Radioactive isotopes, both natural and artificial, present in the environment, may be convenient indicators that can be used to study many physical and chemical processes as well as the transport of pollutants in the ecosystem. The studies have shown that in identification of particulate matter emission sources a radioactive lead isotope (Pb-210) can be used. The Pb-210 increased activity concentration in the top soil layers suggests its current atmospheric deposition. This conclusion is confirmed by the results of the Principal Components Analysis, conducted using the measured radionuclide content in 0-30 cm deep soil layer samples.
Keywords: Pb-210, pollutant emission indicator
IntroductionRadioactivity is not only a source of human exposure, but it also has many practical applications. Using the properties of radioactive isotopes, it is possible, for example, to generate electricity, test materials, diagnose and treat people. Radioisotopes are also used in environmental studies [1].Radioactive isotopes are used, inter alia, to study the mechanisms and dynamics of the processes in soil and plants , to determine the age of rocks, minerals, sediments and soil (eg C-14, U-238, U-235 and Th-232), to study the circulation of elements and their radioactive isotopes in the food chain and in the monitoring studies (natural isotopes, eg K-40, U-238, or artificial isotopes, [1].The examples of monitoring studies include the assessment of the activity of caesium isotopes in surface soil in spatial terms [2][3][4][5].Radioactive isotopes are also used in laboratory testing of processes under controlled conditions, which makes it possible to describe them and to assess the behavior in the environment. The use of these methods is presented, inter alia, in sample Australian studies 1 Independent Chair of Biotechnology and Molecular Biology, Opole University, ul. kard. B. Kominka 6, 45-035 Opole, Poland, phone +48 77 401 60 46, email: agna@uni.opole.pl Unauthenticated Download Date | 5/8/18 5:37 AM Agnieszka Dołhańczuk-Śródka 380 [6]. The use of Cs-134, Sr-85 and Zn-65 made it possible to determine the penetration of radioactive fallout into tropical soil. were used to identify the mechanism and dynamics of trace metal bonding in port sediments.Radioactive isotopes present in the environment, such as Th-234, Be-7, Pb-210, Cs-137, Si-32 and C-14, were used to study present-day sedimentation in seas and oceans. Th-234 and Be-7 isotopes are used, inter alia, in bioturbation and sedimentation studies in the high material supply conditions [7,8].Pb-210 isotope is most commonly used to determine the rate of marine [9] and lacustrine [10-14] sediment increase, but also to identify the rate of snow cover increase. The lead method was also used in Alpine glacier studies [15,16].Cs-137 is used, as a time marker, very often together with Pb-210, to determine the age of lacustrine sediments. The literature review shows that Cs-137 may be used to determine the rate of deposition of overbank [17,18], lacustrine and delta [19,...