Various types of mineral and drinking waters have been tested for the simultaneous determination of 226Ra and 22SRa using 3M's EMPORE TM Radium Rad Disks. Both r adionuclides 226Ra and 228Ra were counted through their daughter products, 226Ra by the conventional radon emanation technique and 22SRa through its daughter 22SAc by using a proportional counter. 0.2 M diammonium hydrogen citrate adjusted by ammonia to pH 7.8 was used for radium stripping from the disk and 3.10 -4 M diammonium hydrogen citrate was used for actinium washing from the disk.

The Slovak Republic is very rich in mineral water sources. In recent years, it has been discovered that a number of mineral waters in the Slovak Republic contain high levels of 226 Ra and 228 Ra. Moreover, there is a lack of information on 224 Ra and 223 Ra concentrations in mineral waters as well. The currently approved techniques for alpha emitting radium isotopes are based on radon emanation methods. Due to the long ingrowth periods required by these techniques, any 224 Ra and 223 Ra in the sample decay away and go undetected. For this reason, we have used an alpha spectrometric method for the simultaneous determination of 226 Ra, 223 Ra and 224 Ra. Radium was concentrated by a lead sulphate co-precipitation. The precipitate was dissolved in EDTA and the radium isotopes were separated from possible interfering radionuclides using barium sulphate micro precipitation. The radium-barium precipitate was filtered and counted by alpha spectrometry. 133 Ba was used to quantify the yield by gamma spectrometry. In our laboratory, gamma spectrometry was also used for the determination of 228 Ra in mineral water samples. Radium was concentrated by a lead-barium sulphate co-precipitation. 133 Ba was used to quantify the yield, found to be 97 % on the average, by gamma spectrometry. Furthermore, the committed effective doses for 226 Ra, 224 Ra, 223 Ra, 228 Ra intake via ingestion of mineral waters for the members of public were calculated. 228 Ra [1,3,4,[6][7][8]. The currently approved methods for alpha emitting radium isotopes are based on radon emanation techniques. Due to the long ingrowth periods required by these methods, any 224 Ra and 223 Ra in the sample decay away and go undetected. For this reason, we used an alpha spectrometric method for the simultaneous determination of 226 Ra, 223 Ra and 224 Ra. In our laboratory, radium-lead-barium sulphate co-precipitation followed by gamma spectrometry was used for the determination of 228 Ra in mineral water samples.

No abstract

The Slovak Republic is very rich in mineral water sources. In recent years, it has been discovered that a number of mineral waters in the Slovak Republic contain high levels of 226 Ra and 228 Ra. Moreover, there is a lack of information on 224 Ra and 223 Ra concentrations in mineral waters as well. The currently approved techniques for alpha emitting radium isotopes are based on radon emanation methods. Due to the long ingrowth periods required by these techniques, any 224 Ra and 223 Ra in the sample decay away and go undetected. For this reason, we have used an alpha spectrometric method for the simultaneous determination of 226 Ra, 223 Ra and 224 Ra. Radium was concentrated by a lead sulphate co-precipitation. The precipitate was dissolved in EDTA and the radium isotopes were separated from possible interfering radionuclides using barium sulphate micro precipitation. The radium-barium precipitate was filtered and counted by alpha spectrometry. 133 Ba was used to quantify the yield by gamma spectrometry. In our laboratory, gamma spectrometry was also used for the determination of 228 Ra in mineral water samples. Radium was concentrated by a lead-barium sulphate co-precipitation. 133 Ba was used to quantify the yield, found to be 97 % on the average, by gamma spectrometry. Furthermore, the committed effective doses for 226 Ra, 224 Ra, 223 Ra, 228 Ra intake via ingestion of mineral waters for the members of public were calculated. 228 Ra [1,3,4,[6][7][8]. The currently approved methods for alpha emitting radium isotopes are based on radon emanation techniques. Due to the long ingrowth periods required by these methods, any 224 Ra and 223 Ra in the sample decay away and go undetected. For this reason, we used an alpha spectrometric method for the simultaneous determination of 226 Ra, 223 Ra and 224 Ra. In our laboratory, radium-lead-barium sulphate co-precipitation followed by gamma spectrometry was used for the determination of 228 Ra in mineral water samples.

Radioecologically the most important radionuclide generated by the Chemobyl accident is 137Cs at present. The actual geographic distribution of the 137Cs concentrations in the soil in Central Slovalda for 1995 is presented. On the basis of measured data the relationships between 137Cs concentration in soil profiles and some local parameters (average precipitation, specific activity of 4~ soil types) was studied. Some problems in the modelling and prediction of 137Cs migration in soils are discussed too. The activity of 137Cs was measured at 45 sites. Approximately 66% of total deposition of 137Cs is in the upper 10 cm of soil.