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Original scientific article

CHROMIUM AND NICKEL IN SOIL IN THE WIDER MAGLAJ AREA – CONCENTRATION AND GENESIS

By
Elvir Babajić ,
Elvir Babajić
Contact Elvir Babajić

Geology, Faculty of Mining, Geology and Civil Enginnering, University of Tuzla, Tuzla, Bosnia and Herzegovina

Alisa Babajić ,
Alisa Babajić

Geology, Faculty of Mining, Geology and Civil Enginnering, University of Tuzla, Tuzla, Bosnia and Herzegovina

Željka Stjepić Srkalović ,
Željka Stjepić Srkalović

Geography, Faculty of Science, University of Tuzla, Tuzla, Bosnia and Herzegovina

Dado Srkalović ,
Dado Srkalović

Geology, Faculty of Mining, Geology and Civil Enginnering, University of Tuzla, Tuzla, Bosnia and Herzegovina

Samir Ustalić ,
Samir Ustalić

Geology, Faculty of Mining, Geology and Civil Enginnering, University of Tuzla, Tuzla, Bosnia and Herzegovina

Husnija Akmadžić
Husnija Akmadžić

Geology, Faculty of Mining, Geology and Civil Enginnering, University of Tuzla, Tuzla, Bosnia and Herzegovina

Abstract

Research on potentially toxic elements chromium and nickel and laboratory testing of their concentrations was carried out in the wider area of Maglaj, with the aim to detect and determine their quantities, which gave basis for discussion about origins of these pollutants in soil. Field and laboratory observations included 45 soil samples, taken by the network, which is dictated by geomorphological conditions. The most frequently sampled type of soil are fluvisol and humofluvisol. Concentration of chromium (Cr) and nickel (Ni) are obtained by the most sophisticated laboratory method (ICP-MS), with a highly sensitive detection threshold (0.1 to 10,000 ppm). 

Evaluation of test results showed that concentrations of Cr (max. 954 ppm, min 154 ppm, average 457.5 pmm) and Ni (max 504.5 ppm, min 103.5 ppm; average 275.57 pmm) are significantly increased compared to the concentrations prescribed in the Regulations on determination of allowed amounts of harmful and hazardous substances in soil (Cr max = 100 ppm and Ni max = 50 ppm). Considering geological settings of surrounding area (the dominant presence of igneous ultramafic and mafic rocks) it can be concluded that high concentrations of Cr and Ni have geogenic origins, what is mean that they originate from source rocks from which they are separated through the long-term decomposition and disintegration processes.

References

[{"id":2145,"citationNumber":"1","type":"journal-article","title":"Pedologija. Zavod za ud\u017ebenike i nastavna sredstva","DOI":null,"author":[{"given":"M.","family":"\u0106iri\u0107"}],"issued":{"date-parts":["1991"]},"container-title":null,"volume":null,"issue":null,"page":null}]

[{"id":2146,"citationNumber":"2","type":"chapter","title":"Tuma\u010d za osnovnu geolo\u0161ku kartu, list Zavidovi\u0107i 1:100 000","DOI":null,"author":[{"given":"J.","family":"Pami\u0107"},{"given":"O.","family":"Sunari\u0107-Pami\u0107"},{"given":"I.","family":"Kapeler"},{"given":"J.","family":"Oluji\u0107"}],"issued":{"date-parts":["1966"]},"container-title":"Institut za geolo\u0161ka istra\u017eivanja","volume":null,"issue":null,"page":null}]

[{"id":2147,"citationNumber":"3","type":"chapter","title":"Osnovna geolo\u0161ka kartu, list Zavidovi\u0107i 1:100 000","DOI":null,"author":[{"given":"O.","family":"Sunari\u0107-Pami\u0107"},{"given":"J.","family":"Pami\u0107"},{"given":"I.","family":"Kapeler"},{"given":"J.","family":"Oluji\u0107"},{"given":"F.","family":"Zec"}],"issued":{"date-parts":["1966"]},"container-title":"Institut za geolo\u0161ka istra\u017eivanja","volume":null,"issue":null,"page":null}]

[{"id":2148,"citationNumber":"4","type":"book","title":"Pedogeografija","DOI":null,"author":[{"given":"S.","family":"Ahmetbegovi\u0107"},{"given":"\u017d.","family":"Stjepi\u0107 Srkalovi\u0107"},{"given":"S.","family":"Guti\u0107"}],"issued":{"date-parts":["2017"]},"container-title":null,"volume":null,"issue":null,"page":null}]

