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Biogeochemistry of Ni and Pb in a periodically flooded arable soil: Fractionation and redox-induced (im)mobilization.
J Environ Manage. 2017 Jan 15; 186(Pt 2):141-150.JE

Abstract

The redox-induced (im)mobilization of nickel (Ni) and lead (Pb) under pre-definite redox conditions and their binding forms were studied in a periodically flooded, slightly acidic arable soil enriched with serpentine minerals at the Velika Morava River valley, Serbia. The total contents of Ni and Pb were 152 and 109 mg kg-1, respectively. Geochemical fractionation of Ni, combined with mineralogical analysis, confirmed its geogenic origin in the soil. Potentially mobile fractions were the dominating binding forms of Pb; thus, indicating anthropogenic sources as prevailing. Risk assessment indicated a low risk of Ni and Pb transfer from soil to other environmental constituents. However, the results imply that geogenic metals might pose higher environmental risk than those from anthropogenic origin, in dependence of their total concentrations and contents in the specific solid-phase fractions. Flooding of the soil was simulated in an automated biogeochemical microcosm system, which allows a control and a continuous measurements of redox potential (EH) and pH. Subsequently, the EH was increased in steps of approximately 100 mV from anoxic to oxic conditions. Concurrently, the concentrations of soluble Ni, Pb, iron (Fe), manganese (Mn), dissolved organic carbon (DOC), and sulfates were measured. The EH was brought from low to high values (-220 to 520 mV) and correlated negative with soluble Ni, Pb, Fe, Mn and DOC. Soluble Ni ranged from 125 to 228 μg l-1 while Pb ranged from 3.0 to 21.4 μg l-1. Concentrations of both metals in solution were high at low EH and decreased with increasing EH. Nickel immobilization may be attributed to sorption to or co-precipitation with re-oxidized Fe-Mn (hydr)oxides, whereas Pb, in addition, might be immobilized via precipitation with inorganic ligands, such as carbonates and phosphates. The results imply that Ni and Pb solubility might also be related to the formation of metal-DOC complexes. The detected dynamic and mechanisms might be useful in providing critical information for assessing the potential environmental risk and creating appropriate environmental management strategies for agricultural areas enriched with Ni and Pb.

Authors+Show Affiliations

University of Belgrade-Faculty of Agriculture, Nemanjina 6, 11 080 Belgrade, Serbia. Electronic address: santic@agrif.bg.ac.rs.University of Bielefeld, Department I: Planning and Controlling, Universitätsstraβe 25, 33615 Bielefeld, Germany; University of Wuppertal, Soil- and Groundwater-Management, Pauluskirchstraβe 7, 42285 Wuppertal, Germany.University of Belgrade-Faculty of Agriculture, Nemanjina 6, 11 080 Belgrade, Serbia.UFZ - Helmholtz Centre for Environmental Research, Department of Analytical Chemistry, Permoserstr. 15, 04318 Leipzig, Germany.University of Belgrade-Faculty of Agriculture, Nemanjina 6, 11 080 Belgrade, Serbia.University of Belgrade-Faculty of Agriculture, Nemanjina 6, 11 080 Belgrade, Serbia.University of Wuppertal, Soil- and Groundwater-Management, Pauluskirchstraβe 7, 42285 Wuppertal, Germany.

Pub Type(s)

