raybet体育在线 院报 ›› 2025, Vol. 42 ›› Issue (5): 18-25.DOI: 10.11988/ckyyb.20240200

• 河湖保护与治理 • 上一篇    下一篇

河流近底河床粗细泥沙交换研究进展

金中武(), 李汕, 卢金友(), 郭小虎   

  1. raybet体育在线 水利部长江中下游河湖治理与防洪重点实验室,武汉 430010
  • 收稿日期:2024-03-04 修回日期:2024-08-09 出版日期:2025-05-01 发布日期:2025-05-01
  • 通信作者:
    卢金友(1963-),男,浙江仙居人,正高级工程师,博士,博士生导师,从事河流泥沙运动基本规律研究。E-mail:
  • 作者简介:

    金中武(1976-),男,湖北崇阳人,正高级工程师,博士,硕士生导师,主要从事泥沙运动方面的研究。E-mail:

  • 基金资助:
    国家重点研发计划项目(2023YFC3209500); 国家自然科学基金长江水科学研究联合基金项目(U2240206); 国家自然科学基金长江水科学研究联合基金项目(U2240224)

Research Progress on Coarse and Fine Sediment Exchange Near Riverbed

JIN Zhong-wu(), LI Shan, LU Jin-you(), GUO Xiao-hu   

  1. Key Laboratory of Ministry of Water Resources on River-Lake Regulation and Flood Control in the Middle and Lower Reaches of Yangtze River, Changjiang River Scientific Research Institute,Wuhan 430010, China
  • Received:2024-03-04 Revised:2024-08-09 Published:2025-05-01 Online:2025-05-01

摘要:

河流泥沙交换运动是河流泥沙运动力学中主要难题之一,泥沙交换运动的过程与强度决定了河床冲淤的速率,从而引起河床冲淤演变。归纳总结了河床泥沙上扬通量推演过程及影响因素、河床泥沙粗细交换中泥沙扩散方程以及泥沙交换层厚度方程的形成过程、泥沙交换数学模型的建立、泥沙交换试验研究的方法等最新研究进展,同时梳理该方向研究存在的关键问题和未来趋势。目前尚未统一化的理论公式,计算方法均以经验公式为主,且缺乏可靠实测资料的充分验证。研究有助于深入了解河流近底泥沙交换研究的最新进展,为未来深入研究泥沙交换的重点方向提供参考。

关键词: 泥沙交换, 悬移质泥沙, 河床冲淤, 数学模型, 研究进展

Abstract:

Sediment exchange is one of the key issues in the evolution of riverbed erosion and deposition, and its study holds significant importance for river management and engineering practices. This study systematically reviews domestic and international research progress over the past three decades, focusing on the mechanisms of coarse and fine sediment exchange near the riverbed from four aspects: theoretical models, mathematical models, experimental methods, and field data analysis. The results demonstrate that existing theoretical models (e.g., upward flux formulas based on turbulent bursting, energy balance, and diffusion theories) largely depend on empirical assumptions, lack universally applicable mechanism descriptions, and face limitations due to insufficient field data validation. Although mathematical models describing three-state transitions among suspended load, bedload, and bed material have gradually incorporated probabilistic methods such as Markov chains, they still face challenges in accurately representing sediment exchange process under non-uniform flow conditions. Experimental studies reveal that medium-diameter sediments exhibit higher upward flux due to turbulent bursting and exposure effects. Moreover, formulas for exchange layer thickness dominated by sand wave migration require modifications to account for the influence of resistance transitions in sandy rivers. This study proposes three innovative future directions: (1) integrating prototype observation data to establish unified theoretical formulas for sediment exchange; (2) developing high-precision observation technologies to overcome the bottleneck in dynamically capturing random sediment collision processes; and (3) combining machine learning with physical models to build predictive systems for sediment state transitions. This review provides systematic references for advancing the understanding of sediment exchange mechanisms and optimizing engineering practices.

Key words: sediment exchange, suspended sediment, riverbed erosion and deposition, mathematical models, research progress

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