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河流交汇区水力学特性与水安全研究进展
Research Progress on Flow Characteristics and Water Safety at River Confluences
河流交汇区是河网系统中水、沙、污染物、生物等环境要素的突变点,也是河网行洪与污染物输移扩散的关键控制节点。从野外测量、室内试验与数值模拟方面,总结分析了河流交汇区水流结构与污染物输移的基本特征及其在不同交汇条件作用下的响应规律,以及复杂水流结构与生境对于河流交汇区水安全的重要影响。展望了未来研究重点,建议加强非恒定流条件下的交汇区水力学特性研究,进一步揭示交汇区污染物掺混输移特征与水动力条件之间的响应机制,研究通过工程布局与水力优化调控相结合的措施系统提升了交汇区防洪安全与水生态环境质量。
River confluences are areas where environmental elements such as flow structures, sediment deposition, water quality, and organisms undergo significant changes in river networks, and are the key nodes for flooding and pollutant transport. This review summarizes the basic characteristics of flow structures and pollutant transport at river confluences and their responses to different conditions, along with the important impacts of complex flow structures and habitats on water safety issues in previous field measurements, laboratory experiments, numerical simulations, and theoretical studies. Future research should focus on enhancing the understanding of the hydraulic characteristics of river confluences under unsteady flow conditions, further clarifying the response mechanisms between pollutant transport and hydraulic parameters, and improving the flood safety and the water ecological environmental quality through the combination of engineering layout and hydraulic optimization and regulation.
river confluences / flow structures / pollutant transport / water safety
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平原河网地区河流结构发育受到自然条件和城市化的双重影响。依据遥感解译数据,围绕城市化水平、河流形态、河流结构和河流调蓄功能四个维度,就建成区面积比例、河流长宽分布、河系分维、河流调蓄能力等具体指标,分析了城市化水平和土地利用特征不同区域的河流空间形态、结构特征和功能状态,探讨了城市化进程中平原河网地区河流结构的可能演化轨迹,尝试建立了城市化影响下平原河网地区河流结构分类方法,提出了城市河流综合整治过程中应充分重视保护自然河流结构,注重发挥河流综合功能等观点。
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Stream structure development in river network regions was both affected by physical conditions and rapid urbanization.Based on remote-sensing data,four measuring dimensions including the degree of urbanization,river patterns,stream structure and river functions were brought forward to be used as tools for stream structure classification.Twelve indicators such as the percentage of urbanized area,river length and width distribution,river fractal dimension,river flood storage and control capacities were designed for explaining the four measuring dimensions and describing the characteristics of stream structure type.The characteristics of three kinds of stream structure that were defined as the mainstream type,and the "#" type and the natural type were discussed based on the classification system developed in the paper.The results showed that the mainstream type was formed mainly because of high level of urbanization and branches were engineered out for the sake of urban construction and expanded.The natural type was maintained mostly in the area with lower lever of urbanization,which always reflects the local physical features.The "#" type stream structure was a sort of result caused by intermediate level of urbanization under spatial distribution of mainstreams in a catchment.Generally,following the urbanization process,stream structure might be changed from the natural type to the "#" type and at last,to become the mainstream type.The paper further discussed the qualitative and quantitative criteria that could used to guide differentiating structure status in river network regions.The authors thought it was valuable and important to maintain natural stream structure and plan and restore multi-functions of rivers in the process of urbanization.
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River confluences are key features of a river network, and their effects on contaminant transport and transformation need to be understood to control the contamination of a river network. This paper investigates the dynamic characteristics of phosphorus (P) contamination on the surface sediment at a river confluence of the Huai River, China, where water and sediment contamination is severe. The results highlight that P contamination of the surface sediment at a river confluence is more severe than that of the main stream of the river network to which the river confluence belongs. Floods have critical impact on the transport of sediment and its surface texture. In the annual water cycle the initial small flood can convey much more contaminated sediment and pollute the downstream river, whereas the subsequent large flood leads to the coarsening of the surface sediment and decrease of the total P (TP) content on the surface sediment (TPS). Water temperature is one of the most important factors affecting the temporal variability of the TPS at the river confluence. Higher P amounts are adsorbed on the surface sediment during lower water temperatures in winter and spring. Calcium bound P (Ca-P) is a relatively stable fraction of the sedimentary P during the dynamic processes of contamination of the surface sediment, and the nonapatite P gets released from the surface sediment during the summer. Effects of P concentration of the surface water and that of pH on TPS variability are not discernable in the current study. These results will be useful for controlling phosphorus contamination at river confluences and in river networks.
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