TY  - JOUR
AU  - Vukašinović, Ivana
AU  - Todorović, Dragana J.
AU  - Djordjević, Aleksandar
AU  - Rajković, Miloš
AU  - Pavlović, Vladimir
PY  - 2015
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/3884
AB  - This paper presents a study of the profile distribution of available micronutrients Fe, Mn, Cu and Zn and radionuclide 137Cs in cultivated soil at the experimental field 'Radmilovac' (property of Agricultural Faculty, Belgrade University) in the vicinity of Vinča Institute of Nuclear Sciences. The soil belongs to the anthrosol class of anthropogenic soils according to FAO (2006). At first, the deep plowing was performed while preparing soil for planting peach trees followed by cultivation of soil for 12 years. All agricultural treatments at the experimental field ceased for three years. After that period, soil sampling was carried out. Contents of DTPA-extracted Fe, Mn, Cu and Zn were in the range of (mg kg-1): 5.8-41.6; 9.2-34.2; 1-7.6 and 0.2-1.3, respectively. Detected activity concentration (Bq kg-1) for 137Cs ranged from 1.8 to 35. It was noticed that distribution patterns of 137Cs radionuclide and available Cu and Zn along soil depth were very similar and they were analyzed by simple linear regression; mutual affinity for the soil organic matter might affect their distribution in soil. Contents of available Fe and Mn exhibited different, more constant distribution within a soil horizon.
AB  - U ovom radu ispitivana je raspodela sadržaja pristupačnih mikroelemenata Fe, Mn, Cu i Zn i koncentracije aktivnosti proizvedenog radionuklida 137Cs u profilima zemljišta (dubine 080 cm) sakupljenih sa voćnjaka pod zasadom breskvi na oglednom školskom poljoprivrednom dobru 'Radmilovac' (Poljoprivredni fakultet, Univerzitet u Beogradu) u neposrednoj blizini Instituta za nuklearne nauke 'Vinča'. Zemljište pripada klasi antrosol antropogenih zemljišta prema međunarodnoj FAO (2006) klasifikaciji. Priprema zemljišta za sadnju bresaka izvršena je rigolovanjem, posle čega je usledila 12 godina duga nega voćnjaka. Uzorkovanje zemljišta izvršeno je tri godine nakon prestanka svih poljoprivrednih tretmana zemljišta na oglednom polju. Sadržaji pristupačnih mikroelemenata Fe, Mn, Cu i Zn (dobijeni ekstrakcijom sa rastvorom 0,005 M DTPA) nalazili su se u opsegu (mg kg-1): 5,841,6; 9,234,2; 17,6 odnosno 0,21,3. Detektovana koncentracija aktivnosti 137Cs u zemljištu (merena metodom gama-spektrometrije korišćenjem koaksijalnog HPGe-detektora) nalazila se u intervalu (Bq kg-1): 1,835. Uočeno je da su obrasci distribucije po dubini profila pristupačnih oblika Cu i Zn i radionuklida 137Cs bili veoma slični, a rezultati proste linearne regresione analize su pokazali da je uzajamni afinitet prema organskoj materiji zemljišta mogao da utiče na takvu njihovu distribuciju. Sadržaji pristupačnih mikroelemenata Fe i Mn, pokazali su da imaju drugačiju, uniformniju distribuciju po dubini ispitivanih profila zemljišta.
PB  - Univerzitet u Beogradu - Poljoprivredni fakultet, Beograd
T2  - Journal of Agricultural Sciences (Belgrade)
T1  - Depth distribution of available micronutrients in cultivated soil
T1  - Raspodela pristupačnih sadržaja mikroelemenata po dubini kultivisanog zemljišta
EP  - 187
IS  - 2
SP  - 177
VL  - 60
DO  - 10.2298/JAS1502177V
ER  - 