Journal Article

Language

eng

PubMed ID

27318758

Citation

Antić-Mladenović, Svetlana, et al. "Biogeochemistry of Ni and Pb in a Periodically Flooded Arable Soil: Fractionation and Redox-induced (im)mobilization." Journal of Environmental Management, vol. 186, no. Pt 2, 2017, pp. 141-150.
Antić-Mladenović S, Frohne T, Kresović M, et al. Biogeochemistry of Ni and Pb in a periodically flooded arable soil: Fractionation and redox-induced (im)mobilization. J Environ Manage. 2017;186(Pt 2):141-150.
Antić-Mladenović, S., Frohne, T., Kresović, M., Stärk, H. J., Tomić, Z., Ličina, V., & Rinklebe, J. (2017). Biogeochemistry of Ni and Pb in a periodically flooded arable soil: Fractionation and redox-induced (im)mobilization. Journal of Environmental Management, 186(Pt 2), 141-150. https://doi.org/10.1016/j.jenvman.2016.06.005
Antić-Mladenović S, et al. Biogeochemistry of Ni and Pb in a Periodically Flooded Arable Soil: Fractionation and Redox-induced (im)mobilization. J Environ Manage. 2017 Jan 15;186(Pt 2):141-150. PubMed PMID: 27318758.
* Article titles in AMA citation format should be in sentence-case
TY - JOUR T1 - Biogeochemistry of Ni and Pb in a periodically flooded arable soil: Fractionation and redox-induced (im)mobilization. AU - Antić-Mladenović,Svetlana, AU - Frohne,Tina, AU - Kresović,Mirjana, AU - Stärk,Hans-Joachim, AU - Tomić,Zorica, AU - Ličina,Vlado, AU - Rinklebe,Jörg, Y1 - 2016/06/16/ PY - 2016/02/19/received PY - 2016/06/03/revised PY - 2016/06/04/accepted PY - 2016/6/20/pubmed PY - 2017/3/14/medline PY - 2016/6/20/entrez KW - DOC KW - Metals KW - Redox potential KW - Solubility KW - Sources SP - 141 EP - 150 JF - Journal of environmental management JO - J Environ Manage VL - 186 IS - Pt 2 N2 - The redox-induced (im)mobilization of nickel (Ni) and lead (Pb) under pre-definite redox conditions and their binding forms were studied in a periodically flooded, slightly acidic arable soil enriched with serpentine minerals at the Velika Morava River valley, Serbia. The total contents of Ni and Pb were 152 and 109 mg kg-1, respectively. Geochemical fractionation of Ni, combined with mineralogical analysis, confirmed its geogenic origin in the soil. Potentially mobile fractions were the dominating binding forms of Pb; thus, indicating anthropogenic sources as prevailing. Risk assessment indicated a low risk of Ni and Pb transfer from soil to other environmental constituents. However, the results imply that geogenic metals might pose higher environmental risk than those from anthropogenic origin, in dependence of their total concentrations and contents in the specific solid-phase fractions. Flooding of the soil was simulated in an automated biogeochemical microcosm system, which allows a control and a continuous measurements of redox potential (EH) and pH. Subsequently, the EH was increased in steps of approximately 100 mV from anoxic to oxic conditions. Concurrently, the concentrations of soluble Ni, Pb, iron (Fe), manganese (Mn), dissolved organic carbon (DOC), and sulfates were measured. The EH was brought from low to high values (-220 to 520 mV) and correlated negative with soluble Ni, Pb, Fe, Mn and DOC. Soluble Ni ranged from 125 to 228 μg l-1 while Pb ranged from 3.0 to 21.4 μg l-1. Concentrations of both metals in solution were high at low EH and decreased with increasing EH. Nickel immobilization may be attributed to sorption to or co-precipitation with re-oxidized Fe-Mn (hydr)oxides, whereas Pb, in addition, might be immobilized via precipitation with inorganic ligands, such as carbonates and phosphates. The results imply that Ni and Pb solubility might also be related to the formation of metal-DOC complexes. The detected dynamic and mechanisms might be useful in providing critical information for assessing the potential environmental risk and creating appropriate environmental management strategies for agricultural areas enriched with Ni and Pb. SN - 1095-8630 UR - https://www.unboundmedicine.com/medline/citation/27318758/Biogeochemistry_of_Ni_and_Pb_in_a_periodically_flooded_arable_soil:_Fractionation_and_redox_induced__im_mobilization_ DB - PRIME DP - Unbound Medicine ER -