东寨港河口冬季氮营养盐分布及浮游植物氮吸收速率研究

The nitrogen distribution and phytoplankton uptake rates in the wintertime at Dongzhai estuary

  • 摘要: 近年来,因人类活动导致的大量活性氮通过河口输入近海,沿海地区的富营养化和有害藻华问题日益加剧。深入研究河口系统中氮营养盐的分布以及浮游植物对不同形式氮营养盐的吸收偏好,对揭示藻华暴发机制和陆源超额氮管理具有重要意义。本研究于2022年12月在海南省东寨港河口开展了环境因子和氮营养盐浓度调查,并通过15N同位素示踪实验,定量分析了浮游植物对尿素(Urea-N)、铵氮(NH4+)、硝酸盐(NO3)和亚硝酸盐(NO2)的吸收速率。结果表明,冬季东寨港水体溶解态氮营养盐浓度沿河口向外海递减,浓度排序为NO3 > NH4+ > NO2 > Urea-N,其浓度范围分别为5.84~49.78 µmol/L、1.16~40.64 µmol/L、0.83~2.98 µmol/L、0.25~0.98 µmol/L。浮游植物氮吸收速率排序为NH4+ > Urea-N > NO3 > NO2,其范围分别为46.6~280.1 nmol/L/h、4.7~21.3 nmol/L/h、1.1~9.8 nmol/L/h和0.03~3.4 nmol/L/h。浮游植物对氮的相对偏好指数(the relative preference index,RPI)结果表明,还原态氮(NH4+和Urea-N)的偏好RPI(NH4+)和RPI(Urea-N)范围分别为2.11~7.95和1.92~4.34显著高于氧化态氮(NO3和NO2RPI(NO3)和RPI(NO2)均小于1。在中、低盐度区域,浮游植物对Urea-N的偏好有时会超过NH4+,即RPI(Urea-N)/RPI(NH4+) > 1。本研究表明,东寨港河口冬季水体溶解态氮中以氧化态的NO3为主,但浮游植物更偏好利用还原态氮。此外,对于还原态氮而言,上游浮游植物对Urea-N的偏好可能较NH4+更高。本研究结果丰富了对小型河口浮游植物不同形态氮吸收的认识。

     

    Abstract: In recent years, due to human activities, a large amount of active nitrogen (N) has been transported into estuaries and coasts, causing eutrophication and harmful algal blooms. Understanding the distribution of different forms of N in estuarine systems and the relative preference of phytoplankton for different N forms is of great practical significance for the algal bloom mechanism exploration and the effective excess N management. In December 2022, environmental parameters and different forms of nitrogen concentrations were investigated in the Dongzhai estuary, Hainan Province. By using the 15N labelling technique, incubation experiments were carried out to quantify the phytoplankton uptake rates of Urea-N, ammonium (NH4+), nitrate (NO3) and nitrite (NO2). The results showed that dissolved N concentrations in the water of Dongzhai estuary decreased along the river to the offshore in winter. The order of N concentration was NO3 > NH4+ > NO2 > Urea-N, which ranged from 5.84−49.78 µmol/L, 1.16−40.64 µmol/L, 0.83−2.98 µmol/L and 0.25−0.98 µmol/L, respectively. The order of N uptake rates was NH4+ > Urea-N > NO3 > NO2, which ranged from 46.6−280.1 nmol/L/h, 4.7−21.3 nmol/L/h, 1.1−9.8 nmol/L/h, and 0.03−3.4 nmol/L/h, respectively. Phytoplankton preferred reducing N (NH4+ and urea-N), more specifically, the value of relative preference index (RPI) of NH4+ RPI(NH4+) and urea-N RPI(Urea-N) is 2.11−7.95 and 1.92−4.34, respectively, higher than the relative preference of oxidizing N (NO3 and NO2) both RPI(NO3) and RPI(NO2) were < 1. At the sampling stations with low and medium salinity, the preference for Urea-N sometimes exceeded that for NH4+, i.e., RPI(Urea-N)/RPI(NH4+) > 1. The study suggests that NO3 is the main dissolved N forms in Dongzhai estuary in winter, but phytoplankton prefers to utilize reduced N. Moreover, phytoplankton living in the upstream may have a higher preference for Urea-N than NH4+. Our study enriches the understanding of different forms of N uptake by phytoplankton in the small estuary.

     

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