@article{
author = "Vukašinović, Ivana and Todorović, Dragana J. and Djordjević, Aleksandar and Rajković, Miloš and Pavlović, Vladimir",
year = "2015",
abstract = "This paper presents a study of the profile distribution of available micronutrients Fe, Mn, Cu and Zn and radionuclide 137Cs in cultivated soil at the experimental field 'Radmilovac' (property of Agricultural Faculty, Belgrade University) in the vicinity of Vinča Institute of Nuclear Sciences. The soil belongs to the anthrosol class of anthropogenic soils according to FAO (2006). At first, the deep plowing was performed while preparing soil for planting peach trees followed by cultivation of soil for 12 years. All agricultural treatments at the experimental field ceased for three years. After that period, soil sampling was carried out. Contents of DTPA-extracted Fe, Mn, Cu and Zn were in the range of (mg kg-1): 5.8-41.6; 9.2-34.2; 1-7.6 and 0.2-1.3, respectively. Detected activity concentration (Bq kg-1) for 137Cs ranged from 1.8 to 35. It was noticed that distribution patterns of 137Cs radionuclide and available Cu and Zn along soil depth were very similar and they were analyzed by simple linear regression; mutual affinity for the soil organic matter might affect their distribution in soil. Contents of available Fe and Mn exhibited different, more constant distribution within a soil horizon., U ovom radu ispitivana je raspodela sadržaja pristupačnih mikroelemenata Fe, Mn, Cu i Zn i koncentracije aktivnosti proizvedenog radionuklida 137Cs u profilima zemljišta (dubine 080 cm) sakupljenih sa voćnjaka pod zasadom breskvi na oglednom školskom poljoprivrednom dobru 'Radmilovac' (Poljoprivredni fakultet, Univerzitet u Beogradu) u neposrednoj blizini Instituta za nuklearne nauke 'Vinča'. Zemljište pripada klasi antrosol antropogenih zemljišta prema međunarodnoj FAO (2006) klasifikaciji. Priprema zemljišta za sadnju bresaka izvršena je rigolovanjem, posle čega je usledila 12 godina duga nega voćnjaka. Uzorkovanje zemljišta izvršeno je tri godine nakon prestanka svih poljoprivrednih tretmana zemljišta na oglednom polju. Sadržaji pristupačnih mikroelemenata Fe, Mn, Cu i Zn (dobijeni ekstrakcijom sa rastvorom 0,005 M DTPA) nalazili su se u opsegu (mg kg-1): 5,841,6; 9,234,2; 17,6 odnosno 0,21,3. Detektovana koncentracija aktivnosti 137Cs u zemljištu (merena metodom gama-spektrometrije korišćenjem koaksijalnog HPGe-detektora) nalazila se u intervalu (Bq kg-1): 1,835. Uočeno je da su obrasci distribucije po dubini profila pristupačnih oblika Cu i Zn i radionuklida 137Cs bili veoma slični, a rezultati proste linearne regresione analize su pokazali da je uzajamni afinitet prema organskoj materiji zemljišta mogao da utiče na takvu njihovu distribuciju. Sadržaji pristupačnih mikroelemenata Fe i Mn, pokazali su da imaju drugačiju, uniformniju distribuciju po dubini ispitivanih profila zemljišta.",
publisher = "Univerzitet u Beogradu - Poljoprivredni fakultet, Beograd",
journal = "Journal of Agricultural Sciences (Belgrade)",
title = "Depth distribution of available micronutrients in cultivated soil, Raspodela pristupačnih sadržaja mikroelemenata po dubini kultivisanog zemljišta",
pages = "187-177",
number = "2",
volume = "60",
doi = "10.2298/JAS1502177V"
}

Vukašinović, I., Todorović, D. J., Djordjević, A., Rajković, M.,& Pavlović, V.. (2015). Depth distribution of available micronutrients in cultivated soil. in Journal of Agricultural Sciences (Belgrade)
Univerzitet u Beogradu - Poljoprivredni fakultet, Beograd., 60(2), 177-187.
https://doi.org/10.2298/JAS1502177V

Vukašinović I, Todorović DJ, Djordjević A, Rajković M, Pavlović V. Depth distribution of available micronutrients in cultivated soil. in Journal of Agricultural Sciences (Belgrade). 2015;60(2):177-187.
doi:10.2298/JAS1502177V .

Vukašinović, Ivana, Todorović, Dragana J., Djordjević, Aleksandar, Rajković, Miloš, Pavlović, Vladimir, "Depth distribution of available micronutrients in cultivated soil" in Journal of Agricultural Sciences (Belgrade), 60, no. 2 (2015):177-187,
https://doi.org/10.2298/JAS1502177V . .

TY  - JOUR
AU  - Sarap, Nataša B.
AU  - Janković, Marija M.
AU  - Dolijanović, Željko
AU  - Kovačević, Dušan
AU  - Rajacić, Milica M.
AU  - Nikolić, Jelena D.
AU  - Todorović, Dragana J.
PY  - 2015
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/3796
AB  - This study focuses on determination of soil to plant transfer factor (TF) of long lived radionuclides Sr-90 and Cs-137. Sr-90 and Cs-137 activity concentration in agricultural soil samples was ranged between  lt  0.3 and 1.3 Bq kg(-1) and 14 and 30 Bq kg(-1), from  lt  2.6 to 7.2 Bq kg(-1) and 5 to 13 Bq kg(-1) fresh matter in roots and from 0.4 to 1.1 Bq kg(-1) and  lt  0.2 to 0.7 Bq kg(-1) fresh matter in the rest parts of plant, respectively. Calculated values for Sr-90 and Cs-137 TF from soil to plant ranged from 0.57 to 11.2 and 0.01 to 0.43, respectively.
PB  - Springer, Dordrecht
T2  - Journal of Radioanalytical and Nuclear Chemistry
T1  - Soil-to-plant transfer factor for Sr-90 and Cs-137
EP  - 2527
IS  - 3
SP  - 2523
VL  - 303
DO  - 10.1007/s10967-014-3809-3
ER  - 

