were measured using alpha spectrometry. In winter, the highest concentration of uranium isotopes and total uranium was in the Vistula River water from Malbork (13.13 ± 0.22 Bq m −3 for 234 U, 12.45 ± 0.21 Bq m −3 for 238 U and 1.02 ± 0.30 mg m −3 for total uranium), and the lowest was in water from Dȩblin (1.73 ± 0.07 Bq m −3 for 234 U, 1.55 ± 0.07 Bq m −3 for 238 U and 0.13 ± 0.09 mg m −3 for total uranium). In analyzed river samples uranium isotopes 234 U and 238 U are not in the radioactive equilibrium state. The values of 234 U/ 238 U activity ratio lie between 1.05-1.70. During spring, the highest concentration of uranium isotopes and total uranium was found in the Vistula River water from Malbork (12.36 ± 0.19 Bq m −3 for 234 U, 10.77 ± 0.17 Bq m −3 for 238 U and 0.88 ± 0.25 mg m −3 for total uranium), and the lowest was in water taken from Sandomierz (5.77 ± 0.14 Bq m −3 for 234 U) and Kraków (4.08 ± 0.11 Bq m −3 for 238 U and 0.33 ± 0.18 mg m −3 for total uranium). The values of 234 U/ 238 U activity ratio lie between 1.15-1.64. In summer, the highest concentration of uranium isotopes and total uranium was found in the Vistula River water samples taken from Malbork (8.22 ± 0.21 Bq m −3 for 234 U, 7.60 ± 0.21 Bq m −3 for 238 U and 0.62 ± 0.29 mg m −3 for total uranium), and the lowest was in water from Sandomierz (6.37 ± 0.12 Bq m −3 for 234 U) and Kraków (3.56 ± 0.19 Bq m −3 for 238 U and 0.29 ± 0.33 mg m −3 for total uranium). The values of 234 U/ 238 U activity ratio lie between 1.08-1.95. In autumn the highest concentration of uranium isotopes and total uranium was in the Vistula River water from Malbork (17.80 ± 0.25 Bq m −3 for 234 U, 15.12 ± 0.23 Bq m −3 for 238 U and 1.23 ± 0.34 mg m −3 for total uranium) and the lowest was in water from Toruń (8.15 ± 0.49 Bq m −3 for 234 U) and Kraków (6.34 ± 0.47 Bq m −3 for 238 U and 0.52 ± 0.78 mg m −3 for total uranium). The values of 234 U/ 238 U activity ratio lie between 1.10-1.74. Annually, the southern Baltic Sea is enriched by about 507 GBq uranium isotopes 234 U and 238 U, with 490 GBq going to the Gdańsk Bay and 16.5 GBq to Vistula Lagoon. The highest surface 238 U runoff was observed in spring (to 1200 kBq km −2 quarter −1 for catchment's area), the lowest in summer for Bug with Narew catchment's area to 20 kBq km −2 quarter −1 ). These studies are very important