首页> 外文期刊>Hydrobiologia >The status and characteristics of eutrophication in the Yangtze River (Changjiang) Estuary and the adjacent East China Sea, China.
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The status and characteristics of eutrophication in the Yangtze River (Changjiang) Estuary and the adjacent East China Sea, China.

机译:长江口和邻近的中国东海富营养化的现状和特征。

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摘要

Eutrophication has become increasingly serious and noxious algal blooms have been of more frequent occurrence in the Yangtze River Estuary and in the adjacent East China Sea. In 2003 and 2004, four cruises were undertaken in three zones in the estuary and in the adjacent sea to investigate nitrate (NO3-N), ammonium (NH4-N), nitrite (NO2-N), soluble reactive phosphorus (SRP), dissolved reactive silica (DRSi), dissolved oxygen (DO), phytoplankton chlorophyll a (Chl a) and suspended particulate matter (SPM). The highest concentrations of DIN (NO3-N+NH4-N+NO2-N), SRP and DRSi were 131.6, 1.2 and 155.6 micro M, respectively. The maximum Chl a concentration was 19.5 mg m-3 in spring. An analysis of historical and recent data revealed that in the last 40 years, nitrate and SRP concentrations increased from 11 to 97 micro M and from 0.4 to 0.95 micro M, respectively. From 1963 to 2004, N:P ratios also increased from 30-40 up to 150. In parallel with the N and P enrichment, a significant increase of Chl a was detected, Chl a maximum being 20 mg m-3, nearly four times higher than in the 1980s. In 2004, the mean DO concentration in bottom waters was 4.35 mg l-1, much lower than in the 1980s. In comparison with other estuaries, the Yangtze River Estuary was characterized by high DIN and DRSi concentrations, with low SRP concentrations. Despite the higher nutrient concentrations, Chl a concentrations were lower in the inner estuary (Zones 1 and 2) than in the adjacent sea (Zone 3). Based on nutrient availability, SPM and hydrodynamics, we assumed that in Zones 1 and 2 phytoplankton growth was suppressed by high turbidity, large tidal amplitude and short residence time. Furthermore, in Zone 3 water stratification was also an important factor that resulted in a greater phytoplankton biomass and lower DO concentrations. Due to hydrodynamics and turbidity, the open sea was unexpectedly more sensitive to nutrient enrichment and related eutrophication processes..
机译:富营养化变得越来越严重,有害的藻华在长江口和邻近的东海频繁发生。 2003年和2004年,在河口和邻近海域的三个区域进行了四次航行,以调查硝酸盐(NO3-N),铵盐(NH4-N),亚硝酸盐(NO2-N),可溶性活性磷(SRP),溶解反应性二氧化硅(DRSi),溶解氧(DO),浮游植物叶绿素a(Chl a)和悬浮颗粒物(SPM)。 DIN(NO3-N + NH4-N + NO2-N),SRP和DRSi的最高浓度分别为131.6、1.2和155.6 microM。春季最大Chl a浓度为19.5 mg m-3。对历史和最新数据的分析表明,在过去40年中,硝酸盐和SRP的浓度分别从11微米增加到97微米,从0.4微米增加到0.95微米。从1963年到2004年,N:P的比例也从30-40增加到150。与N和P富集同时,检测到Chla显着增加,Chl最大值为20 mg m-3,几乎是四倍。高于1980年代。 2004年,底水中的溶解氧平均浓度为4.35 mg l-1,远低于1980年代。与其他河口相比,长江口具有较高的DIN和DRSi浓度,而具有较低的SRP浓度。尽管养分浓度较高,但内河口(1区和2区)的Chla浓度却比邻近海域(3区)的低。根据养分的可利用性,SPM和水动力,我们假设在1区和2区浮游植物的生长受到高浊度,大潮汐幅度和短停留时间的抑制。此外,在3区中,水分层也是导致浮游植物生物量增加和DO浓度降低的重要因素。由于流体动力学和浑浊性,公海出乎意料地对养分富集和相关的富营养化过程更加敏感。

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