@article{
author = "Sarap, Nataša B. and Janković, Marija M. and Dolijanović, Željko and Kovačević, Dušan and Rajacić, Milica M. and Nikolić, Jelena D. and Todorović, Dragana J.",
year = "2015",
abstract = "This study focuses on determination of soil to plant transfer factor (TF) of long lived radionuclides Sr-90 and Cs-137. Sr-90 and Cs-137 activity concentration in agricultural soil samples was ranged between  lt  0.3 and 1.3 Bq kg(-1) and 14 and 30 Bq kg(-1), from  lt  2.6 to 7.2 Bq kg(-1) and 5 to 13 Bq kg(-1) fresh matter in roots and from 0.4 to 1.1 Bq kg(-1) and  lt  0.2 to 0.7 Bq kg(-1) fresh matter in the rest parts of plant, respectively. Calculated values for Sr-90 and Cs-137 TF from soil to plant ranged from 0.57 to 11.2 and 0.01 to 0.43, respectively.",
publisher = "Springer, Dordrecht",
journal = "Journal of Radioanalytical and Nuclear Chemistry",
title = "Soil-to-plant transfer factor for Sr-90 and Cs-137",
pages = "2527-2523",
number = "3",
volume = "303",
doi = "10.1007/s10967-014-3809-3"
}

Sarap, N. B., Janković, M. M., Dolijanović, Ž., Kovačević, D., Rajacić, M. M., Nikolić, J. D.,& Todorović, D. J.. (2015). Soil-to-plant transfer factor for Sr-90 and Cs-137. in Journal of Radioanalytical and Nuclear Chemistry
Springer, Dordrecht., 303(3), 2523-2527.
https://doi.org/10.1007/s10967-014-3809-3

Sarap NB, Janković MM, Dolijanović Ž, Kovačević D, Rajacić MM, Nikolić JD, Todorović DJ. Soil-to-plant transfer factor for Sr-90 and Cs-137. in Journal of Radioanalytical and Nuclear Chemistry. 2015;303(3):2523-2527.
doi:10.1007/s10967-014-3809-3 .

Sarap, Nataša B., Janković, Marija M., Dolijanović, Željko, Kovačević, Dušan, Rajacić, Milica M., Nikolić, Jelena D., Todorović, Dragana J., "Soil-to-plant transfer factor for Sr-90 and Cs-137" in Journal of Radioanalytical and Nuclear Chemistry, 303, no. 3 (2015):2523-2527,
https://doi.org/10.1007/s10967-014-3809-3 . .

TY  - JOUR
AU  - Vukašinović, Ivana
AU  - Todorović, Dragana J.
AU  - Nikolić, Nataša S.
AU  - Mihajlović-Radosavljević, Ana
AU  - Nenadović, Snežana S.
AU  - Eremić-Savković, Maja
PY  - 2014
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/3477
AB  - The study of spatial distribution of activity concentration of U-238, Ra-226, (210)pb, Th-232, K-40 and Cs-237 radionuclides in the surface soil samples (n = 42) collected in the vicinity of four coal-fired power plants in Serbia is presented. Radioactivity measurements in soils performed by gamma-ray spectrometry showed values [Bqkg(-1)] in the range: 15-117 for U-238, 21-115 for Ra-226, 33-65 for (210)pb, 20-69 for Th-232, 324-736 for K-40, and 2-59 for Cs-137. Surface soil radioactivity that could have resulted from deposition of radionuclides from airborne discharges or resuspension of ash from disposal sites showed no enhanced levels. It was found that variation of soil textural properties, pH values, and carbonate content influenced activity levels of natural radionuclides while radiocesium activities were associated with soil organic matter content. Modification of some soil properties was observed in the immediate vicinity ( lt 1 km) of power plants where the soil was more alkaline with coarser particles (0.2-0.05 mm) and carbonates accumulated. Calculated average values of the absorbed gamma dose rate and annual external effective dose originating from the terrestrial radionudides were 69.4 nGy/h and 0.085 mSv, respectively.
PB  - Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd
T2  - Nuclear Technology & Radiation Protection
T1  - Radioactivity measurements in soils surrounding four coal-fired power plants in Serbia by gamma-ray spectrometry and estimated dose
EP  - 306
IS  - 4
SP  - 296
VL  - 29
DO  - 10.2298/NTRP1404296V
ER  - 

@article{
author = "Vukašinović, Ivana and Todorović, Dragana J. and Nikolić, Nataša S. and Mihajlović-Radosavljević, Ana and Nenadović, Snežana S. and Eremić-Savković, Maja",
year = "2014",
abstract = "The study of spatial distribution of activity concentration of U-238, Ra-226, (210)pb, Th-232, K-40 and Cs-237 radionuclides in the surface soil samples (n = 42) collected in the vicinity of four coal-fired power plants in Serbia is presented. Radioactivity measurements in soils performed by gamma-ray spectrometry showed values [Bqkg(-1)] in the range: 15-117 for U-238, 21-115 for Ra-226, 33-65 for (210)pb, 20-69 for Th-232, 324-736 for K-40, and 2-59 for Cs-137. Surface soil radioactivity that could have resulted from deposition of radionuclides from airborne discharges or resuspension of ash from disposal sites showed no enhanced levels. It was found that variation of soil textural properties, pH values, and carbonate content influenced activity levels of natural radionuclides while radiocesium activities were associated with soil organic matter content. Modification of some soil properties was observed in the immediate vicinity ( lt 1 km) of power plants where the soil was more alkaline with coarser particles (0.2-0.05 mm) and carbonates accumulated. Calculated average values of the absorbed gamma dose rate and annual external effective dose originating from the terrestrial radionudides were 69.4 nGy/h and 0.085 mSv, respectively.",
publisher = "Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd",
journal = "Nuclear Technology & Radiation Protection",
title = "Radioactivity measurements in soils surrounding four coal-fired power plants in Serbia by gamma-ray spectrometry and estimated dose",
pages = "306-296",
number = "4",
volume = "29",
doi = "10.2298/NTRP1404296V"
}

