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The solid phase distribution and bioaccessibility of potentially harmful elements in natural ironstone soils in the UK

机译:英国天然铁矿石中潜在有害元素的固相分布和生物可接近性

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摘要

Chemical reactions and physical and biological processes influence the mobility of potentially harmful elements (PHEs) present within soils. In the UK, soil PHE such as arsenic (As), chromium (Cr) and nickel (Ni) occur at elevated concentrations in soils derived from ironstone parent materials. Exposure to soil PHE via oral ingestion, inhalation or dermal uptake poses a potential risk to human health. However, PHE mobility in soils is governed by its solid phase distribution within the soil matrix and therefore the presence of PHE may not indicate a risk to human health. ududThis study examines the geochemical forms of As, Cr Ni, found in ironstone derived topsoils from north Oxfordshire in the UK, where total concentrations were in the range 14.0 – 417 mg kg-1 As, 51.0 – 447 mg kg-1 Cr and 17.0 – 218 mg kg-1 Ni. Solid phase distribution information was determined by the application of a non-specfic sequential extraction methodology combined with self modelling mixture resolution of the concentrations of elements in the extract solutions, determined by ICP-AES. Seven distinct physico-chemical components, including iron (Fe), manganese (Mn) and aluminium (Al) oxides, calcium (Ca) carbonates, organic and fertilizer sources were identified in the Oxfordshire soils, all of which were identified as being hosts to one or more of the PHE of interest. Estimates of PHE intake via the oral ingestion route were determined using an in vitro physiologically based gastro-intestinal simulation bioacessibility test. Bioaccessible PHE concentrations ranged from 1.60 – 12.8 mg kg-1 As, 0.55 – 2.02 mg kg-1 Cr and 1.18 – 4.52 mg kg-1 Ni. The combination of bioaccessobility data with mobility/solid phase distribution information provided by the sequentional extraction methodology indicates that: Fe oxides are the predominant host of immobile As and Cr; mobile As is associated with carbonates and organic phases; relatively mobile Cr with Mn/Al oxides; mobile/relatively mobile Ni is predominant in Al/Mn oxide components and carbonate soil components. The coupling of sequential extraction and bioaccessibility techniques provides a robust approach to understanding the relationship between PHE mobility and the potential human health risks from soil exposure via ingestion.ud
机译:化学反应以及物理和生物过程会影响土壤中潜在有害元素(PHE)的迁移。在英国,从铁矿石母体材料衍生的土壤中,砷(As),铬(Cr)和镍(Ni)等土壤PHE的浓度较高。通过口服摄入,吸入或皮肤吸收接触土壤PHE会对人体健康构成潜在风险。但是,PHE在土壤中的流动性受其在土壤基质中的固相分布控制,因此,PHE的存在可能并不表示对人体健康构成威胁。 ud ud这项研究研究了在英国牛津郡北部铁矿石衍生的表层土壤中发现的As,Cr Ni的地球化学形式,该地区的总浓度为14.0 – 417 mg kg-1 As,51.0 – 447 mg kg-1铬和17.0 – 218 mg kg-1 Ni。固相分布信息是通过应用非特定的顺序萃取方法,并结合通过ICP-AES测定萃取液中元素浓度的自建模混合物分辨率来确定的。在牛津郡的土壤中鉴定出七个不同的理化成分,包括铁(Fe),锰(Mn)和铝(Al)氧化物,碳酸钙(Ca),有机和肥料来源,所有这些成分均被认为是土壤的寄主一个或多个相关的PHE。使用基于体外生理学的胃肠道模拟生物可及性测试,确定通过口服摄入途径摄入的PHE的估算值。生物可及的PHE浓度范围为1.60 – 12.8 mg kg-1 As,0.55 – 2.02 mg kg-1 Cr和1.18 – 4.52 mg kg-1 Ni。相继提取方法提供的生物可及性数据与迁移率/固相分布信息的结合表明:Fe氧化物是固定态As和Cr的主要宿主;与碳酸盐和有机相相关的移动砷;相对移动的Cr和Mn / Al氧化物;流动/相对流动的Ni在Al / Mn氧化物组分和碳酸盐土壤组分中占主导地位。顺序提取和生物可及性技术的结合为了解PHE流动性与通过摄入土壤暴露的潜在人类健康风险之间的关系提供了一种可靠的方法。

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  • 作者

    Wragg Joanna;

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  • 年度 2012
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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