[{"id":2149,"citationNumber":"5","type":"article-journal","title":"Soil pollution in day-care centers and playgrounds in Norway: national action plan for mapping and remediation","DOI":null,"author":[{"given":"R.T.","family":"Ottesen"},{"given":"J.","family":"Alexander"},{"given":"M.","family":"Langedal"},{"given":"T.","family":"Haugland"},{"given":"E.","family":"H\u00f8ygaard"}],"issued":{"date-parts":["2008"]},"container-title":"Enviromental","volume":null,"issue":null,"page":null}]

[{"id":2150,"citationNumber":"6","type":"book","title":"Geokemijski atlas Siska","DOI":null,"author":[{"given":"Ajka","family":"\u0160or\u0161a"},{"given":"J.","family":"Halami\u0107"}],"issued":{"date-parts":["2014"]},"container-title":null,"volume":null,"issue":null,"page":null}]

[{"id":2151,"citationNumber":"7","type":"chapter","title":"Geokemijski atlas Republike Hrvatske","DOI":null,"author":[{"given":"J.","family":"Halami\u0107"},{"given":"S.","family":"Miko"}],"issued":{"date-parts":["2009"]},"container-title":"Hrvatski geolo\u0161ki Insitut","volume":null,"issue":null,"page":null}]

[{"id":2152,"citationNumber":"8","type":"journal-article","title":"Geohemija. Rudarsko-geolo\u0161ki fakultet Univerziteta u Tuzli","DOI":null,"author":[{"given":"I.","family":"Kubat"}],"issued":{"date-parts":["1997"]},"container-title":null,"volume":null,"issue":null,"page":null}]

[{"id":2153,"citationNumber":"9","type":"article-journal","title":"The ecology of serpentine soils","DOI":null,"author":[{"given":"R.H.","family":"Whittaker"}],"issued":{"date-parts":["1954"]},"container-title":"Ecology","volume":"35","issue":"2","page":"258\u2013288"}]

[{"id":2154,"citationNumber":"10","type":"article-journal","title":"Distribution of Chromium and Nickel in Plants and Soil from Serpentine and Other Sites","DOI":null,"author":[{"given":"P.R.Aad Peterson","family":"Shewry"},{"given":"P.J.","family":""}],"issued":{"date-parts":["1976"]},"container-title":"Journal of Ecology. Vlol","volume":"64","issue":"1","page":"195\u2013212"}]

[{"id":2155,"citationNumber":"11","type":"article-journal","title":"Sources and extractibility of chromium and nickel in soil profiles developed on Czech serpentinites","DOI":null,"author":[{"given":"C.","family":"Quantin"},{"given":"V.","family":"Ettler"},{"given":"J.","family":"Garnier"},{"given":"O.","family":"\u0160ebek"}],"issued":{"date-parts":["2008"]},"container-title":"Comptes Rendus Geosience","volume":"340","issue":"ue 12","page":"872\u2013882"}]

[{"id":2156,"citationNumber":"12","type":"article-journal","title":"Metal accumulation in cattle raised in a serpentine-soil area: Relationship between metal concentrations in soil, forage and animal tissues\"","DOI":null,"author":[{"given":"M.Benedito","family":"Miranda"},{"given":"J.L.","family":"Blanco-Penedo"},{"given":"I.","family":"L\u00f3pez-Lamas"},{"given":"C.","family":"Merino"},{"given":"A.","family":"L\u00f3pez-Alonso"},{"given":"M.","family":""}],"issued":{"date-parts":["2009"]},"container-title":"Journal of Trace Elements in Medicine and Biology","volume":"23","issue":"3","page":"231"}]

[{"id":2157,"citationNumber":"13","type":"book","title":"Weathering and transport of chromium and nickel from serpentinite in the Coast Range ophiolite to the","DOI":null,"author":[],"issued":{"date-parts":["2015"]},"container-title":null,"volume":"62","issue":null,"page":"72\u201386"}]

[{"id":2158,"citationNumber":"14","type":"chapter","title":"Pravilnik o utvr\u0111ivanju dozvoljenih koli\u010dina \u0161tetnih i opasnih tvari u zemlji\u0161tu i metode njihovog ispitivanja","DOI":null,"author":[],"issued":{"date-parts":[null]},"container-title":"Slu\u017ebene novine Federacije Bosne i Hercegovine, broj 72\/09.2009. godine","volume":null,"issue":null,"page":null}]

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