Vukašinović, I., Todorović, D. J., Nikolić, N. S., Mihajlović-Radosavljević, A., Nenadović, S. S.,& Eremić-Savković, M.. (2014). Radioactivity measurements in soils surrounding four coal-fired power plants in Serbia by gamma-ray spectrometry and estimated dose. in Nuclear Technology & Radiation Protection
Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd., 29(4), 296-306.
https://doi.org/10.2298/NTRP1404296V

Vukašinović I, Todorović DJ, Nikolić NS, Mihajlović-Radosavljević A, Nenadović SS, Eremić-Savković M. Radioactivity measurements in soils surrounding four coal-fired power plants in Serbia by gamma-ray spectrometry and estimated dose. in Nuclear Technology & Radiation Protection. 2014;29(4):296-306.
doi:10.2298/NTRP1404296V .

Vukašinović, Ivana, Todorović, Dragana J., Nikolić, Nataša S., Mihajlović-Radosavljević, Ana, Nenadović, Snežana S., Eremić-Savković, Maja, "Radioactivity measurements in soils surrounding four coal-fired power plants in Serbia by gamma-ray spectrometry and estimated dose" in Nuclear Technology & Radiation Protection, 29, no. 4 (2014):296-306,
https://doi.org/10.2298/NTRP1404296V . .

TY  - JOUR
AU  - Vukašinović, Ivana
AU  - Todorović, Dragana
AU  - Djordjević, Aleksandar
AU  - Rajković, Miloš
AU  - Pavlović, Vladimir
PY  - 2013
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/3115
AB  - This is a preliminary study of the depth distribution of Cs-137 radionuclides in cultivated anthrosol soil of a 15-year old peach tree plantation at the experimental field "Radmilovac" near Belgrade. Before planting, the soil was ploughed at the depth of 1 m. The soil had not been annually ploughed, irrigated and treated with mineral fertilizers for three years before sampling. Activity concentration for Cs-137 ranged from 1.8 Bq kg(-1) to 35 Bq kg(-1). Along the soil depth it varied highly, reaching as high a total variation coefficient as 83 %. Radiocaesium distribution patterns depended on the extent of soil mixing in the plough layer, as it was mechanically transferred from the surface to the lower soil layers during cultivation. Cs-137 was associated with humus content and fixation to clay fractions in the soil. Our results single out soil's hygroscopic water as a valuable parameter for Cs-137 behaviour that could be used commonly if the measurement is standardised.
PB  - Inst Medical Research & Occupational Health, Zagreb
T2  - Arhiv za higijenu rada i toksikologiju-Archives of Industrial Hygiene and Toxicology
T1  - Depth distribution of cs-137 in anthrosol from the experimental field "Radmilovac" near Belgrade, Serbia
EP  - 430
IS  - 3
SP  - 425
VL  - 64
DO  - 10.2478/10004-1254-64-2013-2276
ER  - 

@article{
author = "Vukašinović, Ivana and Todorović, Dragana and Djordjević, Aleksandar and Rajković, Miloš and Pavlović, Vladimir",
year = "2013",
abstract = "This is a preliminary study of the depth distribution of Cs-137 radionuclides in cultivated anthrosol soil of a 15-year old peach tree plantation at the experimental field "Radmilovac" near Belgrade. Before planting, the soil was ploughed at the depth of 1 m. The soil had not been annually ploughed, irrigated and treated with mineral fertilizers for three years before sampling. Activity concentration for Cs-137 ranged from 1.8 Bq kg(-1) to 35 Bq kg(-1). Along the soil depth it varied highly, reaching as high a total variation coefficient as 83 %. Radiocaesium distribution patterns depended on the extent of soil mixing in the plough layer, as it was mechanically transferred from the surface to the lower soil layers during cultivation. Cs-137 was associated with humus content and fixation to clay fractions in the soil. Our results single out soil's hygroscopic water as a valuable parameter for Cs-137 behaviour that could be used commonly if the measurement is standardised.",
publisher = "Inst Medical Research & Occupational Health, Zagreb",
journal = "Arhiv za higijenu rada i toksikologiju-Archives of Industrial Hygiene and Toxicology",
title = "Depth distribution of cs-137 in anthrosol from the experimental field "Radmilovac" near Belgrade, Serbia",
pages = "430-425",
number = "3",
volume = "64",
doi = "10.2478/10004-1254-64-2013-2276"
}

