Abstract
To investigate the interconnection of the Sava, Sava Lake, and ranney wells waters, the method of enviromental isotopes was used. This involved the measurement of tritium concentrations and oxygen and hydrogen stable isotope ratios. Starting from the generally accepted simple hydrogeological aquifer model which supposes that the two water components contribute to the pumped ranney wells water, the water sampling was done from the Sava, the Sava Lake, and properly selected ranney wells R-2, R-4, R-8, and R-18, from December 1975 to October 1976. As a representative sampling site of the backside groundwater reservoir, a deep back positioned well was chosen. The dates of sampling corresponded to the high and low water levels of the Sava. The tritium data indicated that the concentration in the pumped ranney wells water followed relatively closely the concentration in the Sava and the Sava Lake water with a time delay of less than 10 days. From the analyzed correlation data on oxygen and hydrogen stable isotope ratios, the participation of the backside aquifer groundwater in R-2, R-4, and R-18 was less than 10% and in R-8 between 20 and 30%.
Boreli, F;
[1]
Hadzisehovic, M;
Stojakovic, R;
Paligoric, D;
Vukmirovic, Z;
Lazarevic, V
[2]
- Belgrade Univ. (Yugoslavia). Elektrotehnicki Fakultet
- Institut za Nuklearne Nauke Boris Kidric, Belgrade (Yugoslavia)
Citation Formats
Boreli, F, Hadzisehovic, M, Stojakovic, R, Paligoric, D, Vukmirovic, Z, and Lazarevic, V.
Influence of water pollution of the Sava River on the ranney wells in Beograd.
Yugoslavia: N. p.,
1977.
Web.
Boreli, F, Hadzisehovic, M, Stojakovic, R, Paligoric, D, Vukmirovic, Z, & Lazarevic, V.
Influence of water pollution of the Sava River on the ranney wells in Beograd.
Yugoslavia.
Boreli, F, Hadzisehovic, M, Stojakovic, R, Paligoric, D, Vukmirovic, Z, and Lazarevic, V.
1977.
"Influence of water pollution of the Sava River on the ranney wells in Beograd."
Yugoslavia.
@misc{etde_6632468,
title = {Influence of water pollution of the Sava River on the ranney wells in Beograd}
author = {Boreli, F, Hadzisehovic, M, Stojakovic, R, Paligoric, D, Vukmirovic, Z, and Lazarevic, V}
abstractNote = {To investigate the interconnection of the Sava, Sava Lake, and ranney wells waters, the method of enviromental isotopes was used. This involved the measurement of tritium concentrations and oxygen and hydrogen stable isotope ratios. Starting from the generally accepted simple hydrogeological aquifer model which supposes that the two water components contribute to the pumped ranney wells water, the water sampling was done from the Sava, the Sava Lake, and properly selected ranney wells R-2, R-4, R-8, and R-18, from December 1975 to October 1976. As a representative sampling site of the backside groundwater reservoir, a deep back positioned well was chosen. The dates of sampling corresponded to the high and low water levels of the Sava. The tritium data indicated that the concentration in the pumped ranney wells water followed relatively closely the concentration in the Sava and the Sava Lake water with a time delay of less than 10 days. From the analyzed correlation data on oxygen and hydrogen stable isotope ratios, the participation of the backside aquifer groundwater in R-2, R-4, and R-18 was less than 10% and in R-8 between 20 and 30%.}
journal = []
volume = {16}
journal type = {AC}
place = {Yugoslavia}
year = {1977}
month = {Jan}
}
title = {Influence of water pollution of the Sava River on the ranney wells in Beograd}
author = {Boreli, F, Hadzisehovic, M, Stojakovic, R, Paligoric, D, Vukmirovic, Z, and Lazarevic, V}
abstractNote = {To investigate the interconnection of the Sava, Sava Lake, and ranney wells waters, the method of enviromental isotopes was used. This involved the measurement of tritium concentrations and oxygen and hydrogen stable isotope ratios. Starting from the generally accepted simple hydrogeological aquifer model which supposes that the two water components contribute to the pumped ranney wells water, the water sampling was done from the Sava, the Sava Lake, and properly selected ranney wells R-2, R-4, R-8, and R-18, from December 1975 to October 1976. As a representative sampling site of the backside groundwater reservoir, a deep back positioned well was chosen. The dates of sampling corresponded to the high and low water levels of the Sava. The tritium data indicated that the concentration in the pumped ranney wells water followed relatively closely the concentration in the Sava and the Sava Lake water with a time delay of less than 10 days. From the analyzed correlation data on oxygen and hydrogen stable isotope ratios, the participation of the backside aquifer groundwater in R-2, R-4, and R-18 was less than 10% and in R-8 between 20 and 30%.}
journal = []
volume = {16}
journal type = {AC}
place = {Yugoslavia}
year = {1977}
month = {Jan}
}