The concentrations of artificial radionuclides were assessed by using ¹³⁷Cs, which represents the residual contamination in the environment after nuclear weapons tests in the atmosphere, mainly in the 1950s and 1960s, and also the nuclear reactor accident at Chernobyl in 1986. The half-life of ¹³⁷Cs is 30.2 y [8]. Annual average activities in river sediments at the monitored sites ranged from 11.4 to 17.5 Bq/kg, with an average of 14.0 Bq/kg.

Differences in the ¹³⁷Cs concentrations of sediment between the monitored sites correspond to the available information on the distribution in the Czech Republic after the accident at the Chernobyl nuclear reactor [9]. The highest activities of ¹³⁷Cs, with an average of 87.6 Bq/kg and range from 38.9 to 124 Bq/kg, were detected at the Topělec site on the Otava River.

Annual average activities in suspended matter ranged from 16.8 to 31.4 Bq/kg, with an average of 25.0 Bq/kg. The average activity of ¹³⁷Cs in the suspended matter was nearly two times higher than that in river sediments. 

Further, the assessment of ratio of ¹³⁷Cs activities in suspended matter and sediments at individual sites was performed. The ratio ranged from 1 to 36.8, with an average 6.2. The activity of ¹³⁷Cs was higher in suspended matter than in river sediments at all sites.

The data from the basic network were analysed for possible time trends in the ¹³⁷Cs values (Equation (1)). Statistical significance of regression curve was tested by using F-test. Effective half-life was calculated according to Equations (2) and (3) [10,11]:

where a is radionuclide activity in sediments (Bq/kg); λ_eff, effective decay constant of ¹³⁷Cs (1/y); t, time (y); and q, natural logarithm of radionuclide activity in sediments (suspended matter) at the beginning of observation (Bq/kg).

where T_eff is effective half-life of ¹³⁷Cs (y).

where T_eco is ecological half-life of ¹³⁷Cs (y) and T_P is physical half-life of ¹³⁷Cs (y).

The annual average values were used for determining the effective half-life of ¹³⁷Cs in sediments 23.8 y and ecological half-life 112 y (see Figure 2).

The average decrease in the ¹³⁷Cs in sediments exceeds that of the physical half-life (30.2 y). We assume that the quicker reduction of ¹³⁷Cs is caused by natural fluvial and biological processes, and thus that the effective and ecological half-lives are less than the radioactivity decay.

The annual average values of ¹³⁷Cs in suspended matter were used for determining the effective half-life of ¹³⁷Cs in suspended matter 11.4 y and ecological half-life 18.4 y (Figure 2). Observed decrease of ¹³⁷Cs in suspended matter was faster than in sediments.

⁴⁰K is a natural isotope with very long half-life (1.28 × 10⁹ y) (with an abundance of 0.0118%) and classified among the so-called primordial radionuclides (radionuclides which arose with the emergence of the Earth). In the Earth’s crust, it is dispersed homogeneously [8,12]. Observed annual average values ranged from 513 to 605 Bq/kg, with an average of 570 Bq/kg. In the monitoring period, the observed values did not exhibit any significant trend, using Equation (1) (Figure 3).

The results of the monitoring programme in the Czech Republic are in good agreement with the range of ⁴⁰K activities reported in the literature for sediments and suspended matter, which is 500 - 700 Bq/kg [13].

The assessment of ⁴⁰K in suspended matter was not performed.

The isotopes ²²⁶Ra and ²²⁸Ra are among the most representative of the natural decay series of uranium and thorium, with half-lives of 1600 y and 5.7 y, respectively [8].

Development of annual average ²²⁶Ra activities in river sediments and suspended matter for the period 2000-2010 and 2001-2010 respectively is showed in the Figure 4.

Annual average values of ²²⁶Ra in river sediments for the whole territory of Czech Republic ranged from 50.8 to 67.9 Bq/kg, with an average of 60.5 Bq/kg. In the monitoring period 2000-2010, the observed annual average values for basic network did not exhibit any significant trend, using Equation (1).

Annual average values of ²²⁶Ra in suspended matter ranged from 75.5 to 184 Bq/kg, with an average of 120 Bq/kg. In the monitoring period 2001-2010, the observed annual average values were used for determining the effective half-life of ²²⁶Ra in suspended matter 7 y, using Equation (1).

Development of annual average ²²⁸Ra activities in river sediments and suspended matter for the period 2000-2010 and 2001-2010 respectively is showed in the Figure 5.

