Sofija M. Forkapić

Dr. Sofija M. Forkapić


Research Focus & Metrics

Academic Career Length

13Years (2014-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 2017 in Journal of Environmental Radioactivity
Verified
Journal Article
Closed access
SFSofija M. Forkapić
Sofija M. Forkapić
JVJ. Vasin
J. Vasin
IBI. Bikit
I. Bikit
DMD. Mrdja
D. Mrdja
KBK. Bikit
K. Bikit
SMStanko Milić
Stanko Milić

8 May 2014 in Environmental Science and Pollution Research
Verified
Journal Article
Closed access
PDF file
MRMilana Stanislav Rakić
Milana Stanislav Rakić
Maja KaramanMaja Karaman
Maja Karaman
SFSofija M. Forkapić
Sofija M. Forkapić
JHJan Hansman
Jan Hansman
Marko KebertMarko Kebert
Marko Kebert
DMDušan S Mrđa
Dušan S Mrđa

1 January 2017 in Journal of Environmental Radioactivity
Verified
Journal Article
Closed access
SFSofija M. Forkapić
Sofija M. Forkapić
DMD. Maletić
D. Maletić
JVJ. Vasin
J. Vasin
KBK. Bikit
K. Bikit
DMD. Mrdja
D. Mrdja
RBR. Banjanac
R. Banjanac

1 January 2020 in Open Geosciences
Verified
Journal Article
Open access
PDF file
KKKristina S. Kalkan
Kristina S. Kalkan
SFSofija M. Forkapić
Sofija M. Forkapić
Slobodan MarkovicSlobodan Markovic
Slobodan Markovic
KBKristina Bikit
Kristina Bikit
MGMilivoj Gavrilov
Milivoj Gavrilov
RLRobert Lakatoš
Robert Lakatoš
Soil erosion is one of the largest global problems of environmental protection and sustainable development, causing serious land degradation and environmental deterioration. The need for fast and accurate soil rate assessment of erosion and deposition favors the application of alternative methods based on the radionuclide measurement technique contrary to long-term conventional methods. In this paper, we used gamma spectrometry measurements of 137Cs and unsupported 210Pb ex in order to quantify the erosion on the Titel Loess Plateau near the Tisa (Tisza) River in the Vojvodina province of Serbia. Along the slope of the study area and in the immediate vicinity eight representative soil depth profiles were taken and the radioactivity content in 1 cm thick soil layers was analyzed. Soil erosion rates were estimated according to the profile distribution model and the diffusion and migration model for undisturbed soil. The net soil erosion rates, estimated by 137Cs method range from −2.3 t ha−1 yr−1 to −2.7 t ha−1 yr−1, related to the used conversion model which is comparable to published results of similar studies of soil erosion in the region. Vertical distribution of natural radionuclides in soil profiles was also discussed and compared with the profile distribution of unsupported 210Pb ex measurements. The use of diffusion and migration model to convert the results of 210Pb ex activities to soil redistribution rates indicates a slightly higher net erosion of −3.7 t ha−1 yr−1 with 98% of the sediment delivery ratio.

1 September 2016 in Nukleonika
Verified
Journal Article
Open access
PDF file
SFSofija M. Forkapić
Sofija M. Forkapić
KBKristina Bikit
Kristina Bikit
VAVesna Arsić
Vesna Arsić
JIJovana Ilić
Jovana Ilić
GPGordana Pantelić
Gordana Pantelić
MŽMilos Živanović
Milos Živanović
Results and conclusions of interlaboratory comparison of indoor radon in 2015 in Serbia are presented. The participants were three accredited laboratories from Serbia: Serbian Institute of Occupational Health “Dr Dragomir Karajović”, Laboratory for Radioactivity and Dose Measurements at the Faculty of Sciences, University of Novi Sad and Radiation and Environmental Protection Department, Vinča Institute of Nuclear Science. The laboratories make use of the same method for radon measurement, using charcoal canisters according to US Environmental Protection Agency (EPA) protocol 520/5-87-005. Calibration of detection efficiency was performed using EPA radium standard. Radon activity concentrations were determined on the basis of the intensity of short-living radon daughters, 214Bi and 214Pb, gamma lines. The results of intercomparison were evaluated by using the u-test, which was calculated according to the International Atomic Energy Agency criteria. In this paper, not only limitations but also the advantages and possibilities of application of this method for measuring levels of human exposure to radon are discussed.