中国长江口最大水龄带与营养盐的动态及相关性

IF 2.6 3区 地球科学 Q1 MARINE & FRESHWATER BIOLOGY
Yanliang Du , Xiaoyu Ma , Guiquan Xu , Xiaobo Liu , Chang Liu , Shiyan Wang , Shiqiang Lu , Zhen Han , Ailing Yan , Xu Ma
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引用次数: 0

摘要

在河流与海洋交汇的大河口,水文过程主导着营养物质和其他生物地球化学化合物的时空浓度。水龄是衡量水更新时间尺度的指标,也是水动力和污染物迁移的特征参数。建立了从长江大同水文站到东海的大规模江海联动多过程耦合二维 EFDC 模型。模拟并分析了河流流量变化对长江口水动力和营养盐的影响。长江口的污染物负荷主要来自上游流入和本地输入。来自上游的总磷(TP)负荷比例大于总氮(TN)负荷,分别约占 90% 和 78%。随着河流流量的减少,大部分地区的 TN 浓度都会下降,只有在大的污水排放口附近,TN 浓度会上升,而 TP 浓度则呈下降趋势。当河道流量从 60000 m3/s 以上下降到 10000 m3/s 的较低值时,长江口上海段南侧河道的平均 TN 浓度上升了近 13%,而 TP 浓度下降了近 5%。模型结果表明,河口内的水龄与流速成反比。相比之下,河口外的水龄与河流流量成负相关。水年龄最大区(WAMZ)位于河口内,从河口内到距河口 90 公里处,可能与浊度最大区(TMZ)的位置相吻合,浊度最大区随着长江口河水排放量的增减而向海面或陆地移动。除位置外,最大水龄值与河流流量呈负相关,这也可能与浊度强度有关。水龄和 WAMZ 可作为预测长江口水环境和营养汇变化的指标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamics and correlations of maximum water age zones and nutrients in the Changjiang Estuary, China

The hydrological process dominates the spatial and temporal concentrations of nutrients and other biogeochemical compounds in the large estuary where river and ocean meet. Water age is a measure of water renewal timescale and a characteristic parameter of hydrodynamics and contaminant transport. A large-scale river-sea linked and multi-process coupled 2D EFDC model was constructed from Datong hydrometric station of Changjiang River to the East China Sea. The effects of changes in river discharge on hydrodynamics and nutrients in the Changjiang Estuary were simulated and analyzed. Pollutant loads to the Changjiang Estuary are mainly from upstream inflows and local inputs. The proportion of total phosphorus (TP) loads from upstream is greater than the total nitrogen (TN) loads, accounting for about 90% and 78%, respectively. As the river discharge decreases, TN concentrations decrease in most regions, except for near large sewage discharges where TN concentrations increase while TP concentrations show a decreasing trend. When the river flow drops from over 60000 m3/s to a relatively low value of 10000 m3/s, the average TN concentration in the southern channel of the Shanghai section of the Changjiang Estuary increases by nearly 13%, while TP concentration decreases by nearly 5%. The model results show that the water age inside the river mouth is inversely proportional to the flow rate. In contrast, the water age outside the mouth is negatively with the river discharge. The water age maximum zones (WAMZ) are found in the estuary, ranging from within the estuary to 90 km from the mouth, and are likely to coincide with the positions of the turbidity maximum zones (TMZ), which move seawards or landwards with the increase or decrease of river discharge in the Changjiang Estuary. In addition to location, the value of water age maxima varies negatively with river discharge, which is also relevant to turbidity intensity likely. Water age and WAMZ can be the indicators to predict the changes in the water environment and nutrient sinks in the Changjiang Estuary.

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来源期刊
CiteScore
5.60
自引率
7.10%
发文量
374
审稿时长
9 months
期刊介绍: Estuarine, Coastal and Shelf Science is an international multidisciplinary journal devoted to the analysis of saline water phenomena ranging from the outer edge of the continental shelf to the upper limits of the tidal zone. The journal provides a unique forum, unifying the multidisciplinary approaches to the study of the oceanography of estuaries, coastal zones, and continental shelf seas. It features original research papers, review papers and short communications treating such disciplines as zoology, botany, geology, sedimentology, physical oceanography.
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