Radiological characteristics and investigation of the radioactive equilibrium in the ashes produced in lignite-fired power plants.

Coal- and lignite-fired power plants produce significant amounts of ashes, which are quite often being used as additives in cement and other building materials. In many cases, coal and lignite present high concentrations of naturally occurring radionuclides, such as 238U, 226Ra, 210Pb, 232Th and 40K. During the combustion process, the produced ashes are enriched in the above radionuclides. The different enrichment of the various radionuclides within a radioactive series, such as that of 238U, results in the disturbance of radioactive secular equilibrium. An extensive research project for the determination of the natural radioactivity of lignite and ashes from Greek lignite-fired power plants is in progress in the Nuclear Engineering Department of the National Technical University of Athens (NED-NTUA) since 1983. This paper presents detailed results for the natural radioactivity, the secular radioactive equilibrium disturbance and the radon exhalation rate of the fly-ash collected at the different stages along the emission control system of a lignite-fired power plant as well as of the bottom-ash. From the results obtained so far, it may be concluded that 226Ra radioactivity of fly-ash in some cases exceeds 1 kBq kg(-1), which is much higher than the mean 226Ra radioactivity of surface soils in Greece (25 Bq kg(-1)). Furthermore, the radioactivity of 210Pb in fly-ash may reach 4 kBq kg(-1). These results are interpreted in relation to the physical properties of the investigated nuclides, the temperature in the flue-gas pathway, as well as the fly-ash grain size distribution. It is concluded that towards the coldest parts of the emission control system of the power plant, the radioactivity of some natural nuclides is gradually enhanced, secular radioactive equilibrium is significantly disturbed and the radon exhalation rate tends to increase.

[1]  J. Po,et al.  Emanation coefficients for Rn in sized coal fly ash. , 1985 .

[2]  J. Tadmor Radioactivity from coal-fired power plants: A review , 1986 .

[3]  T. Chu,et al.  Concentrations of radionuclides of size fractionated fly-ash emissions from a thermal power plant using Taiwan coal. , 1992, Journal of radiation research.

[4]  M. Anagnostakis,et al.  An experimental/numerical method for the efficiency calibration of low-energy germanium detectors , 1996 .

[5]  B. Erlandsson,et al.  Radioactivity concentrations in non-nuclear industries , 1996 .

[6]  M. Manolopoulou,et al.  Behavior of natural radionuclides in lignites and fly ashes , 1992 .

[7]  S. E. Simopoulos,et al.  Natural radioactivity releases from lignite power plants in Greece , 1987 .

[8]  M. Anagnostakis,et al.  Building materials radon exhalation rate: ERRICCA intercomparison exercise results. , 2001, The Science of the total environment.

[9]  M. Anagnostakis,et al.  Photon attenuation, natural radioactivity content and radon exhalation rate of building materials. , 2002, Journal of environmental radioactivity.

[10]  Z. Dezső,et al.  Significant radioactive contamination of soil around a coal-fired thermal power plant. , 2002, Journal of environmental radioactivity.

[11]  S. Charalambous,et al.  On the escaping radioactivity from coal power plants (CPP). , 1984, Health physics.

[12]  K. Michailidis,et al.  Mineralogy, geochemistry and physical properties of fly ash from the Megalopolis lignite fields, Peloponnese, Southern Greece , 1996 .

[13]  J. Ondov,et al.  Behavior of natural radionuclides in western coal-fired power plants , 1978 .

[14]  C. R. Cothern,et al.  Radon and Its Decay Products in Indoor Air and Indoor Radon and Its Hazards and Environmental Radon , 1989 .