TY  - JOUR
AU  - Đukić, Vesna
AU  - Radić, Zoran
PY  - 2016
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/736
AB  - The objective of this study is to perform a sensitivity analysis of the SHETRAN model on the example of the torrential Lukovska River catchment in Serbia. The sensitivity analysis of the model was performed for the following parameters: the vertical saturated hydraulic conductivity of the subsurface soil, the horizontal saturated hydraulic conductivity in the saturated zone, the Strickler roughness coefficients for overland flow and for streams, the available water content in the soil and the erodibility coefficients due to rain and due to overland flow. It can be concluded that the water and sediment discharge are very sensitive to the values of the vertical saturated hydraulic conductivity of the subsurface soil in the range of 0.001 to 0.1 m/day; to the values of the horizontal saturated hydraulic conductivity in the saturated zone in the range of 0.01 to 5 m/day and to the values of the Strickler's coefficients for overland flow and for rivers in the range of 0.1 to 100 m1/3s-1 and 15 to 40 m1/3s, respectively. The sediment concentrations in a flow and sediment discharge are very sensitive to the values of erodibility coefficient due to overland flow in the range of 0.5 to 1.5 mg/m2s and to the values of erodibility coefficient due to rain in the range between 0.1 and 40 J1. The obtained results could be used to simplify the parameter calibration procedure and to facilitate estimation of parameters in ungauged mountainous basins of similar characteristics.
T2  - Water Resources Management
T1  - Sensitivity Analysis of a Physically Based Distributed Model
EP  - 1684
IS  - 5
SP  - 1669
VL  - 30
DO  - 10.1007/s11269-016-1243-8
UR  - conv_1206
ER  - 

@article{
author = "Đukić, Vesna and Radić, Zoran",
year = "2016",
abstract = "The objective of this study is to perform a sensitivity analysis of the SHETRAN model on the example of the torrential Lukovska River catchment in Serbia. The sensitivity analysis of the model was performed for the following parameters: the vertical saturated hydraulic conductivity of the subsurface soil, the horizontal saturated hydraulic conductivity in the saturated zone, the Strickler roughness coefficients for overland flow and for streams, the available water content in the soil and the erodibility coefficients due to rain and due to overland flow. It can be concluded that the water and sediment discharge are very sensitive to the values of the vertical saturated hydraulic conductivity of the subsurface soil in the range of 0.001 to 0.1 m/day; to the values of the horizontal saturated hydraulic conductivity in the saturated zone in the range of 0.01 to 5 m/day and to the values of the Strickler's coefficients for overland flow and for rivers in the range of 0.1 to 100 m1/3s-1 and 15 to 40 m1/3s, respectively. The sediment concentrations in a flow and sediment discharge are very sensitive to the values of erodibility coefficient due to overland flow in the range of 0.5 to 1.5 mg/m2s and to the values of erodibility coefficient due to rain in the range between 0.1 and 40 J1. The obtained results could be used to simplify the parameter calibration procedure and to facilitate estimation of parameters in ungauged mountainous basins of similar characteristics.",
journal = "Water Resources Management",
title = "Sensitivity Analysis of a Physically Based Distributed Model",
pages = "1684-1669",
number = "5",
volume = "30",
doi = "10.1007/s11269-016-1243-8",
url = "conv_1206"
}

Đukić, V.,& Radić, Z.. (2016). Sensitivity Analysis of a Physically Based Distributed Model. in Water Resources Management, 30(5), 1669-1684.
https://doi.org/10.1007/s11269-016-1243-8
conv_1206

Đukić V, Radić Z. Sensitivity Analysis of a Physically Based Distributed Model. in Water Resources Management. 2016;30(5):1669-1684.
doi:10.1007/s11269-016-1243-8
conv_1206 .

Đukić, Vesna, Radić, Zoran, "Sensitivity Analysis of a Physically Based Distributed Model" in Water Resources Management, 30, no. 5 (2016):1669-1684,
https://doi.org/10.1007/s11269-016-1243-8 .,
conv_1206 .

