TY  - CONF
AU  - Djordjević, Aleksandar
AU  - Grujic, Gordana
AU  - Kaluđerović, Lazar
AU  - Bogosavljević, Jelena
AU  - Đorđević, Snežana
PY  - 2023
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/6767
AB  - The paper presents the results of research on the content of accessible forms of Ni and Cr in the ranker-type soils that are formed on the serpentinites massifs in Serbia. Soil samples were taken from seven 
different locations across Serbia (Zlatibor mountain, Kopaonik mountain, Miroč, Maljen mountain, 
Bukovi, Suvobor and Bubanj Potok) at the altitude range between 100 and 1700 m. There were 
analyzed 46 soil samples in total. The concentration of accessible forms of Ni and Cr was determined 
by extraction in a solution of DTPA-TEA (pH 7.3, ratio soil and solution = 1:2) by optical emission 
spectroscopy with induced coupled plasma (ICP-OES).
The content of accessible Ni in the all examined soil samples of ranker-type soils varies from 68 - 920 
mg/kg, while the most common results (about 70% of the total number of samples) vary from 200 -
600 mg/kg. The content of accessible Cr in all examined soils varies from 16 - 216 mg/kg. The content 
of both, Ni and Cr significantly exceeds the value limits in soils. 
The results of the analysis of all soil samples of ranker-type soils refer to high concentration of 
accessible Ni and Cr and thus correspond to phytotoxic concentrations.
Given the fact that there are no anthropogenic sources of pollution nearby the investigation locations, 
it can be concluded that such a high concentration of accessible Ni and Cr in the ranker-type soils, that 
were formed on serpentinites massifs under the various pedogenetic conditions, is of geochemical 
origin. The geochemical distribution of Ni and Cr places this type of soil in the group of lithogenic soils.
PB  - Society for Environmental Geochemistry and Health
C3  - 38th International Conference on Geochemistry and Health SEGH2023, Athens, Greece
T1  - Geochemical origin of Ni and Cr in ranker-type soils formed on serpentinites  massifs in Serbia
EP  - 111
SP  - 111
UR  - https://hdl.handle.net/21.15107/rcub_agrospace_6767
ER  - 

@conference{
author = "Djordjević, Aleksandar and Grujic, Gordana and Kaluđerović, Lazar and Bogosavljević, Jelena and Đorđević, Snežana",
year = "2023",
abstract = "The paper presents the results of research on the content of accessible forms of Ni and Cr in the ranker-type soils that are formed on the serpentinites massifs in Serbia. Soil samples were taken from seven 
different locations across Serbia (Zlatibor mountain, Kopaonik mountain, Miroč, Maljen mountain, 
Bukovi, Suvobor and Bubanj Potok) at the altitude range between 100 and 1700 m. There were 
analyzed 46 soil samples in total. The concentration of accessible forms of Ni and Cr was determined 
by extraction in a solution of DTPA-TEA (pH 7.3, ratio soil and solution = 1:2) by optical emission 
spectroscopy with induced coupled plasma (ICP-OES).
The content of accessible Ni in the all examined soil samples of ranker-type soils varies from 68 - 920 
mg/kg, while the most common results (about 70% of the total number of samples) vary from 200 -
600 mg/kg. The content of accessible Cr in all examined soils varies from 16 - 216 mg/kg. The content 
of both, Ni and Cr significantly exceeds the value limits in soils. 
The results of the analysis of all soil samples of ranker-type soils refer to high concentration of 
accessible Ni and Cr and thus correspond to phytotoxic concentrations.
Given the fact that there are no anthropogenic sources of pollution nearby the investigation locations, 
it can be concluded that such a high concentration of accessible Ni and Cr in the ranker-type soils, that 
were formed on serpentinites massifs under the various pedogenetic conditions, is of geochemical 
origin. The geochemical distribution of Ni and Cr places this type of soil in the group of lithogenic soils.",
publisher = "Society for Environmental Geochemistry and Health",
journal = "38th International Conference on Geochemistry and Health SEGH2023, Athens, Greece",
title = "Geochemical origin of Ni and Cr in ranker-type soils formed on serpentinites  massifs in Serbia",
pages = "111-111",
url = "https://hdl.handle.net/21.15107/rcub_agrospace_6767"
}

Djordjević, A., Grujic, G., Kaluđerović, L., Bogosavljević, J.,& Đorđević, S.. (2023). Geochemical origin of Ni and Cr in ranker-type soils formed on serpentinites  massifs in Serbia. in 38th International Conference on Geochemistry and Health SEGH2023, Athens, Greece
Society for Environmental Geochemistry and Health., 111-111.
https://hdl.handle.net/21.15107/rcub_agrospace_6767

Djordjević A, Grujic G, Kaluđerović L, Bogosavljević J, Đorđević S. Geochemical origin of Ni and Cr in ranker-type soils formed on serpentinites  massifs in Serbia. in 38th International Conference on Geochemistry and Health SEGH2023, Athens, Greece. 2023;:111-111.
https://hdl.handle.net/21.15107/rcub_agrospace_6767 .

Djordjević, Aleksandar, Grujic, Gordana, Kaluđerović, Lazar, Bogosavljević, Jelena, Đorđević, Snežana, "Geochemical origin of Ni and Cr in ranker-type soils formed on serpentinites  massifs in Serbia" in 38th International Conference on Geochemistry and Health SEGH2023, Athens, Greece (2023):111-111,
https://hdl.handle.net/21.15107/rcub_agrospace_6767 .