华南典型大型水库氮磷化学计量时空特征及影响因子分析——以高州水库为例
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1:暨南大学生态学系,广州 510632 ,2:广东省水库蓝藻水华防治中心,广州 510632 ,3:广东省高州水库管理中心,茂名 525242

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广东省自然科学基金项目(2024A1515012604)和国家自然科学基金项目(31901144)联合资助


Spatio-temporal pattern of nitrogen and phosphorus stoichiometry in a typical large reservoir in South China: A case study of Gaozhou Reservoir
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1:Department of Ecology, Jinan University, Guangzhou 510632 , P.R.China,2: Guangdong Provincial Center for Prevention and Control of Cyanobacterial Blooms in Reservoirs, Guangzhou 510632 , P.R.China,3: Gaozhou Reservoir Management Center, Guangdong Province, Maoming 525242 , P.R.China

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    摘要:

    氮磷化学计量是淡水生态学研究的重要内容,水体中氮磷供应水平和比例对湖库生态系统结构和功能有重要影响。为深入了解华南地区大型水库水体氮磷化学计量特征,本研究以典型大型水库(高州水库)为对象,于2023年1—12月期间开展野外调查,运用多元统计分析影响氮磷化学计量时空动态的因子。结果表明,水库湖泊区总氮(TN)和总磷(TP)浓度均值分别为(0.54±0.13)和(0.026±0.011) mg/L,指示水库处于中富营养水平;TN〖DK〗∶TP质量比在5~59间波动,均值为24±11,指示磷是初级生产力的主要限制因子,在部分时期为氮限制水体。溶解性无机氮(DIN)浓度在0.14~0.60 mg/L之间,溶解性活性磷(SRP)浓度长期小于0.01 mg/L,指示磷是浮游植物生长的主要限制性因子。湖泊区底层SRP浓度均值为(0.006±0.003) mg/L且与上层水体没有显著差异,同时底层DIN全年稳定维持在0.6 mg/L左右,指示内源释放弱,湖泊区氮磷主要受外源输入影响。颗粒态氮磷是外源输入的主要形态,水温、水体稳定性和浮游植物是影响外源性氮磷输送至湖泊区的主要因子。稳定的水体环境减弱了河流区氮磷对湖泊区的影响,是湖泊区氮磷化学计量相对稳定的重要原因。研究表明,外源营养盐输入是调节高州水库氮磷化学计量和富营养化进程的关键过程。

    Abstract:

    Stoichiometry of nitrogen and phosphorus is important for the study of freshwater ecology, as the level and ratio of nitrogen and phosphorus greatly influence ecosystem structure and function. To understand the feature of nitrogen and phosphorus stoichiometry in large reservoirs in South China, this study carried out a sampling program from January to December 2023 in a typical large reservoir (Gaozhou Reservoir). Multivariate statistics was used to analyze the factors influencing their spatio-temporal dynamics. The results showed that the average concentrations of total nitrogen (TN) and total phosphorus (TP) were (0.54±0.13) mg/L and (0.026±0.011) mg/L respectively, indicating the meso-eutrophic status of Gaozhou Reservoir. And the mass ratio of TN∶TP ranged in 5-59 (24±11), suggesting mostly P limitation and sometimes N limitation on primary production. The dissolved inorganic nitrogen (DIN) was higher than 0.13 mg/L, and the dissolved inorganic phosphorus (SRP) was lower than 0.01 mg/L, indicating mainly P-limiting for phytoplankton growth in the reservoir. Low SRP concentration (0.006±0.003) mg/L and stable DIN concentration ( about 0.6 mg/L) in bottom water indicated limited internal release, and external input was the main nutrient source for the reservoir. Particulate form was the main component of TP and TN. Thus, water temperature, water stability and phytoplankton were the main factors affecting the spatial and temporal distribution of nitrogen and phosphorus. High water stability reduced the influence of riverine nutrients on lucastrine zone, and resulted in more stable nitrogen and phosphorus stoichiometry. The results suggested that the external nutrients were the most important process regulating nitrogen and phosphorus stoichiometry and eutrophication in the large reservoir.

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毛仲蒙,蒋燕茹,刘瑞敏,陈凌,顾继光,肖利娟.华南典型大型水库氮磷化学计量时空特征及影响因子分析——以高州水库为例.湖泊科学,2025,37(4):1189-1197. DOI:10.18307/2025.0411

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  • 收稿日期:2024-07-25
  • 最后修改日期:2024-12-06
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  • 在线发布日期: 2025-07-04
  • 出版日期: 2025-07-06
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