TY  - JOUR
AU  - Đukić, Vesna
AU  - Radić, Zoran
PY  - 2014
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/579
AB  - In the present study the SHETRAN river basin modelling system was used in conjunction with Geographic Information System (GIS) to estimate potential erosion and deposition rates within the catchment and the concentrations of sediment in a flow at the catchment outlet on the example of the 114.31 km(2) mountainous torrential Lukovska River catchment in Serbia. The streams in the Lukovska River catchment are short, steep and often produce hazardous torrential floods as a consequence of strong rainfall of short duration. The soil erosion and sediment discharge were analysed in view of the catchment response to physical characteristics of the catchment. Considering that the most of total annual sediment discharge in watersheds of torrential character is achieved during storm events, the SHETRAN modelling system was calibrated on the example of a storm event in 1986 and validated for three other storm events in 1974, 1976 and 1979. The simulated results of discharges and sediment concentrations at the catchment outlet for both calibration and validation events were compared with the observed data and found to be reasonable. The changes of erosion and deposition rates within the catchment and in the course of time were estimated for the calibration event in 1986. The simulated erosion rates were within the range of 1 to 10.5 t/ha and corresponded to the observed rates of erosion in Europe during extreme rain events. The presented methodology is useful in identifying the erosion vulnerable regions in a catchment where erosion control measures should be implemented.
T2  - Water Resources Management
T1  - GIS Based Estimation of Sediment Discharge and Areas of Soil Erosion and Deposition for the Torrential Lukovska River Catchment in Serbia
EP  - 4581
IS  - 13
SP  - 4567
VL  - 28
DO  - 10.1007/s11269-014-0751-7
UR  - conv_1128
ER  - 

@article{
author = "Đukić, Vesna and Radić, Zoran",
year = "2014",
abstract = "In the present study the SHETRAN river basin modelling system was used in conjunction with Geographic Information System (GIS) to estimate potential erosion and deposition rates within the catchment and the concentrations of sediment in a flow at the catchment outlet on the example of the 114.31 km(2) mountainous torrential Lukovska River catchment in Serbia. The streams in the Lukovska River catchment are short, steep and often produce hazardous torrential floods as a consequence of strong rainfall of short duration. The soil erosion and sediment discharge were analysed in view of the catchment response to physical characteristics of the catchment. Considering that the most of total annual sediment discharge in watersheds of torrential character is achieved during storm events, the SHETRAN modelling system was calibrated on the example of a storm event in 1986 and validated for three other storm events in 1974, 1976 and 1979. The simulated results of discharges and sediment concentrations at the catchment outlet for both calibration and validation events were compared with the observed data and found to be reasonable. The changes of erosion and deposition rates within the catchment and in the course of time were estimated for the calibration event in 1986. The simulated erosion rates were within the range of 1 to 10.5 t/ha and corresponded to the observed rates of erosion in Europe during extreme rain events. The presented methodology is useful in identifying the erosion vulnerable regions in a catchment where erosion control measures should be implemented.",
journal = "Water Resources Management",
title = "GIS Based Estimation of Sediment Discharge and Areas of Soil Erosion and Deposition for the Torrential Lukovska River Catchment in Serbia",
pages = "4581-4567",
number = "13",
volume = "28",
doi = "10.1007/s11269-014-0751-7",
url = "conv_1128"
}

Đukić, V.,& Radić, Z.. (2014). GIS Based Estimation of Sediment Discharge and Areas of Soil Erosion and Deposition for the Torrential Lukovska River Catchment in Serbia. in Water Resources Management, 28(13), 4567-4581.
https://doi.org/10.1007/s11269-014-0751-7
conv_1128

Đukić V, Radić Z. GIS Based Estimation of Sediment Discharge and Areas of Soil Erosion and Deposition for the Torrential Lukovska River Catchment in Serbia. in Water Resources Management. 2014;28(13):4567-4581.
doi:10.1007/s11269-014-0751-7
conv_1128 .

Đukić, Vesna, Radić, Zoran, "GIS Based Estimation of Sediment Discharge and Areas of Soil Erosion and Deposition for the Torrential Lukovska River Catchment in Serbia" in Water Resources Management, 28, no. 13 (2014):4567-4581,
https://doi.org/10.1007/s11269-014-0751-7 .,
conv_1128 .