Anthropogenic pollution of the aquatic environment by ²²⁸Ra is unlikely, because thorium ores are not mined in the Czech Republic.

Annual average values of ²²⁸Ra in river sediments ranged from 40.2 to 53.9 Bq/kg, with an average of 47.2 Bq/kg. In the monitoring period 2000-2010, the observed annual average values of ²²⁸Ra for basic network did not exhibit any significant trend, using Equation (1). 

Annual average values of ²²⁸Ra in suspended matter ranged from 65 to 158 Bq/kg, with an average of 87.9 Bq/kg. In the monitoring period 2001-2010, the observed annual average values were used for determining the effective half-life of ²²⁸Ra in suspended matter 9.7 y, using Equation (1).

Observed values correspond to the natural occurrence of ²²⁸Ra in watercourses.

Activities of ²²⁸Ra in suspended matter are in greater range than activities in sediments. Also decrease of activity of ²²⁸Ra in suspended matter exceeded that of the physical half-life at most sites. This we attribute to presence of parent radionuclide ²³²Th with physical half-life

of 1.4 × 10¹⁰ y [8]. However decrease of activity ²²⁸Ra should be studied in more details.

Additionally was carried out monitoring activity of ²²⁶Ra and ²²⁸Ra in sediments at sites of former uranium (and coal) mining and processing in the period 2006-2008 (extended network). Observed annual average values ²²⁶Ra ranged at these sites from 102 to 133 Bq/kg, with an average of 123 Bq/kg. Observed annual average values of ²²⁸Ra ranged from 42.5 to 54.4 Bq/kg, with an average of 49.8 Bq/kg. While average activity of ²²⁸Ra for extended network was same as that in other (basic network), average activity of ²²⁶Ra was two times greater.

The ratio of ²²⁶Ra and ²²⁸Ra activities in suspended matter and in sediments was assessed. The ratio of ²²⁶Ra activities ranged from 0.3 to 4.6 with an average 1.9. The ratio of ²²⁸Ra activities ranged from 0.7 to 6.9 with an average 2.3. Activity of ²²⁶Ra and ²²⁸Ra was higher in suspended matter in 82 % and 94 % respectively.

Hanslík [14] proposed that it is possible to use the ²²⁶Ra:²²⁸Ra ratio to identify the degree of radionuclide contamination in the environment from uranium ore (and coal) mining activities. The ratio is around 1.0 in natural samples, while in areas affected by uranium ore mining, it is significantly higher. The activity of ²²⁶Ra is increased as a result of contamination, while the activity of ²²⁸Ra corresponds to the natural radium levels. On this basis, Hanslík [14] proposed five classes of river sediment contamination by ²²⁶Ra according to the ²²⁶Ra:²²⁸Ra ratio (see Table 1).

These classes were used for classification of river sediments collected in the individual sites in the period 2000-2010. Results from extended network were included to the assessment too. The numbers of the sites in the individual classes are shown in Figure 6.

In the period 2000-2005 and 2009-2010, most of the sites were classified as class I (84% - 91%), i.e. as uncontaminated. In the period 2006-2008, the inclusion of the sites affected by former mining and processing of

uranium ore has been reflected by an increase in the representation of contaminated classes.

These classes were used also for classification of suspended matter. The numbers of the sites in the individual classes are shown in Figure 7. Most of the sites were classified as class I (from 50% to 100%) too.

The ratio of ²²⁶Ra and ²²⁸Ra activities from 5 selected sites with former uranium mining and processing was in average higher in sediments than in suspended matter. Only at one site was evaluated ratio higher in suspended matter. We think it is because of better conditions of water and stopping of mining and on-going mining water treatment respectively.

The average values were used further to determine natural background levels of radionuclides in the Czech Republic. For ⁴⁰K, the natural background level was estimated to be 570 Bq/kg. To evaluate the background level for ²²⁶Ra, the river sites affected by human activities (mining and processing uranium ore, coal) were eliminated from the assessment, and only river sites falling

into class I were used for the analysis. The average natural background values for ²²⁶Ra and ²²⁸Ra in sediments were essentially identical at 47.8 Bq/kg for ²²⁶Ra and 47.2 for ²²⁸Ra. In suspended matter it was 86.5 Bq/kg for ²²⁶Ra and 87.9 Bq/kg for ²²⁸Ra.The uncertainty of the background values was expressed as the standard deviation.