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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Anthropogenic inventories and historical and present accumulation rates of copper in Great Lakes sediments
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Anthropogenic inventories and historical and present accumulation rates of copper in Great Lakes sediments

机译:大湖沉积物中人为资源清单以及铜的历史和当前积累率

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Sediment cores were collected from depositional basins in lakes Michigan, Ontario and Superior to assess spatial and temporal variations in Cu accumulation rates and inventories. Sediment chronologies were determined via Pb-210 dating. and Pb-210 inventories were used to correct for the effects of sediment focusing. Among the lakes studied, Cu loading histories generally decrease to the present, signifying a regional reduction in the anthropogenic release of Cu to the environment. Focusing-corrected Cu accumulation rates in surficial sediments vary significantly within lakes Michigan and Ontario, suggesting that recent inputs of Cu to these 2 lakes may have been dominated by localized sources. Variations in Cu accumulation rates within Lake Superior are interpreted to be insignificant, suggesting either that Lake Superior is well-mixed with respect to copper inputs or that the lake is dominated by a single source for Cu. Recent measurements of atmospheric fluxes of Cu within the Great Lakes region generally indicate that the atmosphere accounts for less than 50% of the Cu accumulating in surficial sediments. Historical Cu accumulation rates from Lake Superior are poorly correlated with Cu production associated with local smelters, but agree favorably with national production rates. Trends in historical Cu accumulation rates within all 3 lakes may indicate that recent declines in Cu loading can be attributed to the enactment of stricter environmental regulations as well as changes in the use of Cu. Focusing-corrected Cu inventories in lakes Michigan, Ontario, and Superior are generally invariant within a given lake, indicating that, historically, these lakes have been dominated either by a single source or were well-mixed with respect to Cu inputs. The disparity between the results from recent accumulation rates and historical inventories may reflect differences in how the Great Lakes respond to contaminant loading on short (e.g. years) versus long (e.g. decades) timescales. (C) 1998 Elsevier Science Ltd. All rights reserved. [References: 85]
机译:从密歇根湖,安大略湖和苏必利尔湖的沉积盆地收集沉积岩心,以评估铜积累速率和存量的时空变化。沉积物年代通过Pb-210测年确定。和Pb-210清单用于纠正沉积物聚焦的影响。在所研究的湖泊中,到目前为止,铜的负载历史总体上有所减少,这表明人为释放到环境中的铜的区域性减少。在密歇根州和安大略湖中,经聚焦校正的表层沉积物中铜的累积速率差异很大,这表明最近对这两个湖的铜输入可能已被局部来源所控制。苏必利尔湖中铜积累速率的变化被认为是微不足道的,这表明苏必利尔湖在铜输入方面混合得很好,或者该湖由单一的铜来源所主导。最近对大湖区铜的大气通量的测量结果通常表明,大气中表层沉积物中铜的累积量不到50%。苏必利尔湖的历史铜积累率与当地冶炼厂的铜产量相关性很低,但与全国的生产率有很好的一致性。所有三个湖泊中的历史铜累积速率的趋势可能表明,最近铜负荷的下降可归因于更严格的环境法规的制定以及铜的使用变化。集中校正的密歇根州,安大略省和苏必利尔湖中的铜库存在给定的湖中通常是不变的,这表明,从历史上看,这些湖要么由单一来源控制,要么就铜投入而言是充分混合的。最近积累率和历史清单的结果之间的差异可能反映了大湖区在短(例如几年)和长(例如几十)时间尺度上对污染物负荷的反应方式上的差异。 (C)1998 Elsevier ScienceLtd。保留所有权利。 [参考:85]

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