Abstract <p>The causes of the disturbance of the radioactive equilibrium between long-lived parent <sup>90</sup>Sr and short-lived daughter <sup>90</sup>Y in water and aquatic microbiota of V-2 natural reservoir (Lake Kysyl-Tash), serving as a nuclear facility and a liquid radioactive waste repository, are discussed, and the extent of this disturbance is estimated. A sample of green foam taken from the reservoir surface, containing various phytoplankton species, was used as microbiota. Radiometric measurements with variation of the exposure time and processing of the decay/accumulation curves were performed to determine the <sup>90</sup>Sr and <sup>90</sup>Y activities in water and in the microbiota filtered off using the blue band paper filter. By the moment of sampling, the <sup>90</sup>Y/<sup>90</sup>Sr specific activity ratio was ~0.5 in water and ~50 in microbiota (the contribution of the <sup>90</sup>Y to the total activity of β-emitting nuclides was ~98%), with the <sup>90</sup>Sr and <sup>137</sup>Cs activities making up ~1.5 and ~0.5%, respectively. The specific activity of the most finely dispersed fraction of the microbiota, obtained after filtration, reaches 31 kBq/g, exceeding by a factor of ~20000 the specific activity of <sup>90</sup>Sr in V-2 water. The results obtained should be taken into account when estimating the dose to microbiota.</p>

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Disturbance of the 90Sr–90Y Radioactive Equilibrium in Water and Phytoplankton

  • K. Yu. Mokrov

摘要

Abstract

The causes of the disturbance of the radioactive equilibrium between long-lived parent 90Sr and short-lived daughter 90Y in water and aquatic microbiota of V-2 natural reservoir (Lake Kysyl-Tash), serving as a nuclear facility and a liquid radioactive waste repository, are discussed, and the extent of this disturbance is estimated. A sample of green foam taken from the reservoir surface, containing various phytoplankton species, was used as microbiota. Radiometric measurements with variation of the exposure time and processing of the decay/accumulation curves were performed to determine the 90Sr and 90Y activities in water and in the microbiota filtered off using the blue band paper filter. By the moment of sampling, the 90Y/90Sr specific activity ratio was ~0.5 in water and ~50 in microbiota (the contribution of the 90Y to the total activity of β-emitting nuclides was ~98%), with the 90Sr and 137Cs activities making up ~1.5 and ~0.5%, respectively. The specific activity of the most finely dispersed fraction of the microbiota, obtained after filtration, reaches 31 kBq/g, exceeding by a factor of ~20000 the specific activity of 90Sr in V-2 water. The results obtained should be taken into account when estimating the dose to microbiota.