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The effects of Hurricane Irene and Tropical Storm Lee on the bed sediment geochemistry of U.S. Atlantic coastal rivers

机译:艾琳飓风和热带风暴李对美国​​大西洋沿岸河流底泥地球化学的影响

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Hurricane Irene and Tropical Storm Lee, both of which made landfall in the U.S. between late August and early September 2011, generated record or near record water discharges in 41 coastal rivers between the North Carolina/South Carolina border and the U.S./Canadian border. Despite the discharge of substantial amounts of suspended sediment from many of these rivers, as well as the probable influx of substantial amounts of eroded material from the surrounding basins, the geochemical effects on the <63-µm fractions of the bed sediments appear relatively limited [<20% of the constituents determined (256 out of 1394)]. Based on surface area measurements, this lack of change occurred despite substantial alterations in both the grain size distribution and the composition of the bed sediments. The sediment-associated constituents which display both concentration increases and decreases include: total sulfur (TS), Hg, Ag, total organic carbon (TOC), total nitrogen (TN), Zn, Se, Co, Cu, Pb, As, Cr, and total carbon (TC). As a group, these constituents tend to be associated either with urbanization/elevated population densities and/or wastewater/solid sludge. The limited number of significant sediment-associated chemical changes that were detected probably resulted from two potential processes: (1) the flushing of in-stream land-use affected sediments that were replaced by baseline material more representative of local geology and/or soils (declining concentrations), and/or (2) the inclusion of more heavily affected material as a result of urban nonpoint-source runoff and/or releases from flooded treatment facilities (increasing concentrations). Published 2013. This article is a U.S. Government work and is in the public domain in the USA.
机译:2011年8月下旬至9月初在美国登陆的艾琳飓风和热带风暴李飓风,在北卡罗来纳州/南卡罗来纳州边界与美国/加拿大边界之间的41条沿海河流中产生了创纪录的或接近创纪录的排水量。尽管从许多河流中排出了大量的悬浮沉积物,并且可能从周围的盆地大量涌入了侵蚀物质,但地球化学作用对小于63 µm的底质沉积物的影响似乎相对有限[ <确定的成分中20%(1394中的256)]。根据表面积测量,尽管晶粒尺寸分布和床沉积物的成分发生了显着变化,但仍未发生这种变化。浓度升高和降低的沉积物相关成分包括:总硫(TS),汞,银,总有机碳(TOC),总氮(TN),锌,硒,钴,铜,铅,砷,铬,以及总碳(TC)。作为一个整体,这些成分往往与城市化/人口密度增加和/或废水/固体污泥相关。被发现的数量有限的与沉积物有关的重大化学变化可能是由于两个潜在的过程造成的:(1)冲洗河内受土地利用影响的沉积物,并用基线物质代替,这些物质更能代表当地的地质和/或土壤(浓度下降),和/或(2)由于城市非点源径流和/或洪水淹没的处理设施释放的污染物(浓度增加)而包括了受影响更严重的物质。 2013年出版。本文是美国政府的工作,在美国属于公共领域。

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