丹江口水库丰水期与枯水期CO2通量变化特征及影响因素
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武汉大学水资源工程与调度全国重点实验室

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国家自然科学基金项目(U2340207, 52394233);湖北省自然科学基金项目(2022CFA094)


Characteristics and influence factors of carbon dioxide flux in Danjiangkou Reservoir during wet and dry periods
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State Key Laboratory of Water Resources Engineering and Management, Wuhan University

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    摘要:

    水库在调节径流的同时深刻改变了河流连续体的碳通量和碳储存,在全球碳循环中扮演着重要的调控作用,其源汇大小受到自然条件、水库特征和调度管理等多方面影响。当前对不同水文条件下水库水?气界面CO2通量动态变化及其影响因素的观测与研究仍十分匮乏,严重制约了水库碳收支估算的准确性。本研究以亚热带季风区的丹江口水库为研究对象,基于2022年4月至2024年2月的涡度通量观测数据,结合结构方程模型(Structural Equation Model, SEM),定量解析丰水期与枯水期水?气界面CO2通量的差异及其影响因素。结果表明,丹江口水库全年CO2通量均值为0.12 ± 1.93 μmol/(m2.s),总体表现为弱碳源,但存在显著的季节性差异,丰水期(4?10月)CO2通量为碳源(0.97 ± 1.22 μmol/(m2.s)),而枯水期(11?3月)转为碳汇(-1.13 ± 2.04 μmol/(m2.s))。SEM路径分析表明,能量因子(显热通量为主)在丰、枯水期均为CO2通量最直接的影响因子,具有极显著负效应。在丰水期,入库流量(Qin)、出库流量(Qout)等水文因子主要通过直接作用提高CO2通量的主要直接负向驱动因子,且在枯水期作用更为显著。丰水期水文和水体物理性质通过促进营养物质积累和浮游植物繁殖,进而增强微生物呼吸作用,显著提高CO2排放,而枯水期水体相对稳定且营养负荷减弱,浮游植物等对CO2通量的作用由正转负,生物过程转而促进CO2吸收。研究结果揭示了丹江口水库不同水文时期下CO2通量源汇特征及驱动机制,为水库碳收支评估及碳调度提供科学依据。

    Abstract:

    Reservoirs, while regulating runoff, profoundly alter the carbon flux and storage along river continua, playing a critical regulatory role in the global carbon cycle. The carbon source–sink dynamics of reservoirs are influenced by various factors, including natural conditions, reservoir characteristics, and operational management. However, observations and studies on the dynamic changes in CO2 fluxes at the water–air interface of reservoirs under different hydrological conditions remain scarce, severely limiting the accuracy of carbon budget assessments. This study focused on the Danjiangkou Reservoir located in the subtropical monsoon region. Based on eddy covariance observations from April 2022 to February 2024, and employing a Structural Equation Model (SEM), the seasonal variations in CO2 fluxes at the water–air interface and their influencing factors during wet and dry periods were quantitatively analyzed. The results showed that the annual mean CO2 flux of the Danjiangkou Reservoir was 0.12 ± 1.93 μmol/(m2.s), indicating a weak carbon source overall, with pronounced seasonal variation. During the wet period (April to October), the reservoir acted as a carbon source (0.97 ± 1.22 μmol/(m2.s)), whereas during the dry period (November to March), it shifted to a carbon sink (?1.13 ± 2.04 μmol/(m2.s)). SEM analysis revealed that energy-related factors, especially sensible heat flux was the most direct and significantly negative influencing factor of CO2 fluxes in both periods, with stronger effects during the dry season. In the wet period, inflow and physical water properties significantly enhanced CO2 emissions through direct effects, while in the dry season, the influence of phytoplankton and nutrients shifted from positive to negative, indicating an increased contribution of biological processes to CO2 uptake. These findings highlights the seasonal source–sink dynamics and driving mechanisms of CO2 fluxes in the Danjiangkou Reservoir under different hydrological regimes, providing a scientific basis for reservoir carbon budget assessments and carbon-oriented management strategies.

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  • 收稿日期:2025-05-21
  • 最后修改日期:2026-04-07
  • 录用日期:2025-08-08
  • 在线发布日期: 2025-11-18
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