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Shift from P to N limitation of phytoplankton biomass across the Pearl River Estuarine plume during summer

机译:夏季珠江口羽流中浮游植物生物量从P限制到N限制的变化

摘要

Anthropogenic loading of nutrients in rivers often increases disproportionally among N,P, and Si, and thus may shift the type of phytoplankton nutrient limitation in the coastal receiving waters. The effect of anthropogenic nutrient loading has rarely been addressed in the Pearl River estuary along the southern coast of China, even though it is one of the largest rivers in the world. We conducted a cruise along the Pearl River estuary and adjacent coastal waters south of Hong Kong during July 17 to 18, 1999. Samples were taken for salinity and nutrients (NO3, SiO4, PO4, NH4 and urea) and nutrient addition experiments were conducted on board. Vertical profiles of salinityshowed a salt-wedge estuary and the coastal plume covering the waters south of Hong Kong. Concentrations of NO3 were very high (ca 90 μM) upstream of the Pearl River estuary, and much of the riverine NO3 was not utilized in the estuary until depletion at the edge of the coastal plume on the east side of Hong Kong. SiO4 was 120 μM upstream and its utilization was similar to that of NO3. PO4 was low in surface waters (0.5 μM) and higher below the halocline in the estuary. NH4 and urea were generally 4 and 1.5 μM, respectively. In the estuary, N:P ratio was 200:1, indicating potential P limitation, while N:Si was below 1:1. Beyond the coastal plume to the east of Hong Kong, N:P and N:Si ratios were 5:1 and 1:0.3, respectively, indicating potential N limitation. Nutrient limitation was shown in nutrient addition experiments and was consistent with the ratios of nutrients. Therefore, nutrient limitation shifted across the coastal plume from P limitation in the estuary to N limitation in the oceanic waters. Potential P limitation was observed in the estuary; P and Si co-limiting occurred at the edge of the coastal plume, and N was limiting in the oceanic side. This spatial shift in nutrient limitation has great implications for nutrient pollution control and coastal management of Hong Kong waters.
机译:河流中人为造成的养分负荷通常在N,P和Si之间成比例增加,因此可能改变沿海接收水域中浮游植物养分限制的类型。尽管中国是世界上最大的河流之一,但在中国南部沿海的珠江河口,人为养分负荷的影响很少得到解决。 1999年7月17日至18日,我们沿着珠江口及香港南部附近的沿海水域进行了巡游。对盐分和养分(NO3,SiO4,PO4,NH4和尿素)进行了采样,并在1999年进行了养分添加实验。板。盐度的垂直剖面显示一个盐楔河口和覆盖香港南部水域的沿海羽状流。珠江口上游的NO3浓度非常高(约90μM),直到河水在香港东侧的边缘被耗尽之前,河中的大部分NO3才被利用。 SiO4上游为120μM,其利用率与NO3相似。在地表水中,PO4含量低(<0.5μM),在河口以下的盐含量高。 NH4和尿素通常分别小于4和1.5μM。在河口,N:P比为200:1,表明潜在的P限制,而N:Si则低于1:1。除了香港东部的沿海羽状流之外,N:P和N:Si的比例分别<5:1和1:0.3,表明潜在的N限制。在养分添加实验中显示了养分限制,并且与养分比例保持一致。因此,营养物质的限制从沿海的羽状流从河口的P限制转变为海洋水域的N限制。在河口观察到了潜在的P限制; P和Si共同限制发生在沿海羽状流的边缘,而N在海洋一侧受到限制。养分限制的这种空间变化对香港水域的养分污染控制和海岸管理具有重大意义。

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