首页|期刊导航|湖泊科学|湖泊高温事件与"退养还湖"对太湖CH4排放的双重效应解析

湖泊高温事件与"退养还湖"对太湖CH4排放的双重效应解析OA

Dual effects of lake high-temperature events and"Cessation of Aquaculture and Return to Lake"on CH4 emissions in Lake Taihu

中文摘要英文摘要

全球变暖导致湖泊高温事件频发,加之东太湖2019年实施的"退养还湖"工程,二者共同作用,加剧了湖泊甲烷(CH4)排放动态的复杂性.本研究旨在阐明湖泊高温事件与生态恢复对太湖CH4排放的影响及其关联机制.基于太湖涡度通量网东太湖站点2018-2020年的高频观测数据,采用季节性阈值法识别高温事件,系统分析了高温对CH4通量的影响及"退养还湖"工程的调节效应.结果表明,季节性阈值法能精准捕捉驱动CH4排放的短期高温过程,适配季节性水温波动与CH4排放高频时变特征,2018-2020年共识别出高温事件23次.高温事件对CH4排放的促进效应存在季节差异,春、秋季强于夏、冬季.单次事件中,CH4通量多呈现3阶段变化:前期平稳、中期激增、后期回落."退养还湖"工程有效抑制了高温期的CH4排放.生态恢复期间,高温事件前、中、后期CH4通量(中位数分别为0.05~0.17、0.07~0.25、0.04~0.15 μg/(m2·s)较水产养殖期(0.42~4.89、1.05~5.26、0.71~4.60 μg/(m2·s))降低约 72%~95%.本研究可为理解浅水湖泊碳循环对气候变暖与生态管理的响应机制提供理论支撑.

Under global warming,the increasing frequency of high-temperature events in lakes,combined with the ecological resto-ration project"Cessation of Aquaculture and Return to Lake"implemented in east Lake Taihu since 2019,has created complex in-teractions that complicate the dynamics of lacustrine methane(CH4)emissions.This study aims to elucidate the impacts of these high-temperature events and ecological restoration on CH4 emissions in Lake Taihu and their underlying mechanisms.Using high-frequency observational data from the Dongtaihu site of the Taihu Eddy Flux Network(2018-2020),we employed the seasonal threshold method to identify high-temperature events and systematically analyzed their effects on CH4 fluxes alongside the regulatory influence of the restoration project.Results show that the seasonal threshold method effectively captured short-term high-tempera-ture processes that drive CH4 emissions,accommodating both seasonal water-temperature fluctuations and high-frequency temporal variations in emissions.From 2018 to 2020,23 high-temperature events were identified.Their promotive effect on CH4 emissions exhibited distinct seasonal differences,being stronger in spring and autumn than in summer and winter.During individual events,CH4 fluxes typically followed a three-phase pattern:stable in the pre-heatwave period,a sharp increase during the heatwave,and a decline in the post-heatwave period.The"Cessation of Aquaculture and Return to Lake"project effectively suppressed CH4 emis-sions during high-temperature periods.In the ecological restoration phase,the median CH4 fluxes before,during,and after high-temperature events were 0.05-0.17,0.07-0.25,and 0.04-0.15 μg/(m2·s),respectively,representing reductions of approxi-mately 72%-95%compared to the prior aquaculture phase(0.42-4.89,1.05-5.26,and 0.71-4.60 μg/(m2·s),respective-ly).This study provides a theoretical basis for understanding the response mechanisms of carbon cycling in shallow lakes to climate wanming and ecological management.

姜月影;张弥;蒲旖旎;贾磊;葛培;杨剑;乔珩;祝子涵;肖薇

南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气象灾害预报与评估协同创新中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044南京信息工程大学,气候系统预测与变化应对全国重点实验室大气环境中心,南京 210044||南京信息工程大学,气象灾害预报与评估协同创新中心,南京 210044

太湖CH4通量动态阈值时空变化特征退养还湖

Lake TaihuCH4 fluxdynamic thresholdspatiotemporal variation characteristicsCessation of Aquaculture and Re-turn to Lake

《湖泊科学》 2026 (5)

1920-1930,11

国家自然科学基金项目(41975142,42021004,U24A20590)、江苏省"333人才"领军型人才团队项目(BRA2022023)和中国气象局生态系统碳源汇重点开放实验室项目(ECSS-CMA202302,ECSS-CMA202404)联合资助.

10.18307/2026.0521

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