Evolution mechanism of physical morphology of oxbow lake in the middle Yangtze River

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Catena Pub Date : 2024-10-02 DOI:10.1016/j.catena.2024.108432
Xi Jiang , Xiaoguang Liu , Jiasheng Wang , Feng Jiao
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Abstract

Oxbow lakes, formed through river meandering cutoffs, are recognized as key components of river ecosystems, characterized by both fluvial and lacustrine features. The focus of previous research has been placed primarily on post-disconnection changes, leaving gaps in the understanding of their long-term morphological evolution. This gap is addressed through a comparative analysis of gate-controlled and naturally connected oxbow lakes over a 30-year period. In this study, Tian’ezhou Lake (gate-controlled) and Shangchewan Lake (naturally connected), located in the middle Yangtze River, are investigated. Key morphological parameters such as curvature, shoreline development index, and shrinkage rate were measured using Google Earth Engine (GEE). The influence of hydrological and meteorological factors on lake morphology was analyzed through Redundancy Analysis (RDA). Significant morphological changes were observed from 1990 to 2000. During this period, Tian’ezhou’s curvature was found to increase by 0.003/year, while Shangchewan’s curvature decreased by 0.011/year. After the construction of the Three Gorges Dam (TGD), a reduction in the rate of morphological evolution was detected, particularly between 2000 and 2010, when Tian’ezhou’s curvature decreased by 0.071/year and Shangchewan’s increased by 0.04/year. Post-2010, no significant changes in planar morphology were recorded in either lake. It was revealed by RDA that annual precipitation from 1990 to 1999 played a dominant role in influencing the morphological evolution of both lakes. From 2000 to 2020, water level fluctuations and hydrological connectivity emerged as the primary drivers. Gate control at Tian’ezhou Lake mitigated extreme water level fluctuations, contributing to a more stable environment and a slower rate of morphological evolution compared to Shangchewan. The findings underscore the importance of balanced water management strategies, integrating both natural and engineered hydrological interventions. Practical guidance is provided for ecological restoration and river management, with an emphasis on maintaining stable habitats and ensuring ecosystem resilience in response to hydrological changes.
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长江中游牛首湖物理形态的演变机制
通过河流蜿蜒断流形成的牛首湖被认为是河流生态系统的关键组成部分,同时具有河道和湖泊特征。以往研究的重点主要放在断流后的变化上,因此对其长期形态演变的了解存在空白。本研究通过对 30 年间门控牛首湖和自然连通牛首湖的对比分析,弥补了这一空白。本研究调查了位于长江中游的天娥洲湖(闸控式)和上川湾湖(自然连通式)。使用谷歌地球引擎(GEE)测量了湖泊的主要形态参数,如弯曲度、岸线发展指数和收缩率。通过冗余分析(RDA)分析了水文和气象因素对湖泊形态的影响。从 1990 年到 2000 年,湖泊形态发生了显著变化。在此期间,天鄂州的曲率每年增加 0.003,而上川湾的曲率每年减少 0.011。三峡大坝建成后,形态演变速度有所减慢,特别是在 2000 年至 2010 年期间,天鄂州曲率下降了 0.071/年,而上车厢曲率上升了 0.04/年。2010 年之后,两个湖泊的平面形态均未发生明显变化。RDA 显示,1990-1999 年的年降水量对两湖的形态演变起主导作用。从 2000 年到 2020 年,水位波动和水文连通性成为主要驱动因素。天鄂州湖的闸门控制缓解了水位的剧烈波动,使湖泊环境更加稳定,形态演变速度也比上川湾慢。研究结果强调了综合自然和工程水文干预措施的平衡水管理策略的重要性。研究为生态恢复和河流管理提供了实用指导,重点是保持稳定的栖息地,确保生态系统对水文变化的适应能力。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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