长江流域资源与环境 >> 2025, Vol. 34 >> Issue (09): 1998-.doi: 10.11870/cjlyzyyhj202509009

• 自然资源 • 上一篇    下一篇

长江中游典型弯曲分汊河段浮游植物时空演化特性

石浩洋1,2, 郭辉1,2*, 胡煜1,2, 杨文俊1,2, 陈端1,2   

  1. (1. 长江科学院水力学研究所, 湖北 武汉 430010; 2 长江科学院流域水资源与
    生态环境科学湖北省重点实验室, 湖北 武汉 430010)
  • 出版日期:2025-09-20 发布日期:2025-09-22

Temporal and Spatial Evolution Characteristics of Phytoplankton in Typical Reaches of the Middle Reaches of the Yangtze River

SHI Hao-yang1,2, GUO Hui1,2 , HU Yu1,2, YANG Wen-jun1,2, CHEN Duan1,2   

  1. (1. Hydraulics Department, Changjiang River Scientific Research Institute, Wuhan 430010, China;
    2. Hubei Provincial Key Laboratory of Basin Water Resource and Eco-environmental Sciences,
    Changjiang River Scientific Research Institute, Wuhan 430010, China)
  • Online:2025-09-20 Published:2025-09-22

摘要: 为探究典型弯曲分汊河段浮游植物时空演化特性,于2020年9月(丰水期)、12月(枯水期)至2021年5月(平水期)在长江中游关洲河段开展3次原位观测,设置顺直、微弯、分汊3种类型共6个观测断面,开展环境因子、营养盐和浮游植物调查分析。结果表明:研究区域共采集到浮游植物6门47属86种,其中硅藻门和蓝藻门为优势种群。时间上,丰水期至次年平水期浮游植物种类逐步增加,但藻类密度明显下降,浮游植物种类及密度受水文时期影响显著。空间上,弯曲分汊河段浮游植物种类最多且丰度占整个关洲区域的34.04%,关洲洲头、洲中及洲尾(过渡河段、弯曲分汊河段)相对丰度高于顺直断面。关洲河段受上游来水影响,左汊和右汊水动力随来流条件变化显著,进而引起环境因子和营养盐结构差异,驱动浮游植物群落局部空间分布变化。水体pH、水温、电导率和氮、磷元素是影响关洲弯曲分汊段浮游植物的主要驱动因子,其中水体环境因子对浮游植物的影响更显著。

Abstract: In order to explore the temporal and spatial evolution characteristics of phytoplankton in a typical curved braided river, three in-situ observations were carried out in Guanzhou reach of the middle reaches of the Yangtze River from September 2020 (wet season), December 2020 (dry season) to May 2021 (normal season). Six observation sections of three types of straight, slightly curved and branched were set up to investigate and analyze environmental factors, nutrients and phytoplankton. The results showed that a total of 86 species of phytoplankton belonging to 47 genera and 6 phyla were collected in the study area, of which Bacillariophyta and Cyanophyta were the dominant species. In terms of temporal changes, the species of phytoplankton increased gradually from the wet season to the normal season of the next year, but the density of algae decreased significantly. The species and density of phytoplankton were significantly affected by the hydrological periods. In terms of spatial distribution, the curved braided river had the largest number of phytoplankton species and its abundance accounted for 34.04 % of the whole Guanzhou area. The relative abundance of phytoplankton in the head, middle and tail of Guanzhou (transitional river and curved braided river) was higher than that in the straight section. The Guanzhou section was affected by the upstream water, and the hydrodynamic forces of the left and right branches changed significantly with the incoming flow conditions, which in turn caused differences in environmental factors and nutrient structure, and drove the local spatial distribution of phytoplankton communities. The pH, water temperature,conductivity, nitrogen and phosphorus in the water were the main driving factors of the phytoplankton in the curved bifurcation section of Guanzhou. The influence of water environmental factors on phytoplankton was more significant.

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