首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Impacts of human activity and extreme weather events on sedimentary organic matter in the Andong salt marsh, Hangzhou Bay, China
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Impacts of human activity and extreme weather events on sedimentary organic matter in the Andong salt marsh, Hangzhou Bay, China

机译:人类活动和极端天气事件对杭州湾杭州盐沼沉积有机物的影响

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摘要

In this study, lignin-derived phenols, stable carbon isotopes and bulk elemental compositions were determined along the length of two sediment cores (Cl and C2) from the Andong salt marsh, which is located southwest of Hangzhou Bay, China. The purpose of this study was to determine the short-term changes and their implications along sediment profiles. The 1997 high tide had caused an increase in the terrestrial organic matter (OM) signal from 1996/1997 to 2000 in both cores, which was indicated by a high A (total lignin in mg/100 mg OC), TOC, C/N and more negative delta C-13 values. The slight increases in terrestrial OM along the length of the cores between 2003 and 2006 were most likely attributable to the construction of the Hangzhou Bay Bridge. Both events have likely caused an increase in erosion, and thus, these events have increased the input of terrestrial OM to nearby areas. The effects of the distinctively dry year of 2006 can be observed along C2 between 2006 and 2008 in the steadily declining terrestrial OM signal. The overall slight decrease in terrestrial OM and the distinct increase in TOC along the length of both cores toward the present were most likely because of the overall reduced sediment caused by the trapping of materials within reservoirs. These results show that the reduction in terrestrial OM in the Andong salt marsh for the past 30 years was due to reservoirs and the 2006 drought, but this was counterbalanced by the 1997 high tide event and construction of the Hangzhou Bay Bridge, which resulted in increased erosion and terrestrial OM input.
机译:在该研究中,沿着来自Andong Salt Marsh的两个沉积物核(Cl和C2)的长度测定了木质素衍生的酚,稳定的碳同位素和散装元素组合物,该矿物沼泽地位于中国杭州湾西南部。本研究的目的是确定短期变化及其沿沉积物概况的影响。 1997年高潮引起了两种核心的1996/1997至2000年陆地有机物(OM)信号的增加,该核心由高A(Mg / 100mg OC),TOC,C / N表示更长的ΔC-13值。沿着2003年至2006年核心长度的地面Om的轻微增加最有可能归因于杭州湾桥的建设。这两个事件可能导致侵蚀增加,因此,这些事件增加了地面OM到附近地区的输入。在稳定下降的地面OM信号中,可以沿2006年至2008年在2006年至2008年之间观察到2006年独特干燥的年。陆地OM的总体略微减少和TOC在两种核心的长度朝向现在的差异差异很可能是最有可能由于储层内材料引起的整体降低的沉积物。这些结果表明,过去30年的曾经30年代的陆地OM的减少是由于水库和2006年的干旱,但这是1997年的高潮事件和杭州湾大桥建设的对抗,这导致了增加侵蚀和地面OM输入。

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