福建省山仔水库碳磷比生态计量特征研究

    Study on the ecological stoichiometric characteristics of the carbon-phosphorus ratio in Shanzai Reservoir, Fujian Province

    • 摘要:
      目的 富营养化引发的蓝藻水华已严重威胁水体健康和生态系统稳定。本研究旨在探讨溶解性无机碳和总磷比(DIC/TP)时空分布规律及其对水库浮游植物群落结构的影响,评估其作为富营养化预警指标的敏感性。
      方法  2023年4月至2024年2月,在山仔水库库心、坝前、日溪入口、皇帝洞和河道5个采样点采集水样及浮游植物样本,测定水文理化指标、DIC、溶解性有机碳(DOC)及TP浓度,通过方差分析和相关性分析(ANOVA)探究指标间的关联性。
      结果 研究期间共检出浮游植物6门51属,总密度范围为1.90×106~2.71×108 个·L−1,季节变化为春>夏>秋>冬;DIC/TP比值范围为12.0~825.4(均值为178.9),时空分布差异显著,季节变化趋势为冬>秋>夏>春,空间变化趋势为库心>坝前>日溪入口>皇帝洞>河道;DIC/TP比值与浮游植物总密度(r=−0.440)、蓝藻密度(r=−0.480)均呈显著负相关,与硅藻密度(r=0.410)呈显著正相关(P<0.001),且与综合营养状态指数及水温、透明度等环境因子显著相关(P<0.05)。
      结论 DIC/TP比值是调控浮游植物群落的关键因子,春、夏季比值低,蓝藻风险高,冬季比值高,绿藻与硅藻优势显著,其升高可推动群落由蓝藻主导转向绿藻和硅藻主导。相较于氮磷比(TN/TP),DIC/TP比值对富营养化状态响应更敏锐,可作为水库富营养化早期预警的敏感指标。本研究深化了DIC/TP比值对水库浮游植物群落结构影响的认识,为富营养化水体修复提供了新的理论视角和实践参考。

       

      Abstract:
      Objective Eutrophication-induced cyanobacterial blooms have posed a severe threat to water body health and ecosystem stability. This study aims to investigate the spatiotemporal distribution characteristics of the dissolved inorganic carbon-to-total phosphorus ratio (DIC/TP) and its effects on the phytoplankton community structure in reservoirs, as well as to evaluate the sensitivity of DIC/TP as an early-warning indicator for eutrophication.
      Methods From April 2023 to February 2024, water samples and phytoplankton samples were collected at 5 sampling sites (reservoir center, dam front , Rixi inlet, Huangdi Cave, and river channel) in Shanzai Reservoir. Hydrological and physicochemical indicators, together with concentrations of DIC, dissolved organic carbon (DOC) and TP were measured. Analysis of variance (ANOVA) and correlation analysis were performed to explore the correlations among these indicators.
      Results A total of 6 phyla and 51 genera of phytoplankton were identified during the study period. The total phytoplankton density ranged from 1.90×106 to 2.71×108 cells·L−1, exhibiting a seasonal variation pattern of spring>summer>autumn>winter. The DIC/TP ratio varied from 12.0 to 825.4, with an average value of 178.9, and showed significant spatiotemporal differences. Its seasonal variation followed the order of winter>autumn>summer>spring, while the spatial variation was in the sequence of reservoir center>dam front>Rixi inlet>Huangdi Cave>river channel. Correlation analysis revealed that the DIC/TP ratio was extremely significantly negatively correlated with total phytoplankton density (r=−0.440) and cyanobacterial density (r=−0.480), whereas extremely significantly positively correlated with diatom density (all P<0.001). Additionally, the ratio was also significantly correlated with the trophic state index and environmental factors such as water temperature (WT) and secchidisc (SD) (P<0.05).
      Conclusion The DIC/TP ratio is a key factor regulating the phytoplankton community structure. Low DIC/TP ratios in spring and summer are associated with high cyanobacterial bloom risks, while high ratios in winter favor the dominance of chlorophytes and diatoms. An increase in the DIC/TP ratio can drive the phytoplankton community to shift from cyanobacteria-dominated to chlorophyta- and bacillariophyta-dominated. Compared with the nitrogen-to-phosphorus ratio (TN/TP), the DIC/TP ratio responds more sensitively to eutrophication status, thus serving as a sensitive indicator for the early warning of reservoir eutrophication. The study deepens the understanding of the effects of the DIC/TP ratio on phytoplankton community structure in reservoirs, providing a new theoretical perspective and practical reference for the restoration of eutrophic water bodies.

       

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