Partition of geogenic nickel in paddy soils derived from serpentinites
Tóm tắt
Serpentinitic soils contain high concentrations of geogenic Ni. During serpentinitic mineral weathering, the Ni released from soils into ecosystems could be a source of non-anthropogenic metal contamination. In this study, soil samples were collected from two pedons in paddy fields in Taiwan and Japan; these samples were used to explore the profile distribution of total and labile Ni, demonstrating the contribution of Ni-bearing Fe and Mn oxides to the Ni partition in these soils. Serpentine and chlorite were the dominant primary minerals; thus, the soils reflected serpentinitic characteristics and exhibited high background concentrations of Ni. The total Ni content ranged from 240 to 520 mg kg−1. Repeated redox and leaching cycles caused the redistribution of Ni in the paddy soils. The diethylenetriamine pentaacetate (DTPA)-extractable Ni, an availability index of Ni, increased as the soil depth decreased in the two pedons. An additional pool of labile Ni was present in the soils because the Ni concentration determined using a 0.1 N HCl extraction was much higher than was that determined using the DTPA extraction. Fe and Mn oxides were closely related to the labile Ni in these paddy soils. However, Ni was predominantly retained by amorphous and crystalline Fe oxides rather than Mn oxides. Shortening the flooded duration of paddy field is required to reduce the solubility of Ni because that the labile Ni and redox-sensitive Fe oxides can affect both the paddy soils and environment when Ni is released into the soil solution and becomes bioavailable under reducing conditions.
Tài liệu tham khảo
Adriano DC (1986) Trace elements in the terrestrial environment. Springer, New York
Alves S, Trancoso MA, Goncalves MLS, Santos MMC (2011) A nickel availability study in serpentinised areas of Portugal. Geoderma 164:115–163
Amir H, Pineau R (1998) Effects of metals on the germination and growth of fungal isolates from New Caledonian ultramafic soils. Soil Biol Biochem 30:2043–2054
Anda M (2012) Cation imbalance and heavy metal contents of seven Indonesian soils affected by elemental compositions of parent rocks. Geoderma 189–190:388–396
Antić-Mladenović S, Rinklebe J, Frohne T, Stärk HJ, Wennrich R, Tomić Z, Ličina V (2011) Impact of controlled redox conditions on nickel in a serpentine soil. J Soils Sediments 11:406–415
Baker DE, Amacher MC (1982) Nickel, copper, zinc, and cadmium. In: Keeney DR (ed) Methods of soil analysis, Part 2. Chemical and microbiological properties, Agronomy Monograph 9, 2nd edn. Agronomy Society of America and Soil Science Society of America, Madison, pp 323–336
Becquer T, Quantin C, Rotté-Capet S, Ghanbaja J, Mustin C, Herbillon AJ (2006) Sources of trace metals in ferralsols in New Caledonia. Eur J Soil Sci 57:200–213
Blume HP, Schwertmann U (1969) Genetic evaluation of profile distribution of aluminum, iron, and manganese oxides. Soil Sci Soc Am Proc 33:438–444
Brooks RR (1987) Serpentine and its vegetation: a multidisciplinary approach. Croom Helm, London, p 454
Caillaud J, Proust D, Righi D (2006) Weathering sequences of rock-forming minerals in a serpentinite: influence of microsystems on clay mineralogy. Clays Clay Miner 54:87–100
Chang YT, Hseu ZY, Iizuka Y, Yu CD (2013) Morphology, geochemistry, and mineralogy of serpentine soils under the tropical forest in southeastern Taiwan. Taiwan J For Sci 28:185–201
Chardot V, Echevarria G, Gury M, Massoura S, Morel JL (2007) Nickel bioavailability in an ultramafic toposequence in the Vosges Mountains (France). Plant Soil 293:7–21
Cheng CH, Jien SH, Tsai H, Chang YH, Chen YC, Hseu ZY (2009) Geochemical element differentiation in serpentine soils from the ophiolite complexes, eastern Taiwan. Soil Sci 174:283–291
Cheng CH, Jien SH, Iizuka Y, Tsai H, Chang YS, Hseu ZY (2011) Pedogenic chromium and nickel partitioning in serpentine soils along a toposequence. Soil Sci Soc Am J 75:659–668
Cornu S, Deschatrettes V, Salvador-Blanes S, Clozel B, Hardy M, Branchut S, Le Forestier L (2005) Trace element accumulation in Mn–Fe-oxide nodules of a planosolic horizon. Geoderma 125:11–24
Eswaran H, van den Berg E, Reich P (1993) Organic carbon in soils of the world. Soil Sci Soc Am J 57:192–194
Gambrell RP (1996) Manganese. In: Sparks DL (ed) Methods of soil analysis, Part 3. Chemical methods. Agronomy Society of America and Soil Science Society of America, Madison, pp 665–682
Gee GW, Bauder JW (1986) Particle-size analysis. In: Klut A (ed) Methods of soil analysis, Part 1. Physical and mineralogical methods. Agronomy Monograph 9, 2nd edn. Agronomy Society of America and Soil Science Society of America, Madison, pp 383–411
Ho CP, Hseu ZY, Chen NC, Tsai CC (2013) Evaluating heavy metal concentration of plants on a serpentine site for phytoremediation applications. Environ Earth Sci 70:191–199
Hseu ZY (2006) Concentration and distribution of chromium and nickel fractions along a serpentinitic toposequence. Soil Sci 171:341–353
