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Chemical Speciation of Heavy Metals in the Fractionated Rhizosphere Soils of Sunflower Cultivated in a Humic Andosol

机译:腐殖质雄茄培养的向日葵根际分离土壤中重金属的化学形态。

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Chemical speciation and bioaccumulation factor of iron (Fe), manganese (Mn), and zinc (Zn) were investigated in the fractionated rhizosphere soils and tissues of sunflower plants grown in a humic Andosol. The experiment was conducted for a period of 35 days in the greenhouse, and at harvest the soil system was differentiated into bulk, rhizosphere, and rhizoplane soils based on the collection of root-attaching soil aggregates. The chemical speciations of heavy metals in the soil samples were determined after extraction sequentially into fractions classified as exchangeable, carbonate bound, metal-organic complex bound, easily reducible metal oxide bound, hydrogen peroxide (H2O2)-extractable organically bound, amorphous mineral colloid bound, and crystalline Fe oxide bound. Iron and Zn were predominantly crystalline Fe oxide bound in the initial bulk soils whereas Mn was mainly organically bound. Heavy metals in the exchangeable form accumulated in the rhizosphere and rhizoplane soils, comprising <4% of the total content, suggesting their relatively low availability in humic Andosol. Concentrations of organically bound Fe and Mn in soils decreased with the proximity to roots, suggesting that organic fraction is the main source for plant uptake. Concentrations of Mn and Zn in the metal-organic complex also decreased, indicating a greater ability of sunflower to access Mn from more soil pools. Sunflower showed bioaccumulation factors for Zn, Fe, and Mn as large as 0.39, 0.05, and 0.04 respectively, defining the plant as a metal excluder species. This result suggests that access to multiple metal pools in soil is not necessarily a major factor that governs metal accumulation in the plant.View full textDownload full textKeywordsBioaccumulation factor, Helianthus annus L., micronutrient availability, rhizosphere chemistry, trace elements speciationRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00103624.2012.701686
机译:研究了腐殖质Andosol中分馏的根际土壤和向日葵植物组织中铁(Fe),锰(Mn)和锌(Zn)的化学形态和生物富集因子。该实验在温室中进行了35天,在收获时,根据附着根系的土壤团聚体,将土壤系统分为块状,根际和根状土壤。依次萃取成可交换的,碳酸盐结合的,金属-有机络合物结合的,易还原的金属氧化物结合的,过氧化氢的(H 2 O < sub> 2 )-可萃取的有机结合,无定形矿物胶体结合和结晶氧化铁结合。铁和锌主要是结晶的氧化铁,结合在最初的块状土壤中,而锰则主要是有机结合。重金属以可交换形式积累在根际和根际土壤中,占总含量的<4%,表明它们在腐殖质安多索中的利用率相对较低。土壤中有机结合的Fe和Mn的浓度随接近根部而降低,这表明有机质是植物吸收的主要来源。金属-有机配合物中锰和锌的浓度也降低了,表明向日葵从更多的土壤库中吸收锰的能力更高。向日葵显示出的锌,铁和锰的生物蓄积系数分别高达0.39、0.05和0.04,这将植物定义为金属排斥物种。该结果表明,进入土壤中的多个金属池并不一定是控制植物中金属积累的主要因素。查看全文下载全文关键词生物积累因子,向日葵,微量营养素有效性,根际化学,微量元素形态相关var addthis_config = { ui_cobrand:“ Taylor&Francis Online”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”,发布:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/00103624.2012.701686

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