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Seasonal and spatial dynamics of nutrients and phytoplankton biomass in Victoria Harbour and its vicinity before and after sewage abatement

机译:污水减排前后维多利亚港及邻近地区养分和浮游植物生物量的季节和空间动态

摘要

This study investigated the seasonal and spatial dynamics of nutrients and phytoplankton biomass at 12 stations in Hong Kong (HK) waters during a three year period from 2004 to 2006 after upgraded sewage treatment and compared these results to observations before sewage treatment. Pearl River estuary (PRE) discharge significantly increased NO3 and SiO4 concentrations, particularly in western and southern waters when rainfall and river discharge was maximal in summer. Continuous year round discharge of sewage effluent resulted in high NH4 and PO4 in Victoria Harbour (VH) and its vicinity. In winter, spring and fall, the water column at all stations was moderately mixed by winds and tidal currents, and phytoplankton biomass was relatively low compared to summer. In summer, the mean surface phytoplankton chl biomass was generally > 9 mu g L-1 in most areas as a result of thermohaline stratification, and high nutrients, light, and water temperature. In summer, the potential limiting nutrient is PO4 in the most productive southern waters and it seldom decreased to limiting levels (similar to 0.1 mu M), suggesting that phytoplankton growth may be only episodically limiting. The mean bottom dissolved oxygen (DO) remained > 3.5 mg L-1 at most stations, indicating that the eutrophication impact in HK waters was not as severe as expected for such a eutrophic area. After the implementation of chemically enhanced primary sewage treatment in 2001, water quality in VH improved as indicated by a significant decrease in NH4 and PO4 and an increase in bottom DO. In contrast, there were an increase in chl a and NO3, and a significant decrease in bottom DO in southern waters in summer, suggesting that hypoxic events are most likely to occur in this region if phytoplankton biomass and oxygen consumption keep increasing and exceed the buffering capacity of HK waters maintained by monsoon winds, tidal mixing and zooplankton grazing. Therefore, future studies on the long-term changes in nutrient loading from PRE and HK sewage discharge will be crucial for developing future strategies of sewage management in HK waters. (c) 2008 Elsevier Ltd. All rights reserved.
机译:这项研究调查了2004年至2006年的三年期间,对香港(香港)水域的12个站点进行了升级的污水处理后,其养分和浮游生物量的季节和空间动态,并将这些结果与污水处理前的观测结果进行了比较。珠江口(PRE)的排放显着增加了NO3和SiO4的浓度,特别是在西部和南部水域,夏季降雨和河流排放量最大。全年不断排放污水,导致维多利亚港(VH)及其附近地区的NH4和PO4较高。在冬季,春季和秋季,所有站点的水柱都被风和潮流适度混合,与夏季相比,浮游植物的生物量相对较低。夏季,由于盐渍地层分层,高养分,高光照和高水温,大多数地区浮游植物的平均表面生物量通常> 9μg L-1。在夏季,潜在的限制性营养素是南部最富生产力的水域中的PO4,很少减少到限制性水平(类似于0.1μM),这表明浮游植物的生长可能只是流行性的限制性。在大多数站,平均底部溶解氧(DO)保持> 3.5 mg L-1,这表明香港水域的富营养化影响不如对此类富营养化地区的预期那么严重。在2001年实施化学增强的一级污水处理后,VH中的水质得到改善,这是因为NH4和PO4显着减少,而底部DO却增加了。相反,夏季南部水域的chl a和NO3升高,底部DO显着降低,这表明如果浮游植物生物量和氧气消耗持续增加并超过缓冲水平,则该区域最有可能发生缺氧事件。季风,潮汐混合和浮游动物放牧维持香港水域的能力。因此,关于PRE和HK污水排放中养分含量的长期变化的未来研究对于制定香港水域污水管理的未来策略至关重要。 (c)2008 Elsevier Ltd.保留所有权利。

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