Hseu ZY, Iizuka Y (2013) Pedogeochemical characteristics of chromite in a paddy soil derived from serpentinites. Geoderma 202–203:126–133
Hseu ZY, Tsai H, Hsi HC, Chen YC (2007) Weathering sequences of clay minerals in soils along a serpentinitic toposequence. Clays Clay Miner 55:389–401
Hseu ZY, Su SW, Lai HY, Guo HY, Chen TC, Chen ZS (2010) Remediation techniques and heavy metals uptake by different rice varieties in metals-contaminated soils of Taiwan: new aspects for food safety regulation and sustainable agriculture. Soil Sci Plant Nutr 56:31–52
Hsiao KH, Kao PH, Hseu ZY (2007) Effects of chelators on chromium and nickel uptake by Brassica juncea on serpentine-mine tailings for phytoextraction. J Hazard Mater 148:366–376
Johnston WR, Proctor J (1981) Growth of serpentine and non-serpentine races of Festuca rubra in solutions simulating the chemical conditions in a toxic serpentine soil. J Ecol 69:855–869
Kabata-Pendias A, Pendias H (2001) Trace elements in soils and plants. CRC Press, New York
Kelepertzis E, Galanos E, Mitsis I (2013) Origin, mineral speciation and geochemical baseline mapping of Ni and Cr in agricultural topsoils of Thiva valley (central Greece). J Geochem Explor 150:56–68
Kierczak J, Neel C, Aleksander-Kwaterczak U, Helios-Rybicka E, Bril H, Puziewicz J (2008) Solid speciation and mobility of potentially toxic elements from natural and contaminated soils: a combined approach. Chemosphere 73:776–784
Kögel-Knabner I, Amelung W, Cao Z, Fiedler S, Frenzel P, Jahn R, Kalbitz K, Kölbl A, Schloter M (2010) Biogeochemistry of paddy soils. Geoderma 157:1–14
Kyuma K (2004) Paddy soil science. Kyoto University Press, Kyoto
Lee BD, Graham RC, Laurent TE, Amrhein C, Creasy RM (2001) Spatial distribution of soil chemical conditions in a serpentinitic wetland and surrounding landscape. Soil Sci Soc Am J 65:1183–1196
Licina V, Antic-Mladenovic S, Kresovic M, Rinklebe J (2010) Effect of high nickel and chromium background levels in serpentine soil on their accumulation in organs of a perennial plant. Commun Soil Sci Plant Anal 41:482–496
Lindsay WL, Norvell WA (1978) Development of DTPA soil test for Zn, Fe, Mn, Cu. Soil Sci Soc Am J 42:421–428
Massoura ST, Echevarria G, Becquer T, Ghambaja J, Leclerc-Cessac E, Morel JL (2006) Nickel bearing phases and availability in natural and anthropogenic soils. Geoderma 136:28–37
McGahan DG, Southard RJ, Claassen VP (2008) Tectonic inclusions in serpentinite landscapes contribute plant nutrient calcium. Soil Sci Soc Am 72:838–847
McGahan DG, Southard RJ, Claassen VP (2009) Plant-available calcium varies widely in soils on serpentinite landscapes. Soil Sci Soc Am J 73:2087–2095
McGrath SP (1995) Chromium and nickel. In: Alloway BW (ed) Heavy metals in soils, 2nd edn. Blackie Academic and Professional, London, pp 152–178
McKeague JA, Day JH (1966) Dithionite and oxalate extractable Fe and Al as aids in differentiating various classes of soils. Can J Soil Sci 46:13–22
McLean EO (1982) Soil pH and lime requirement. In: Page AL, Miller RH, Keeney DR (eds) Methods of soil analysis, Part 2. Chemical and microbiological properties, Agronomy Monograph 9, 2nd edn. Agronomy Society of America and Soil Science Society of America, Madison, pp 199–224
Mehra OP, Jackson ML (1960) Iron oxides removed from soils and clays by a dithionite–citrate system buffered with sodium bicarbonate. Clays Clay Miner 7:317–327
Mizuno N, Kobayashi S (1971) Several trace element in serpentine paddy soil - Effect of Ni on rice plant growth with reference to contents of Mn, Fe, Cu, Zn and Mo in rice plants and soil. J Sci Soil Manure Jpn 42:214–220 (Japanese with English abstract)
Nelson DW, Sommers LE (1982) Total carbon, organic carbon, and organic matter. In: Page AL, Miller RH, Keeney DR (eds) Methods of soil analysis, Part 2. Chemical and microbiological properties, Agronomy Monograph 9, 2nd edn. Agronomy Society of America and Soil Science Society of America, Madison, pp 539–577
O’Hanley DS (1996) Serpentinites: Records of tectonic and petrological history. Oxford University Press, New York
Oze C, Fendorf S, Bird DK, Coleman RG (2004) Chromium geochemistry of serpentine soils. Intern Geol Rev 46:97–126
Quantin C, Ettler V, Garnier J, Šebek O (2008) Sources and extractibility of chromium and nickel in soil profiles developed on Czech serpentinites. Compt Rendus Geosci 340:872–882
Reeves RD, Baker AJM, Borhidi A, Berazaìn R (1999) Nickel hyperaccumulation in the serpentine flora of Cuba. Ann Bot 83:29–38
Rhoades JD (1982) Cation exchange capacity. In: Page AL, Miller RH, Keeney DR (eds) Methods of soil analysis, Part 2. Chemical and microbiological properties, Agronomy Monograph 9, 2nd edn. Agronomy Society of America and Soil Science Society of America, Madison, pp 149–157
Soil Survey Staff (2010) Keys to soil taxonomy, 12th edn. Natural Resources Conversation Services, United States Department of Agriculture, Washington
Ünver I, Madenoglu S, Dilsiz A, Namli A (2013) Influence of rainfall and temperature on DTPA extractable nickel content of serpentine soils in Turkey. Geoderma 202–203:203–211