basin, under the Ruj mountain, should be considered, too. That doesn't mean that the erosion is strong, because, for example in the basin of Beli Timok, between Knjaževac and Zaječar, it is 186 t/km/year. Following regression, base on flow and silt concentration values can calculate the silt carrying very precisely: t/day=6251+26875 - C+1058 - Q Based on beta coefficients (0.73 for silt and 0.31 for flow) it could be concluded that concentration of silt has greater influence on erosion, than flow. More interesting is the influence of seasonal factor on the carrying of suspended silt. Months with the highest amount of carried suspended material are March, April and May. During these months 50.5 % of average yearly value is evacuated from a basin. Similar excessivity has been noticed in the other basins (Dragicevic S. 2002), only in other months.
AB - U slivu Jerme, do profila Trnski Odorovci, specifični pronos nanosa iznosi 82,3 t/km2/god. Pojedinih godina je izrazito visok (1969. godine iz sliva izneto 267.504 t silta ili 480,0 t/km2/god), dok je drugih godina veoma mali (1979. godine samo 10,4 t/km2/god). S druge strane, sezonska razlika kako u koncentraciji silta, tako i u iznosu erozije, veoma je izrazita. Dakle, kompleksni uticaj svih fizičko geografskih faktora, ima veliki uticaj na sezonski ritam pronosa i koncentracije silta. Najerodibliniji su zimski i prolećni meseci.
PB - Srpsko geografsko društvo, Beograd
T2 - Glasnik Srpskog geografskog društva
T1 - The silt carrying in Jerma river basin
T1 - Pronos silta u slivu Jerme
VL - 83
IS - 2
SP - 3
EP - 10
UR - conv_80
ER -
@article{
author = "Manojlović, Predrag and Mustafić, Sanja and Dragićević, Slavoljub",
year = "2003",
abstract = "The silt carrying in the upper part of Jerma river basin in amount of 82.3 t/km/year is relatively high, considering the situation in all Serbia. The specific silt carrying in the upper part of Crnica river basin is 23.9 t/km/year (Manojlović P.), while it is even lower in the basin of Crni Timok river (3.5 t/km/year; Manojlović P, Gavrilović Lj. 1991.). In the Kolubara river basin, the specific mechanical water erosion is between 4.6 t/km/year (Gradac) and 73.2 t/km/year in Tamnava basin (Dragicevic S. 2002). Greater erosion in the upper part of Jerma river basin is result of great part of metamorphic stones that intensively disintegrates and significant anthropogenic influence in Znepolje. The great slopes at the left side of the basin, under the Ruj mountain, should be considered, too. That doesn't mean that the erosion is strong, because, for example in the basin of Beli Timok, between Knjaževac and Zaječar, it is 186 t/km/year. Following regression, base on flow and silt concentration values can calculate the silt carrying very precisely: t/day=6251+26875 - C+1058 - Q Based on beta coefficients (0.73 for silt and 0.31 for flow) it could be concluded that concentration of silt has greater influence on erosion, than flow. More interesting is the influence of seasonal factor on the carrying of suspended silt. Months with the highest amount of carried suspended material are March, April and May. During these months 50.5 % of average yearly value is evacuated from a basin. Similar excessivity has been noticed in the other basins (Dragicevic S. 2002), only in other months., U slivu Jerme, do profila Trnski Odorovci, specifični pronos nanosa iznosi 82,3 t/km2/god. Pojedinih godina je izrazito visok (1969. godine iz sliva izneto 267.504 t silta ili 480,0 t/km2/god), dok je drugih godina veoma mali (1979. godine samo 10,4 t/km2/god). S druge strane, sezonska razlika kako u koncentraciji silta, tako i u iznosu erozije, veoma je izrazita. Dakle, kompleksni uticaj svih fizičko geografskih faktora, ima veliki uticaj na sezonski ritam pronosa i koncentracije silta. Najerodibliniji su zimski i prolećni meseci.",
publisher = "Srpsko geografsko društvo, Beograd",
journal = "Glasnik Srpskog geografskog društva",
title = "The silt carrying in Jerma river basin, Pronos silta u slivu Jerme",
volume = "83",
number = "2",
pages = "3-10",
url = "conv_80"
}
Manojlović, P., Mustafić, S.,& Dragićević, S.. (2003). The silt carrying in Jerma river basin. in Glasnik Srpskog geografskog društva
Srpsko geografsko društvo, Beograd., 83(2), 3-10.
conv_80
Manojlović P, Mustafić S, Dragićević S. The silt carrying in Jerma river basin. in Glasnik Srpskog geografskog društva. 2003;83(2):3-10.
conv_80 .
Manojlović, Predrag, Mustafić, Sanja, Dragićević, Slavoljub, "The silt carrying in Jerma river basin" in Glasnik Srpskog geografskog društva, 83, no. 2 (2003):3-10,
conv_80 .
