Vertical distribution of 137Cs in cultivated and undisturbed areas

This paper introduces the distribution background and unique characteristics of 137Cs 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 pr...

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Main Authors: Nenadović Snežana S., Nenadović Miloš T., Vukanac Ivana S., Đorđević Aleksandar R., Dragićević Slavoljub S., Lješević Milutin A.
Format: Article
Language:English
Published: VINCA Institute of Nuclear Sciences 2010-01-01
Series:Nuclear Technology and Radiation Protection
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/1451-3994/2010/1451-39941001030N.pdf
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spelling doaj-b87f8898dfcc4e029dd10f56017ee4d32020-11-25T01:50:17ZengVINCA Institute of Nuclear SciencesNuclear Technology and Radiation Protection1451-39942010-01-01251303610.2298/NTRP1001030NVertical distribution of 137Cs in cultivated and undisturbed areasNenadović Snežana S.Nenadović Miloš T.Vukanac Ivana S.Đorđević Aleksandar R.Dragićević Slavoljub S.Lješević Milutin A.This paper introduces the distribution background and unique characteristics of 137Cs 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. 137Cs 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 137Cs (~85 PBq) was released in the atmosphere during the Chernobyl accident. So, 137Cs has been globally distributed, with fallout rates generally related to latitude and precipitation depth. The movement of 137Cs in soil is primarily controlled by soil erosion processes, such as processes caused by water, wind, and tillage. Thus, 137Cs is a valuable tracer to study soil erosion. The specific activity of 137Cs in soil and sediment samples was determined by using the gamma-spectrometric method. http://www.doiserbia.nb.rs/img/doi/1451-3994/2010/1451-39941001030N.pdf137Cserosionsoilgamma-spectrometric method
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language English
format Article
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author Nenadović Snežana S.
Nenadović Miloš T.
Vukanac Ivana S.
Đorđević Aleksandar R.
Dragićević Slavoljub S.
Lješević Milutin A.
spellingShingle Nenadović Snežana S.
Nenadović Miloš T.
Vukanac Ivana S.
Đorđević Aleksandar R.
Dragićević Slavoljub S.
Lješević Milutin A.
Vertical distribution of 137Cs in cultivated and undisturbed areas
Nuclear Technology and Radiation Protection
137Cs
erosion
soil
gamma-spectrometric method
author_facet Nenadović Snežana S.
Nenadović Miloš T.
Vukanac Ivana S.
Đorđević Aleksandar R.
Dragićević Slavoljub S.
Lješević Milutin A.
author_sort Nenadović Snežana S.
title Vertical distribution of 137Cs in cultivated and undisturbed areas
title_short Vertical distribution of 137Cs in cultivated and undisturbed areas
title_full Vertical distribution of 137Cs in cultivated and undisturbed areas
title_fullStr Vertical distribution of 137Cs in cultivated and undisturbed areas
title_full_unstemmed Vertical distribution of 137Cs in cultivated and undisturbed areas
title_sort vertical distribution of 137cs in cultivated and undisturbed areas
publisher VINCA Institute of Nuclear Sciences
series Nuclear Technology and Radiation Protection
issn 1451-3994
publishDate 2010-01-01
description This paper introduces the distribution background and unique characteristics of 137Cs 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. 137Cs 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 137Cs (~85 PBq) was released in the atmosphere during the Chernobyl accident. So, 137Cs has been globally distributed, with fallout rates generally related to latitude and precipitation depth. The movement of 137Cs in soil is primarily controlled by soil erosion processes, such as processes caused by water, wind, and tillage. Thus, 137Cs is a valuable tracer to study soil erosion. The specific activity of 137Cs in soil and sediment samples was determined by using the gamma-spectrometric method.
topic 137Cs
erosion
soil
gamma-spectrometric method
url http://www.doiserbia.nb.rs/img/doi/1451-3994/2010/1451-39941001030N.pdf
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