首页|期刊导航|水生态学杂志|生态调水驱动下富营养化湖泊溶解氧与叶绿素a动态耦合响应研究

生态调水驱动下富营养化湖泊溶解氧与叶绿素a动态耦合响应研究OA

Dynamic Coupling Response of Dissolved Oxygen and Chlorophyll-a in Eutrophic Lakes Driven by Ecological Water Diversion

中文摘要英文摘要

明确生态调水对富营养化湖泊叶绿素a与溶解氧动态耦合关系的调控机制,为优化湖泊调水方案、提升生态修复长效性提供量化依据与科学支撑.以富营养化湖泊太湖为研究对象,聚焦"引江济太"生态调水工程,于调水区贡湖湾与参考区湖心区域各设置2个采样点位,基于2011年(高强度调水)、2014年(中强度调水)、2016年(低强度调水)的监测数据,系统分析不同调水强度下叶绿素a、溶解氧及关键环境因子的时空变化特征,解析二者的耦合响应规律及驱动机制.研究结果表明,生态调水实施后水体叶绿素a浓度和蓝藻水华风险显著(P<0.01)降低,调水区(贡湖湾)叶绿素a浓度从24.35 μg/L降至12.51 μg/L.同时,生态调水改变调水区藻类生长环境,重塑了藻类生长的限制性因子,致使总磷可能不再是调水区叶绿素a浓度的主要影响因子.生态调水期间尽管溶解氧浓度呈现增加趋势,但溶解氧饱和度呈现下降趋势,从96%下降至85%,表明调水可能通过抑制藻类生物量削弱水体光合产氧能力,进而改变溶解氧的收支平衡.此外,生态调水不仅改变了叶绿素a与溶解氧的耦合关系,还可能通过增加外源营养盐输入间接影响溶解氧变化.

Taihu Lake was selected as a representative eutrophic lake for this investigation.Focusing on the"Diverting Yangtze River Water to Taihu"ecological water diversion project,we set two sampling points in the water diversion area(Gonghu Bay)and a reference area(lake center)to conduct monthly field investigations in 2011(high-intensity water diversion period),2014(medium-intensity water diver-sion period),and 2016(low-intensity water diversion period).Based on the monitoring data,the tempo-ral and spatial variation characteristics of chlorophyll-a(Chl-a),dissolved oxygen(DO),and key envi-ronmental factors under different water diversion intensities were systematically analyzed and the cou-pling response laws and driving mechanisms of Chl-a and DO concentrations were identified.We aimed to clarify the regulatory mechanism of ecological water diversion on the dynamic coupling relationship between Chl-a and DO in eutrophic lakes,and provide a quantitative basis and scientific support for opti-mizing lake water diversion schemes and enhancing the long-term effectiveness of ecological restora-tion.The concentration of Chl-a in the water body and the risk of cyanobacterial blooms significantly de-creased(P<0.01)after the water diversion scheme was implemented and the concentration of Chl-a in the water diversion area(Gonghu Bay)decreased from 24.35 μg/L to 12.51 μg/L.Ecological water diversion also altered the algal growth environment in the water diversion area and reshaped the restrictive environ-ment for algal growth so that total phosphorus might not be the main influencing factor for Chl-a concen-tration.During the ecological water diversion period DO increased,but DO saturation decreased from 96%to 85%,indicating that water diversion could decrease photosynthetic oxygen production by lower-ing algal biomass,thereby changing the balance of DO production and consumption.Ecological water di-version not only changed the coupling relationship between Chl-a and DO,but indirectly affected DO by increasing the input of exogenous nutrients.This study clarified the regulatory mechanism of ecological water diversion on the coupling process of lake algal biomass and DO production/consumption and pro-vides quantitative scientific support for optimizing lake water diversion schemes and enhancing the long-term effectiveness of ecological restoration.

肖启涛;袁洁

中国科学院南京地理与湖泊研究所湖泊与流域水安全全国重点实验室,江苏 南京 211135中国科学院武汉文献情报中心,湖北 武汉 430071

资源环境

生态调水叶绿素a溶解氧富营养化耦合响应太湖

ecological water diversionchlorophyll-adissolved oxygeneutrophicationcoupled responseTaihu Lake

《水生态学杂志》 2026 (6)

105-115,11

国家重点研发计划(2025YFE0103700)国家自然科学基金(42271114)中国科学院青年创新促进会会员项目(2023329).

10.15928/j.1674-3075.202601160002

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