枯水季"引江济太"工程对受水河湖水体磷素分布的影响OA
Impact of dry-season water diversion from the Yangtze River to Lake Taihu on phosphor-us distribution in water-receiving areas
本研究以改善太湖水环境的"引江济太"调水工程为背景,重点关注该工程对太湖磷素(特别是生物有效磷)的输入贡献,及其与藻华风险的潜在关联.选取望虞河引水通道及受水区贡湖湾为重点研究区域,并以太湖湖心区作为对照,于2018-2022年枯水季(秋、冬季)开展野外调查,监测总磷(TP)、溶解性总磷(DTP)、溶解性反应磷(SRP)、叶绿素a(Chl.a)等环境因子,推算出颗粒态磷(PP)和溶解性有机磷(DOP),进而通过统计分析评估引水对磷素分布的影响及其与藻类生长的关系.结果表明:秋季引水期间,望虞河自长江至入湖口磷素呈沿程递减趋势,冬季则呈波动上升趋势;从贡湖湾向湖心区方向,TP、DTP、SRP和DOP在引水期与非引水期均表现为波动上升态势.引水期贡湖湾PP占比在秋季和冬季分别为43.16%和37.33%,高于非引水期(31.50%和20.17%),但望虞河入湖磷素浓度总体与湖心区相当甚至更低,表明枯水季引水未显著增加贡湖湾磷素负荷,尤其对溶解态生物有效磷影响有限.相关性分析结果表明,秋季引水期贡湖湾Chl.a与水温、浊度显著相关,冬季则与溶解氧、pH显著相关,未发现Chl.a与各形态磷具有显著相关性.综上所述,在望虞河西控工程调控下,枯水季"引江济太"引水不会显著增加受水湖区磷素负荷,尤其对浮游藻类直接利用的生物有效磷输入有限,贡湖湾藻类生长对磷素响应不敏感.尽管如此,引水输入磷的长期累积效应及其对藻华暴发的潜在影响仍需持续关注与深入研究.
The Water Diversion from Yangtze River to Lake Taihu(WDYT)is a major engineered water transfer project designed to improve the water quality of Lake Taihu.However,its impact on lake phosphorus dynamics,especially the contribution of bioavail-able phosphorus and its linkage to algal bloom risk,remains inadequately understood.This study aimed to evaluate the degree and contribution of the WDYT to phosphorus variations in Lake Taihu and to examine its association with algal bloom potential.Focu-sing on the Wangyu River diversion channel and the receiving Gonghu Bay,with the central lake zone as a reference area,field sampling was conducted during dry seasons(autumn and winter)from 2018 to 2022.Parameters monitored included total phos-phorus(TP),total dissolved phosphorus(DTP),soluble reactive phosphorus(SRP),chlorophyll-a(Chl.a),and other physico-chemical factors;particulate phosphorus(PP)and dissolved organic phosphorus(DOP)were derived.Statistical analyses were employed to assess the influence of water diversion on aquatic phosphorus forms and its correlation with algal indicators.Results in-dicated that phosphorus concentrations in the Wangyu River decreased along the flow path from the Yangtze River to the lake inlet during autumn diversion periods,whereas they fluctuated and increased overall in winter.From Gonghu Bay toward the central lake,concentrations of TP,DTP,SRP,and DOP showed fluctuating yet generally increasing trends during both diversion and non-diversion periods in autumn and winter.The average proportion of PP in Gonghu Bay during diversion periods was 43.16%in autumn and 37.33%in winter,higher than during non-diversion periods(37.33%and 20.16%,respectively).Nevertheless,phosphorus concentrations in the Wangyu River inflow were generally similar to or lower than those in the central lake zone.Dry-season diversion did not significantly increase phosphorus levels in Gonghu Bay,particularly dissolved bioavailable phosphorus.Chl.a in Gonghu Bay correlated with water temperature and turbidity in autumn,whereas it was significantly associated with DO and pH in winter.No significant correlation was found between Chl.a and phosphorus concentrations.Under the operation of the Wangyu River western control project,dry-season diversion does not substantially raise the phosphorus load in the receiving lake ar-ea,especially regarding dissolved bioavailable phosphorus directly available to phytoplankton.Thus,phytoplankton growth in Gon-ghu Bay during the dry season is not sensitive to phosphorus concentrations.Although the phosphorus introduced via diversion shows limited short-term ecological effects,its long-term accumulation and potential role in promoting algal blooms in Lake Taihu require further investigation.
李馨雅;吴修锋;戴江玉;吴时强;刘倩倩;程旭;钟优
南京水利科学研究院,南京 210029南京水利科学研究院,南京 210029||水灾害防御全国重点实验室,南京 210029南京水利科学研究院,南京 210029||水灾害防御全国重点实验室,南京 210029||水利部太湖流域浅水湖泊生态系统野外科学观测研究站,无锡 214024南京水利科学研究院,南京 210029||水灾害防御全国重点实验室,南京 210029南京水利科学研究院,南京 210029南京水利科学研究院,南京 210029南京水利科学研究院,南京 210029
"引江济太"枯水季望虞河贡湖湾磷素
Water Diversion from Yangtze River to Lake Taihu(WDYT)dry seasonWangyu RiverGonghu Bayphosphorus
《湖泊科学》 2026 (3)
994-1005,12
国家自然科学基金项目(52179073)、水利部重大科技项目(SKS-2022059)和南京水利科学研究院基金项目(Y124001,Y124020)联合资助.
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