Vukašinović, I., Todorović, D., Djordjević, A., Rajković, M.,& Pavlović, V.. (2013). Depth distribution of cs-137 in anthrosol from the experimental field "Radmilovac" near Belgrade, Serbia. in Arhiv za higijenu rada i toksikologiju-Archives of Industrial Hygiene and Toxicology
Inst Medical Research & Occupational Health, Zagreb., 64(3), 425-430.
https://doi.org/10.2478/10004-1254-64-2013-2276

Vukašinović I, Todorović D, Djordjević A, Rajković M, Pavlović V. Depth distribution of cs-137 in anthrosol from the experimental field "Radmilovac" near Belgrade, Serbia. in Arhiv za higijenu rada i toksikologiju-Archives of Industrial Hygiene and Toxicology. 2013;64(3):425-430.
doi:10.2478/10004-1254-64-2013-2276 .

Vukašinović, Ivana, Todorović, Dragana, Djordjević, Aleksandar, Rajković, Miloš, Pavlović, Vladimir, "Depth distribution of cs-137 in anthrosol from the experimental field "Radmilovac" near Belgrade, Serbia" in Arhiv za higijenu rada i toksikologiju-Archives of Industrial Hygiene and Toxicology, 64, no. 3 (2013):425-430,
https://doi.org/10.2478/10004-1254-64-2013-2276 . .

TY  - JOUR
AU  - Vukašinović, Ivana
AU  - Djordjević, Aleksandar
AU  - Rajković, Miloš
AU  - Todorović, Dragana
AU  - Pavlović, Vladimir
PY  - 2010
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/2332
AB  - Taking into account the importance of distribution and transfer of radionuclides in the soil-water-plant system, especially in agricultural fields, in this study, natural radionuclide determination in regosol-type soil was performed. The correlations between main soil properties and the contents of natural isotopes U-238, Ra-226, Th-232, and K-40 in agricultural soil and their distribution through the soil depth was studied. For determination of natural radionuclide activity concentration, we used the CANBERRA HPGe detector, applying the gamma spectrometry method. The investigation was performed on an experimental peach tree field characterized by a anthrosol type of soil, derived from the chernozem type of natural soil. The effect of measured soil properties on activity concentration levels was analyzed by simple and multiple linear regression analysis. Considering the linear model, in our soil profiles of 0-80 cm depth, clay content was positively related with U-238, Ra-226, and K-40, and about 30% of the variation of those radionuclides was explained. Sand fraction was negatively related with U-238, Ra-226, Th-232, and K-40 and the correlation was medium, except for Ra-226 (r = -0.68). The joint effect of pH, carbonates, humus, clay, and sand contents on natural radionuclide distribution in the 0-80 cm layer was found by multiple linear regression analysis. Radionuclide behavior was explained by the R-squared statistic. The investigations of uranium distribution showed that when the soil layers of 0-20 cm and 60-80 cm are considered together, uranium behavior is affected by soil pH and the content of humus, carbonates, and clay. Multiple regression analysis of Ra-226, Th-232 and K-40 activities in soil layers of 0-20 cm and 60-80 cm showed that their lower mobility and uniform depth distribution are associated with small variations of carbonates along soil depth and mineral composition of the parent materials, while the soil pH had no effect on their behavior.
PB  - Tubitak Scientific & Technical Research Council Turkey, Ankara
T2  - Turkish Journal of Agriculture and Forestry
T1  - Distribution of natural radionuclides in anthrosol-type soil
EP  - 546
IS  - 6
SP  - 539
VL  - 34
DO  - 10.3906/tar-0911-59
ER  - 

@article{
author = "Vukašinović, Ivana and Djordjević, Aleksandar and Rajković, Miloš and Todorović, Dragana and Pavlović, Vladimir",
year = "2010",
abstract = "Taking into account the importance of distribution and transfer of radionuclides in the soil-water-plant system, especially in agricultural fields, in this study, natural radionuclide determination in regosol-type soil was performed. The correlations between main soil properties and the contents of natural isotopes U-238, Ra-226, Th-232, and K-40 in agricultural soil and their distribution through the soil depth was studied. For determination of natural radionuclide activity concentration, we used the CANBERRA HPGe detector, applying the gamma spectrometry method. The investigation was performed on an experimental peach tree field characterized by a anthrosol type of soil, derived from the chernozem type of natural soil. The effect of measured soil properties on activity concentration levels was analyzed by simple and multiple linear regression analysis. Considering the linear model, in our soil profiles of 0-80 cm depth, clay content was positively related with U-238, Ra-226, and K-40, and about 30% of the variation of those radionuclides was explained. Sand fraction was negatively related with U-238, Ra-226, Th-232, and K-40 and the correlation was medium, except for Ra-226 (r = -0.68). The joint effect of pH, carbonates, humus, clay, and sand contents on natural radionuclide distribution in the 0-80 cm layer was found by multiple linear regression analysis. Radionuclide behavior was explained by the R-squared statistic. The investigations of uranium distribution showed that when the soil layers of 0-20 cm and 60-80 cm are considered together, uranium behavior is affected by soil pH and the content of humus, carbonates, and clay. Multiple regression analysis of Ra-226, Th-232 and K-40 activities in soil layers of 0-20 cm and 60-80 cm showed that their lower mobility and uniform depth distribution are associated with small variations of carbonates along soil depth and mineral composition of the parent materials, while the soil pH had no effect on their behavior.",
publisher = "Tubitak Scientific & Technical Research Council Turkey, Ankara",
journal = "Turkish Journal of Agriculture and Forestry",
title = "Distribution of natural radionuclides in anthrosol-type soil",
pages = "546-539",
number = "6",
volume = "34",
doi = "10.3906/tar-0911-59"
}

