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Open-water and under-ice seasonal variations in trace element content and physicochemical associations in fluvial bed sediment

机译:河床沉积物中微量元素含量和理化联系的露天水和冰底季节变化

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摘要

Across the circumpolar world, intensive anthropogenic activities in the southern reaches of many large, northward-flowing rivers can cause sediment contamination in the downstream depositional environment. The influence of ice cover on concentrations of inorganic contaminants in bed sediment (i.e., sediment quality) is unknown in these rivers, where winter is the dominant season. A geomorphic response unit approach was used to select hydraulically diverse sampling sites across a northern test-case system, the Slave River and delta (Northwest Territories, Canada). Surface sediment samples (top 1cm) were collected from 6 predefined geomorphic response units (12 sites) to assess the relationships between bed sediment physicochemistry (particle size distribution and total organic carbon content) and trace element content (mercury and 18 other trace elements) during open-water conditions. A subset of sites was resampled under-ice to assess the influence of season on these relationships and on total trace element content. Concentrations of the majority of trace elements were strongly correlated with percent fines and proxies for grain size (aluminum and iron), with similar trace element grain size/grain size proxy relationships between seasons. However, finer materials were deposited under ice with associated increases in sediment total organic carbon content and the concentrations of most trace elements investigated. The geomorphic response unit approach was effective at identifying diverse hydrological environments for sampling prior to field operations. Our data demonstrate the need for under-ice sampling to confirm year-round consistency in trace element-geochemical relationships in fluvial systems and to define the upper extremes of these relationships. Whether contaminated or not, under-ice bed sediment can represent a worst-case scenario in terms of trace element concentrations and exposure for sediment-associated organisms in northern fluvial systems. Environ Toxicol Chem 2017;36:2916-2924. (c) 2017 SETAC
机译:在整个极地世界中,许多大的向北流动的河流南部的密集人为活动会在下游沉积环境中造成沉积物污染。在这些冬季是主要季节的河流中,冰盖对床底沉积物中无机污染物浓度(即沉积物质量)的影响尚不清楚。地貌响应单元方法用于在北部测试用例系统,奴隶河和三角洲(加拿大西北地区)中选择水力不同的采样点。从6个预定义的地貌响应单元(12个站点)中收集了表面沉积物样本(顶部1厘米),以评估床沉积物物理化学(粒度分布和总有机碳含量)与微量元素含量(汞和18个其他微量元素)之间的关系。开放水域条件。在冰下对一部分站点进行了重新采样,以评估季节对这些关系和总微量元素含量的影响。大多数微量元素的浓度与晶粒度(铝和铁)的细粉含量和代理百分比密切相关,季节之间的相似微量元素晶粒度/粒度代理关系。然而,较细的物质沉积在冰下,伴随着沉积物中总有机碳含量的增加和所研究的大多数微量元素的浓度的增加。地貌响应单元方法可以有效地识别各种水文环境,以便在野外作业之前进行采样。我们的数据表明,需要进行冰下采样以确认河流系统中痕量元素-地球化学关系的全年一致性,并确定这些关系的最高极限。不论是否受到污染,就北部河流系统中的沉积物相关生物的痕量元素浓度和暴露而言,冰床沉积物可能代表最坏的情况。 Environ Toxicol Chem 2017; 36:2916-2924。 (c)2017年SETAC

著录项

  • 来源
    《Environmental toxicology and chemistry 》 |2017年第11期| 2916-2924| 共9页
  • 作者单位

    Univ Saskatchewan, Toxicol Ctr, Saskatoon, SK, Canada|Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada;

    Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada;

    Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada|Univ Saskatchewan, Sch Environm & Sustainabil, Saskatoon, SK, Canada;

    Univ Saskatchewan, Toxicol Ctr, Saskatoon, SK, Canada|Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada|Univ Saskatchewan, Sch Environm & Sustainabil, Saskatoon, SK, Canada;

    Univ Saskatchewan, Toxicol Ctr, Saskatoon, SK, Canada|Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada|Univ Saskatchewan, Sch Environm & Sustainabil, Saskatoon, SK, Canada;

    Univ Saskatchewan, Sch Publ Hlth, Saskatoon, SK, Canada;

    Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada|Univ Saskatchewan, Sch Environm & Sustainabil, Saskatoon, SK, Canada;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Trace element; Mercury; Sediment; Ice; River;

    机译:微量元素;汞;沉积物;冰;河;

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