An approximation for estimating Compton scatter from a cuboid phantom.

The Kadji-Sai abandoned field of U-bearing brown coal on the southern coast of Lake Issyk-Kul (Kyrgyzstan) poses a threat of radioactive pollution to the world's fifth deepest and second largest pristine highland lake. The valleys of ephemeral streams in the lake catchment are filled with coarse-grained sand and clay, with a background U--Ra activity of 35--55 Bqkg(-1). High activity areas vs. this background come from three sources: (1) scarce outcrops of uraniferous brown coal and mining wastes containing fragments of this coal with (238)U/(226)Ra ratios of 0.8 due to uranium losses through weathering; (2) manmade anomalies caused by a radioactive waste dump, where U was extracted from the ash of coal burnt at a coal-fired power plant. As a result, the (238)U/(226)Ra ratios become 0.15--0.25; (3) six catch pools terraced below the mine, where U activity decreases downslope, and (238)U/(226)Ra ratios reach 150--200. Uranium lost in the extraction process may have been retained on the terraces. The distribution pattern of radionuclides in the bottom sediments of the lake is controlled by water depth and offshore distance. The upper section of homogeneous limy--argillic deposits in the lake center remains undisturbed by currents, as indicated by regular sub-exponential distribution of atmospheric (137)Cs and (210)Pb(atm). Sedimentation rate in the lake center for the past century, found from (210)Pb, was 0.32 mmyr(-1). (238)U/(226)Ra in deep-water sediments was about 3. The activity of uranium adsorbed by sediments from the lake water was estimated by subtraction of the Ra-equilibrium component from the total U activity. Thus, the flux of dissolved U to the bottom sediments was as 2.07 x 10(-7)gcm(-2)yr(-1). The upper section of near-shore deposits was disturbed by currents, with (137)Cs and (210)Pb(atm) more or less uniformly distributed in this layer. Peaks of (226)Ra and (210)Pb occur at different depths from 5 to 20 cm below the sediment surface, with (238)U/(226)Ra ratios 0.28--0.44. The presence of mullite in these sediments indicated that radioactive ash penetrated into the lake in the past. At present, (226)Ra in the ash is buried under a non-radioactive cap.

Cesium Isotopes↗

PubMed2002

Dating of marine sediments and time evolution of heavy metal concentrations in the Bay of Cádiz, Spain.

In this paper the time evolution of heavy metal concentration of Pb, Zn, Cd and Hg, in the sediments of the Bay of Cádiz (southwest of Spain) is studied during the past century, as a result of the industrial influence in the zone. The study has been performed using sedimentary profiles that have been extracted from the seabed. The measurement of 210Pb and 137Cs radionuclides has provided the dating of the sediment layers, up to a depth corresponding to the age of 115 years. The relative sedimentation rates obtained are around 0.2 cm/year. The 137Cs activity profile reflects the concentration of this radionuclide in the atmosphere and into aquatic systems during the second half of the twentieth century. This profile has been used to ratify the results provided by the 210Pb dating method.

Cesium Isotopes↗

PubMed1975

Gamma-ray-induced thymine damage in the DNA in coliphage phi chi 174 and in E. coli.

The radiation chemical reactivity of thymine residues has been compared for single-stranded phi chi 174 DNA free in solution and in the intact bacteriophage, as well as for native E. coli DNA in solution and inside the cell. The gamma-ray-induced release of [3H]H2O from thymine-methyl[3H] was measured to assess the reactivity of the thymine methyl group. Formation of ring-saturated products of the 5,6-dihydroxy-dihydrothymine type (see article) was determined by an alkali-acid degradation assay. It was observed that the formation of that the formation of [3H]H2O was suppressed by a factor of 9 in intact phi chi 174 bacteriophage compared to phi chi 174 DNA, whereas the formation of (see article) was only slightly suppressed in the phage. For E. coli cells the formation of [3H]H29 was reduced 790-fold compared with free E. coli DNA, and (see article) formation was reduced 140-fold. The extents of survival after gamma-irradiation of phi chi 174 phage plaque-forming ability and E. coli colony-forming ability were also determined. Under the conditions used in these experiments, a linear relationship was observed between the loss of biological activity and the formation of thymine damage for both phi chi 174 phage and E. coli cells.

Cesium Isotopes↗