Vukašinović, I., Djordjević, A., Rajković, M., Todorović, D.,& Pavlović, V.. (2010). Distribution of natural radionuclides in anthrosol-type soil. in Turkish Journal of Agriculture and Forestry
Tubitak Scientific & Technical Research Council Turkey, Ankara., 34(6), 539-546.
https://doi.org/10.3906/tar-0911-59

Vukašinović I, Djordjević A, Rajković M, Todorović D, Pavlović V. Distribution of natural radionuclides in anthrosol-type soil. in Turkish Journal of Agriculture and Forestry. 2010;34(6):539-546.
doi:10.3906/tar-0911-59 .

Vukašinović, Ivana, Djordjević, Aleksandar, Rajković, Miloš, Todorović, Dragana, Pavlović, Vladimir, "Distribution of natural radionuclides in anthrosol-type soil" in Turkish Journal of Agriculture and Forestry, 34, no. 6 (2010):539-546,
https://doi.org/10.3906/tar-0911-59 . .

TY  - JOUR
AU  - Vukašinović, Ivana
AU  - Todorović, Dragana J.
AU  - Djordjević, Aleksandar
AU  - Rajković, Miloš
AU  - Stojanović, Mirjana D.
AU  - Pavlović, Vladimir
PY  - 2009
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/1950
AB  - Distribution of natural gamma-emitting radionuclides 238U and 40K were determined in the soil profiles from the peach-trees field on experimental farm Radmilovac, southeast Belgrade. Internal soil morphology has been changed in 1992. when soil rigosol type with deep Ap-horizon (0-80 cm) has been formed by special treatment of parent soil, chernozem type. Gamma-spectrometry method is applied in measurement of radionuclide activities in soil samples by using hyperpure coaxial gamma-ray detector, Canberra type. Investigation results has been shown that the natural activity contents obtained in the experiment are within the range of normal BACKGROUND:  activity according to UNSCEAR (2000) and that radionuclide activity decreased in the plant root zone.
AB  - Distribucija prirodnih radionuklida gama-emitera 238U i 40K je određena u profilima zemljišta sakupljenih sa voćnjaka pod zasadom breskvi na Oglednom školskom poljoprivrednom dobru 'Radmilovac', Poljoprivrednog fakulteta, Beograd-Zemun. Unutrašnja morfologija zemljišta je izmenjena 1992. godine kada je zemljište rigosol tipa sa dubokim Ap-horizontom (0-80 cm) formirano rigolovanjem osnovnog zemljišta černozem tipa. Aktivnost radionuklida u uzorcima zemljišta određena je metodom gama-spektrometrije korišćenjem koaksijalnog HPGe-detektora (Canberra). Rezultati ispitivanja su pokazala da je eksperimentalno određena prirodna aktivnost u granicama normalne osnovne aktivnosti preporučene od strane UNSCEAR (2000) i da aktivnost radionuklida opada u zoni korenovog sistema.
PB  - Univerzitet u Beogradu - Poljoprivredni fakultet, Beograd
T2  - Journal of Agricultural Sciences (Belgrade)
T1  - Natural isotopes 238U and 40K content in rigosol from the area of school estate good 'Radmilovac' of Faculty of Agriculture, Zemun
T1  - Sadržaj prirodnih izotopa 238U i 40K u rigosolu sa područja Oglednog školskog dobra 'Radmilovac', Poljoprivrednog fakulteta u Zemunu
EP  - 151
IS  - 2
SP  - 143
VL  - 54
DO  - 10.2298/JAS0902143V
ER  - 

