Scholarly record
TOTAL HEAVY METAL CONTENTS IN SERPENTINITE SOILS FROM TURKOGLU-KAHRAMANMARAS/TURKEY
Abstract
In this study, total heavy metal distributions in serpentinite soils from T?rko?lu-Kahramanmara? region SE Turkey were investigated. Common ultramafic rock types (dunite, harzburgite, lherzolite, wehrlite) and the secondary alteration products formed by their hydration within the Earth?s crust (serpentinite) are the primary source of serpentinite soils. The characteristics of soils developed on serpentinite and peridotite differ from other soils. Numerous studies have reported that typical heavy metal enrichment in ultramafic soils. Serpentinite-derived soils have high concentrations of Cr and Ni from the parent materials and carry a risk to human health and environmental quality. Soils contaminated with heavy metals represent an escalating problem for all living organisms, such as plants, animals and humans. A total of 15 soil samples were taken from 0-30 cm depth which developed on serpentinite and peridotite parent materials in T?rko?lu district in the South of Kahramanmara? city. Collected soil samples were air-dried, thereafter breaking the agglomerates by using a wood hammer, then sieved through a 100 ? sieve and stored in plastic bags. Later, the concentration of heavy metals including Ni, Cr, Co, Fe and Mn were measured using an X-ray fluorescence. According to the obtained datas, the total Cr, Ni, Co, Mn and Fe contents of the soils varied from 2085 to 5644 mgkg-1, 1595 to 2833 mgkg-1,103 to 187 mgkg-1, 922 to 1680 mgkg-1, 9.49 to 15.83 %, respectively. This study revealed that serpentinite soils are characterized by high concentrations of heavy metals such as Ni, Cr, Co, Mn and Fe. This high level of Ni, Cr, Fe, Mn and Co is obviously toxic and can adversely affect plant growth. Concentrations of Fe, Ni, Cr, Mn and Co were very high and present in the order of Fe>Cr>Ni>Mn>Co. Heavy metals which accumulate in the different plant parts results in the toxicity of plants. Chromium at higher concentrations becomes toxic for the plants and results in the detrimental effect. High concentrations of Ni in plants are toxic and causes severe chlorosis and necrosis and host of other growth abnormalities and anatomical changes. In areas where such heavy metal concentrations are above the limit values, the cultivation of plant species accumulating heavy metals in the root zone is important for environment, human and plant health.
Publication Impact Profile
Publication details
References15
Morrison, J.M., M.B. Goldhaber, L. Lee, J.M. Holloway and R.B. Wanty et al., 2009. A regional-scale study of chromium and nickel in soils of northern California, USA. Applied Geochem., 24: 1500-1511.
Oze, C., Fendorf, S., Bird, D.K. and Coleman, R.G. (2004b) Chromium geochemistry of serpentine soils. International Geology Review, 46: 97-126.
Brooks, R. R., 1987, Serpentine and its vegetation: Portland, OR, Dioscorides Press, 454 p.
Cheng, C.-H., Jien, S.-H., Iizuka, Y., Tsai, H., Chang, Y.-H., Hseu, Z.-Y., 2011. Pedogenic chromium and nickel partitioning in serpentine soils along a toposequence. Soil Science Society of America Journal 75 (2), 659–668.
Siebecker, M., 2010. Nickel speciation in serpentine soils using synchrotron radiation techniques. Proceedings of the 19th World Congress of Soil Science, Soil Solutions for a Changing World, Aug. 1-6, DVD, Brisbane, Australia, pp: 160-162.
Soane, B.D., And D.H. Saunder. 1959. Nickel and chromium toxicity of serpentine soils in southern Rhodesia. Soil Sci. 88:322-330
Baillie, I.C., Evangelista, P.M. and Inciong, N.B. 2000. Differentiation of upland soils on the Palawan ophiolitic complex, Philippines. Catena 39:283-299
Dağhan, H., 2011. Doğal kaynaklarda ağır metal kirliliğinin insan sağlığı üzerine etkileri. Mustafa Kemal Üniversitesi Ziraat Fakültesi Dergisi, 16(2): 15-25
Vithanage M, Rajapaksha AU, Oze C, Rajakaruna N, Dissanayake CB. 2014 Metal release from serpentine soils in Sri Lanka. Environmental Monitoring and Assessment.;186(6):3415-3429.
Somogyi A, Braun M, Posta J (1997). Comparison Between X-ray Fluorescence and Inductively Coupled Plasma Atomic Emission Spectrometry in the Analysis of Sediment Samples. Spectrochimica Acta Part B, p. 2011-2017.
Lindsay, W.L., Norvell,W.A. 1978. Development of a DTPA soil test forzinc, iron, manganese, and copper. Soil Sci. Soc. Amer. J. 42:421-428.
Nelson, D.W., Sommers, L.E., 1996. Total Carbon, Organic Carbon, and Organic Matter. in D.L. Sparks (Ed) Methods of Soil Analysis, Part 3, Chemical Methods, SSSA Book Series Number 5, SSSA., Madison,WI, s. 961-1011
Demiralay, İ. (1993).Toprak Fiziksel Analizleri Atatürk Ünv. Zir. Fak. Yayınları. No:143 Erzurum
Kabata-Pendias, Mukherjee, ve B Arun. Trace Elements from Soil to Human. Berlin: Springer- Verlag , 2007.
McGrath, S.P. 1995. Chromium and nickel. p. 152–178. In B.J. Alloway (ed.) Heavy metals in soils. 2nd. Blackie Academic and Professional, London.
Citing literature
Number of times cited according to Crossref: 4
View or Download full articleAccess options
SWS access login
Login as SWS Scientific CommitteeLogin as SWS Scientific PartnerLogin as SWS AuthorAuthors and approved SWS contributors will read and export their own linked papers after identity matching by SWS profile, email and SGEM GlobalID.
For librarian assistance: [email protected]
Purchase Instant Access
- Article can be downloaded after successful payment.
- Article may be used according to SWS library access terms.
- Article cannot be redistributed.


