首页> 外文期刊>Journal of marine systems: journal of the European Association of Marine Sciences and Techniques >An analysis on half century morphological changes in the Changjiang Estuary: Spatial variability under natural processes and human intervention
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An analysis on half century morphological changes in the Changjiang Estuary: Spatial variability under natural processes and human intervention

机译:长江河口半世纪形态学变化分析:自然过程中的空间变异性和人为干预

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Examination of large scale, alluvial estuarine morphology and associated time evolution is of particular importance regarding management of channel navigability, ecosystem, etc. In this work, we analyze morphological evolution and changes of the channel-shoal system in the Changjiang Estuary, a river- and tide-controlled coastal plain estuary, based on bathymetric data between 1958 and 2016. We see that its channel-shoal pattern is featured by meandering and bifurcated channels persisting over decades. In the vertical direction, hypsometry curves show that the sand bars and shoals are continuously accreted while the deep channels are eroded, leading to narrower and deeper estuarine channels. Intensive human activities in terms of reclamation, embankment, and dredging play a profound role in controlling the decadal morphological evolution by stabilizing coastlines and narrowing channels. Even though, the present Changjiang Estuary is still a pretty wide and shallow system with channel width-to-depth ratios 1000, much larger than usual fluvial rivers and small estuaries. In-depth analysis suggests that the Changjiang Estuary as a whole exhibited an overall deposition trend over 59 years, i.e., a net deposition volume of 8.3 x 10(8) m(3). Spatially, the pan-South Branch was net eroded by 9.7 x 10(8) m(3) whereas the mouth bar zone was net deposited by 18 x 10(8) m(3), suggesting that the mouth bar zone is a major sediment sink. Over time there is no directional deposition or erosion trend in the interval though riverine sediment supply has decreased by 2/3 since the mid-1980s. We infer that the pan-South Branch is more fluvial controlled therefore its morphology responds to riverine sediment load reduction fast while the mouth bar zone is more controlled by both river and tides that its morphological response lags to riverine sediment supply changes at a time scale 10 years, which is an issue largely ignored in previous studies. We argue that the time lag eff
机译:大规模检查大规模,升离雌曲线形态和相关时间进化是关于渠道导航性,生态系统等的管理特别重要的重要性,我们分析了长江口,河流河流系统的形态演化和变化并基于1958年至2016年间的碱基数据的潮流控制的沿海普通河口。我们看到其通道浅层模式是通过几十年来持续存在的蜿蜒和分叉的渠道。在垂直方向上,低测量曲线表明砂杆和浅滩在深通道被侵蚀时连续增加,导致越来越较深的河口通道。通过稳定海岸线和狭窄渠道来控制二等形态演变,在填海,堤防和疏浚方面发挥了深刻的作用。即使,目前的长江口仍然是一个非常宽阔,浅的系统,具有通道宽度深度比率& 1000,比通常的河流河流和小型河口大得多。深入分析表明,长江口为整体展示了超过59年的总沉积趋势,即净沉积体积为8.3 x 10(8)m(3)。在空间上,泛南分支被9.7×10(8)m(3)净侵蚀,而嘴巴区被净沉积18×10(8)m(3),这表明口条带是一个主要的沉积物水槽。随着时间的推移,由于自20世纪80年代中期以来,河流沉积物供应减少了2/3,没有定向沉积或侵蚀趋势。我们推断泛南分支更加氟化,因此其形态响应河流沉积物减少,而河口条带由河流更具控制,其形态反应滞后于河流沉积物供应变化时&gt ; 10年来,这是在以前的研究中主要忽视的问题。我们争辩说,时间滞后

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