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温带中潮河口悬沙动力中的临界转变。

Critical transitions in suspended sediment dynamics in a temperate meso-tidal estuary.

机构信息

Ecosystem Management Research Group, University of Antwerp. Universiteitsplein 1C, 2610, Wilrijk, Belgium.

Estuarine and Delta Systems, Netherlands Institute of Sea Research (NIOZ), P.O. Box 140, 4400 AC, Yerseke, The Netherlands.

出版信息

Sci Rep. 2019 Sep 4;9(1):12745. doi: 10.1038/s41598-019-48978-5.

Abstract

There is growing consensus that human interventions can fundamentally change fine sediment transport in estuaries. Critical transitions in response to human interventions have been hypothesized based on indirect observational evidence and theoretical understanding. So far direct evidence has been lacking. Based on a 20 year data-set of surface suspended particulate matter (SPM) concentrations, we present empirical evidence of critical transitions in a temperate meso-tidal estuary. In 2008-2009 the SPM dynamics of the Scheldt estuary (Belgium/The Netherlands) changed dramatically. Not only did the total amount of sediment in suspension increase, a new maximum turbidity zone (MTZ) at typical winter discharges appeared. At intermediate and low summer discharges the longitudinal distribution of SPM now flickers between two markedly different states. Our data suggest that a range of human interventions (fairway widening and deepening, dredging and dumping activities) set the scene leading to the observed transitions. Moreover the freshwater MTZ in the Scheldt and in its major tributary exhibit an increasing sensitivity towards freshwater discharge, coinciding with water quality improvements. This suggests large scale impacts of changes in eutrophication status on estuarine sediment dynamics. This has largely been a blind spot in morphodynamic research.

摘要

越来越多的人认为,人类干预可以从根本上改变河口的细颗粒物质输运。基于间接观测证据和理论理解,人们假设了人类干预下的关键转变。但到目前为止,还缺乏直接证据。基于一个为期 20 年的表层悬浮颗粒物(SPM)浓度数据集,我们提出了一个温带中潮河口发生关键转变的经验证据。2008-2009 年,斯凯尔特河(比利时/荷兰)的 SPM 动力学发生了巨大变化。不仅悬浮泥沙总量增加,而且在典型的冬季流量下出现了一个新的最大浑浊带(MTZ)。在中等和低夏季流量下,SPM 的纵向分布现在在两个明显不同的状态之间闪烁。我们的数据表明,一系列人类干预措施(航道拓宽和加深、疏浚和倾倒活动)为观察到的转变创造了条件。此外,斯凯尔特河及其主要支流的淡水 MTZ 对淡水流量的敏感性增加,这与水质改善相吻合。这表明富营养化状况的变化对河口泥沙动力学产生了大规模的影响。这在形态动力学研究中一直是一个盲点。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4343/6726847/94edf4f7a728/41598_2019_48978_Fig1_HTML.jpg

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