@article{
author = "Vukašinović, Ivana and Todorović, Dragana J. and Djordjević, Aleksandar and Rajković, Miloš and Stojanović, Mirjana D. and Pavlović, Vladimir",
year = "2009",
abstract = "Distribution of natural gamma-emitting radionuclides 238U and 40K were determined in the soil profiles from the peach-trees field on experimental farm Radmilovac, southeast Belgrade. Internal soil morphology has been changed in 1992. when soil rigosol type with deep Ap-horizon (0-80 cm) has been formed by special treatment of parent soil, chernozem type. Gamma-spectrometry method is applied in measurement of radionuclide activities in soil samples by using hyperpure coaxial gamma-ray detector, Canberra type. Investigation results has been shown that the natural activity contents obtained in the experiment are within the range of normal BACKGROUND:  activity according to UNSCEAR (2000) and that radionuclide activity decreased in the plant root zone., Distribucija prirodnih radionuklida gama-emitera 238U i 40K je određena u profilima zemljišta sakupljenih sa voćnjaka pod zasadom breskvi na Oglednom školskom poljoprivrednom dobru 'Radmilovac', Poljoprivrednog fakulteta, Beograd-Zemun. Unutrašnja morfologija zemljišta je izmenjena 1992. godine kada je zemljište rigosol tipa sa dubokim Ap-horizontom (0-80 cm) formirano rigolovanjem osnovnog zemljišta černozem tipa. Aktivnost radionuklida u uzorcima zemljišta određena je metodom gama-spektrometrije korišćenjem koaksijalnog HPGe-detektora (Canberra). Rezultati ispitivanja su pokazala da je eksperimentalno određena prirodna aktivnost u granicama normalne osnovne aktivnosti preporučene od strane UNSCEAR (2000) i da aktivnost radionuklida opada u zoni korenovog sistema.",
publisher = "Univerzitet u Beogradu - Poljoprivredni fakultet, Beograd",
journal = "Journal of Agricultural Sciences (Belgrade)",
title = "Natural isotopes 238U and 40K content in rigosol from the area of school estate good 'Radmilovac' of Faculty of Agriculture, Zemun, Sadržaj prirodnih izotopa 238U i 40K u rigosolu sa područja Oglednog školskog dobra 'Radmilovac', Poljoprivrednog fakulteta u Zemunu",
pages = "151-143",
number = "2",
volume = "54",
doi = "10.2298/JAS0902143V"
}

Vukašinović, I., Todorović, D. J., Djordjević, A., Rajković, M., Stojanović, M. D.,& Pavlović, V.. (2009). Natural isotopes 238U and 40K content in rigosol from the area of school estate good 'Radmilovac' of Faculty of Agriculture, Zemun. in Journal of Agricultural Sciences (Belgrade)
Univerzitet u Beogradu - Poljoprivredni fakultet, Beograd., 54(2), 143-151.
https://doi.org/10.2298/JAS0902143V

Vukašinović I, Todorović DJ, Djordjević A, Rajković M, Stojanović MD, Pavlović V. Natural isotopes 238U and 40K content in rigosol from the area of school estate good 'Radmilovac' of Faculty of Agriculture, Zemun. in Journal of Agricultural Sciences (Belgrade). 2009;54(2):143-151.
doi:10.2298/JAS0902143V .

Vukašinović, Ivana, Todorović, Dragana J., Djordjević, Aleksandar, Rajković, Miloš, Stojanović, Mirjana D., Pavlović, Vladimir, "Natural isotopes 238U and 40K content in rigosol from the area of school estate good 'Radmilovac' of Faculty of Agriculture, Zemun" in Journal of Agricultural Sciences (Belgrade), 54, no. 2 (2009):143-151,
https://doi.org/10.2298/JAS0902143V . .

TY  - JOUR
AU  - Radenković, Miriana B.
AU  - Cupać, Svjetlana
AU  - Joksić, Jasminka D.
AU  - Todorović, Dragana J.
PY  - 2008
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/1829
AB  - Goal, Scope and BACKGROUND: . During the Balkan conflict in 1999, soil in contaminated areas was enriched in depleted uranium (DU) isotopic signature, relative to the in-situ natural uranium present. After the military activities, most of kinetic DU penetrators or their fragments remained buried in the ground in certain geomorphological and geochemical environments exposed to local weathering conditions. The contamination distribution, mobility and/or fixation of DU in the contaminated soil profile at one hot spot were the subject of our study. The results should disclose what happened with released DU corrosion products in three years elapsed, given the scope of their geochemical fractionation, and mark out the most probable host substrates in investigated soil type. Methods. Gamma-spectrometric analysis of soil samples taken in the DU penetrator impact-zone was done to obtain present contamination levels. Set of samples is subjected to five-step and three-step sequential extraction procedures, specifically selective to different physical/chemical associations in soil. The stable elements are determined in extracts by the atomic absorption spectroscopy. After the ion-exchange based uranium separation procedure, alpha-spectrometric analysis of obtained fractions was done and DU distribution in five extraction phases found from U-235/U-238 and U-234/U-238 isotopic ratios. Results. Depleted uranium concentration falls down to the 1% of the initial value, at approximately 150 mm distance to the source. Carbonates and iron/manganese hydrous oxides are indicated as the most probable substrates for depleted uranium in the characterized soil type. Therefore, in the highly contaminated soil samples, depleted uranium is still weakly bonded and easy exchangeable. The significant levels of organic-bonded depleted uranium are found in surface soil only. Discussion. Dependence of the fractionation on the contamination levels is evident. Samples with higher DU contents have shown a longer maintenance in the exchangeable phases, probably because adsorption/desorption mass transfer through the medium was not very fast. Organic-bonded, depleted uranium is present in surface soil samples due to its higher humus content. Considering geochemical composition of investigated soil, the indicating chemical associations as substrates are in agreement with some considerations based on the results for low-level waste unsaturated zones. Conclusions. The soil contamination with depleted uranium in investigated area is still 'spot' type and not widespread. Dependence of the fractionation on the contamination levels and presence of weakly bonded, depleted uranium in the hot spots areas is evident. Recommendations and Perspectives. A detailed study may be undertaken with suitable extractive reagents to define a bio-available fraction of depleted uranium in soil. The comparison of results for different soil types investigated by the same methodology may be useful. An applied combination of physical/chemical procedures and analysis may help in the decision making on the remediation strategy for sites contaminated with depleted uranium used in military operations.
PB  - Springer Heidelberg, Heidelberg
T2  - Environmental Science and Pollution Research
T1  - Depleted uranium mobility and fractionation in contaminated soil (Southern Serbia)
EP  - 67
IS  - 1
SP  - 61
VL  - 15
DO  - 10.1065/espr2007.03.399
ER  - 

