付涛, 牛丽霞, 党浩铭, 杨清书. 珠江河口氮、磷营养盐的季节分布特征及影响因子研究[J]. 海洋环境科学, 2023, 42(1): 122-130. DOI: 10.12111/j.mes.2022-x-0125
引用本文: 付涛, 牛丽霞, 党浩铭, 杨清书. 珠江河口氮、磷营养盐的季节分布特征及影响因子研究[J]. 海洋环境科学, 2023, 42(1): 122-130. DOI: 10.12111/j.mes.2022-x-0125
FU Tao, NIU Li-xia, DANG Hao-ming, YANG Qing-shu. Effects of seasonal variation of the river discharge input on nitrogen and phosphorus nutrients in Pearl River Estuary[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2023, 42(1): 122-130. DOI: 10.12111/j.mes.2022-x-0125
Citation: FU Tao, NIU Li-xia, DANG Hao-ming, YANG Qing-shu. Effects of seasonal variation of the river discharge input on nitrogen and phosphorus nutrients in Pearl River Estuary[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2023, 42(1): 122-130. DOI: 10.12111/j.mes.2022-x-0125

珠江河口氮、磷营养盐的季节分布特征及影响因子研究

Effects of seasonal variation of the river discharge input on nitrogen and phosphorus nutrients in Pearl River Estuary

  • 摘要: 本文围绕珠江河口氮、磷营养盐的季节分布规律,采用皮尔逊相关分析、“营养盐-盐度”双端元模型探讨氮、磷营养盐的主要影响因子和潜在来源,并对珠江口海域水体进行富营养化评估。结果表明,珠江河口氮、磷营养盐浓度整体较高(均值分别为0.72 mg/L和0.021 mg/L),呈河口湾顶到外海递减的趋势;氮、磷季节变化差异显著,夏季高于其他季节;外海水团对氮的稀释、混合作用高于磷。“营养盐-盐度”双端元模型结果显示,在夏季和秋季,无机氮浓度减小的原因主要是海洋生物的吸收作用(叶绿素a浓度 >10 µg/L);而在秋季和冬季,其浓度减小的原因主要是河口水体混合和径流量小导致无机氮的输入减少。活性磷酸盐主要来自附近城市的污水排放,其浓度减小的原因主要是浮游植物吸收和泥沙吸附。研究海域浮游植物的生长主要受磷限制,水环境呈中度富营养化,因此,夏季爆发富营养化的概率很大。

     

    Abstract: Focusing on the seasonal distribution of nitrogen and phosphorus nutrients in the Pearl River Estuary, this paper uses Pearson’s correlation analysis and “nutrient-salinity” double-end member model to discuss the main influencing factors and potential sources of nitrogen and phosphorus nutrients. The water body was assessed for eutrophication. The results showed that the nutrient concentrations of nitrogen and phosphorus in the Pearl River Estuary were relatively high (mean values were 0.72 mg/L and 0.021 mg/L, respectively), showing a decreasing trend from the top of the estuary to the open sea. In other seasons; the dilution and mixing effect of open water mass on nitrogen nutrients is higher than that of phosphorus nutrients; the results of the “nutrient-salinity” double-end element model show that in summer and autumn, the decrease of inorganic nitrogen concentration is mainly due to the absorption of marine organisms (Chlorophyll a concentration>10 µg/L), while in autumn and winter, the input of inorganic nitrogen is mainly reduced due to the mixing of estuary water and small runoff; active phosphate mainly comes from sewage discharge from nearby cities, and its concentration reduction is mainly due to It is caused by phytoplankton absorption and sediment adsorption; the growth of phytoplankton in this sea area is mainly limited by phosphorus, and the overall water environment is moderately eutrophic, and there is a high probability of eutrophication disasters in summer.

     

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