描述黄河流域基础流 signature 的变化
Shixuan Lyu1, Chunling Guo2, Yuyu Zhai3
1College of Geography and Environment, Shandong Normal University, Jinan, 250358, China; Department of Civil Engineering, University of Bristol, Bristol, BS8 1TR, UK.
Journal of environmental management
|July 10, 2023
概括
黄河盆地 (YRB) 的基流显示出明显的空间模式,并随地形,植被和耕地而变化. 多种因素协同影响基流,对可持续的水资源管理至关重要.
科学领域:
- 水文学的水文学
- 环境科学 环境科学
- 水资源管理 水资源管理
背景情况:
- 基流对于生态健康和经济发展至关重要,特别是在黄河流域 (YRB) 等缺水地区.
- 了解基流动力学对于YRB的可持续水资源管理至关重要,YRB面临自然条件和人类活动带来的挑战.
研究的目的:
- 从2001年到2020年在黄河流域 (YRB) 量化调查基流特征及其决定因素.
- 用多个算法分析基流特征的时空变化,并识别关键影响因素.
主要方法:
- 采用了四种基流分离算法:英国水文研究所 (UKIH),莱恩-霍利克,查普曼-马克斯韦尔和埃克哈特方法.
- 从每日集合平均基流数据中提取了13个基流动力学特征.
- 与取水区特征相关的基流特征,如地形,植被和土地覆盖.
主要成果:
- 在基流签名中确定了显著的空间模式,在上游和下游达到时具有更高的值.
- 在基流特征和流域地形,植被生长和耕地覆盖面的时间变化之间发现了强烈的相关性.
- 证明了土壤质地,降水和植被对基流特征值的协同效应.
结论:
- 在YRB中,基流特征表现出复杂的空间和时间变化,受多种环境和人为因素的影响.
- 这些发现为优化黄河流域和类似河流系统的水资源管理策略提供了宝贵的见解.
相关概念视频
Rapidly Varying Flow
98
Rapidly varying flow (RVF) in open channels is characterized by abrupt changes in flow depth over a short distance, with the rate of depth change relative to distance often approaching unity. These flows are inherently complex due to their transient and multi-dimensional nature, making exact analysis difficult. However, approximate solutions using simplified models provide valuable insights into their behavior.Key Features of Rapidly Varying FlowRVF is commonly observed in scenarios involving...
98
Underflow Gates
79
Underflow gates are vital for controlling water flow in irrigation canals. The three main types of underflow gates — vertical, radial, and drum gates — serve different purposes while ensuring effective flow management. Vertical gates move up and down, generating a free-flowing water jet; radial gates pivot to regulate the flow; and drum gates rotate for precise adjustments. The flow through these gates is influenced by downstream conditions, resulting in free or drowned outflow.Free and...
79
Gradually Varying Flow
88
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
88
Typical Model Studies
385
Fluid mechanics model studies often utilize scaled-down systems to predict fluid behavior in full-scale environments, such as river flows, dam spillways, and structures interacting with open surfaces. Maintaining Froude number similarity in river models is crucial, as it replicates surface flow features like wave patterns and velocities.
385
Design Example: Analyzing Capacity Contours for Flood Risk Assessment
72
Flood risk assessment involves careful planning and analysis to ensure the safety of communities near water retention structures. Capacity contours are a vital tool in this process, as they illustrate the potential spread of water at specific levels in a given area. In the context of building a bund across a small valley, these contours play a critical role in evaluating the safety of nearby residential areas.In this example, the bund is intended to store stormwater in the valley. The engineers...
72
Uniform Depth Channel Flow
98
Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...
98