@article{
author = "Radenković, Miriana B. and Cupać, Svjetlana and Joksić, Jasminka D. and Todorović, Dragana J.",
year = "2008",
abstract = "Goal, Scope and BACKGROUND: . During the Balkan conflict in 1999, soil in contaminated areas was enriched in depleted uranium (DU) isotopic signature, relative to the in-situ natural uranium present. After the military activities, most of kinetic DU penetrators or their fragments remained buried in the ground in certain geomorphological and geochemical environments exposed to local weathering conditions. The contamination distribution, mobility and/or fixation of DU in the contaminated soil profile at one hot spot were the subject of our study. The results should disclose what happened with released DU corrosion products in three years elapsed, given the scope of their geochemical fractionation, and mark out the most probable host substrates in investigated soil type. Methods. Gamma-spectrometric analysis of soil samples taken in the DU penetrator impact-zone was done to obtain present contamination levels. Set of samples is subjected to five-step and three-step sequential extraction procedures, specifically selective to different physical/chemical associations in soil. The stable elements are determined in extracts by the atomic absorption spectroscopy. After the ion-exchange based uranium separation procedure, alpha-spectrometric analysis of obtained fractions was done and DU distribution in five extraction phases found from U-235/U-238 and U-234/U-238 isotopic ratios. Results. Depleted uranium concentration falls down to the 1% of the initial value, at approximately 150 mm distance to the source. Carbonates and iron/manganese hydrous oxides are indicated as the most probable substrates for depleted uranium in the characterized soil type. Therefore, in the highly contaminated soil samples, depleted uranium is still weakly bonded and easy exchangeable. The significant levels of organic-bonded depleted uranium are found in surface soil only. Discussion. Dependence of the fractionation on the contamination levels is evident. Samples with higher DU contents have shown a longer maintenance in the exchangeable phases, probably because adsorption/desorption mass transfer through the medium was not very fast. Organic-bonded, depleted uranium is present in surface soil samples due to its higher humus content. Considering geochemical composition of investigated soil, the indicating chemical associations as substrates are in agreement with some considerations based on the results for low-level waste unsaturated zones. Conclusions. The soil contamination with depleted uranium in investigated area is still 'spot' type and not widespread. Dependence of the fractionation on the contamination levels and presence of weakly bonded, depleted uranium in the hot spots areas is evident. Recommendations and Perspectives. A detailed study may be undertaken with suitable extractive reagents to define a bio-available fraction of depleted uranium in soil. The comparison of results for different soil types investigated by the same methodology may be useful. An applied combination of physical/chemical procedures and analysis may help in the decision making on the remediation strategy for sites contaminated with depleted uranium used in military operations.",
publisher = "Springer Heidelberg, Heidelberg",
journal = "Environmental Science and Pollution Research",
title = "Depleted uranium mobility and fractionation in contaminated soil (Southern Serbia)",
pages = "67-61",
number = "1",
volume = "15",
doi = "10.1065/espr2007.03.399"
}

Radenković, M. B., Cupać, S., Joksić, J. D.,& Todorović, D. J.. (2008). Depleted uranium mobility and fractionation in contaminated soil (Southern Serbia). in Environmental Science and Pollution Research
Springer Heidelberg, Heidelberg., 15(1), 61-67.
https://doi.org/10.1065/espr2007.03.399

Radenković MB, Cupać S, Joksić JD, Todorović DJ. Depleted uranium mobility and fractionation in contaminated soil (Southern Serbia). in Environmental Science and Pollution Research. 2008;15(1):61-67.
doi:10.1065/espr2007.03.399 .

Radenković, Miriana B., Cupać, Svjetlana, Joksić, Jasminka D., Todorović, Dragana J., "Depleted uranium mobility and fractionation in contaminated soil (Southern Serbia)" in Environmental Science and Pollution Research, 15, no. 1 (2008):61-67,
https://doi.org/10.1065/espr2007.03.399 . .