Serbian Ministry of Science and Technological Development [142016, 141001]

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Serbian Ministry of Science and Technological Development [142016, 141001]

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Publications

Vertical Distribution of Cs-137 in Cultivated and Undisturbed Areas

Nenadović, Snežana S.; Nenadović, Miloš; Vukanac, Ivana; Đorđević, Aleksandar R.; Dragicevic, Slavoljub S.; Lješević, Milutin A.

(2010)

TY  - JOUR
AU  - Nenadović, Snežana S.
AU  - Nenadović, Miloš
AU  - Vukanac, Ivana
AU  - Đorđević, Aleksandar R.
AU  - Dragicevic, Slavoljub S.
AU  - Lješević, Milutin A.
PY  - 2010
UR  - https://vinar.vin.bg.ac.rs/handle/123456789/3990
AB  - This paper introduces the distribution background and unique characteristics of Cs-137 in cultivated and undisturbed areas. The samples were taken from three measuring points of the depth of 1 m. We examined all visible horizons and determined their classifications. There were four horizons in one profile. All four horizons had a different zone thickness. Cs-137 is an artificial radionuclide that has been produced primarily as a result of atmospheric thermonuclear weapon tests since the 1950. Also, the great amount of Cs-137 (similar to 85 PBq) was released in the atmosphere during the Chernobyl accident. So, Cs-137 has been globally distributed, with fallout rates generally related to latitude and precipitation depth. The movement of Cs-137 in soil is primarily controlled by soil erosion processes, such as processes caused by water, wind, and tillage. Thus, Cs-137 is a valuable tracer to study soil erosion. The specific activity of Cs-137 in soil and sediment samples was determined by using the gamma-spectrometric method.
T2  - Nuclear technology and radiation protection
T1  - Vertical Distribution of Cs-137 in Cultivated and Undisturbed Areas
VL  - 25
IS  - 1
SP  - 30
EP  - 36
DO  - 10.2298/NTRP1001030N
ER  - 
@article{
author = "Nenadović, Snežana S. and Nenadović, Miloš and Vukanac, Ivana and Đorđević, Aleksandar R. and Dragicevic, Slavoljub S. and Lješević, Milutin A.",
year = "2010",
abstract = "This paper introduces the distribution background and unique characteristics of Cs-137 in cultivated and undisturbed areas. The samples were taken from three measuring points of the depth of 1 m. We examined all visible horizons and determined their classifications. There were four horizons in one profile. All four horizons had a different zone thickness. Cs-137 is an artificial radionuclide that has been produced primarily as a result of atmospheric thermonuclear weapon tests since the 1950. Also, the great amount of Cs-137 (similar to 85 PBq) was released in the atmosphere during the Chernobyl accident. So, Cs-137 has been globally distributed, with fallout rates generally related to latitude and precipitation depth. The movement of Cs-137 in soil is primarily controlled by soil erosion processes, such as processes caused by water, wind, and tillage. Thus, Cs-137 is a valuable tracer to study soil erosion. The specific activity of Cs-137 in soil and sediment samples was determined by using the gamma-spectrometric method.",
journal = "Nuclear technology and radiation protection",
title = "Vertical Distribution of Cs-137 in Cultivated and Undisturbed Areas",
volume = "25",
number = "1",
pages = "30-36",
doi = "10.2298/NTRP1001030N"
}
Nenadović, S. S., Nenadović, M., Vukanac, I., Đorđević, A. R., Dragicevic, S. S.,& Lješević, M. A.. (2010). Vertical Distribution of Cs-137 in Cultivated and Undisturbed Areas. in Nuclear technology and radiation protection, 25(1), 30-36.
https://doi.org/10.2298/NTRP1001030N
Nenadović SS, Nenadović M, Vukanac I, Đorđević AR, Dragicevic SS, Lješević MA. Vertical Distribution of Cs-137 in Cultivated and Undisturbed Areas. in Nuclear technology and radiation protection. 2010;25(1):30-36.
doi:10.2298/NTRP1001030N .
Nenadović, Snežana S., Nenadović, Miloš, Vukanac, Ivana, Đorđević, Aleksandar R., Dragicevic, Slavoljub S., Lješević, Milutin A., "Vertical Distribution of Cs-137 in Cultivated and Undisturbed Areas" in Nuclear technology and radiation protection, 25, no. 1 (2010):30-36,
https://doi.org/10.2298/NTRP1001030N . .
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