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Nitrogen and phosphorus species in the coastal and shelf waters of Southeastern North Carolina, Mid-Atlantic U.S. coast

机译:美国中大西洋北卡罗来纳州东南部沿海和陆架水域中的氮和磷物种

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摘要

The diversity of small-scale wetlands, high salinity tidal creeks, salt marshes, estuaries, and a wide and shallow shelf with the Gulf Stream close to the break makes the coastal zone of south-eastern North Carolina (U.S.) a natural laboratory for the study of the cycling of nitrogen (N) and phosphorus (P) in coastal and shelf waters. We assessed the summer concentrations, forms, and ratios for each N (total dissolved N, nitrate+nitrite, ammonium and dissolved organic N) and P (total dissolved P, o-phosphate and dissolved organic P) pool as these nutrients travel from tidal creeks, salt marshes and two large estuaries to Long and Onslow Bays. Additionally, we measured ancillary physical (temperature, salinity and turbidity) and chemical (dissolved oxygen, chlorophyll a and pH) water properties. Highest concentrations of all individual N and P compounds were found in the upper parts of each tributary and were attributed to loads from agricultural and urban sources to the coastal watersheds, continuing downstream to receiving estuaries. In all areas, dissolved organic N and P species were predominant constituents of the total dissolved N and P pools (64-97% and 56-93%, respectively). The lower parts of estuaries and surface shelf waters were characterized by oceanic surface values, indicating removal of N and P downstream in all tributaries. The different watershed and hydrological characteristics also determined the different speciation of N and P pools in each estuary. Despite a high level of anthropogenic pressure on the uppermost coastal waters, there is self-regulation in this coastal ecosystem with respect to human perturbations; i.e. significant amounts of the N and P load are retained within estuarine and nearshore waters without reaching the shelf.
机译:小规模的湿地,高盐度的潮汐小溪,盐沼,河口以及宽阔而浅的陆架以及墨西哥湾流接近断裂处的多样性,使北卡罗莱纳州东南部的美国(美国)沿海地区成为了天然实验室。沿海和陆架水域中氮(N)和磷(P)循环的研究。当这些营养物从潮汐传播时,我们评估了每个氮(总溶解氮,硝酸盐+亚硝酸盐,铵和溶解有机氮)和磷(总溶解磷,邻磷酸盐和溶解有机磷)的夏季浓度,形式和比率。小河,盐沼和龙湾和昂斯洛湾的两个大型河口。此外,我们测量了辅助物理(温度,盐度和浊度)和化学(溶解氧,叶绿素a和pH)水的性质。在每个支流的上部发现了所有单独的N和P化合物的最高浓度,这归因于从农业和城市资源到沿海集水区的负荷,一直到下游入海口。在所有区域中,溶解的有机氮和磷物质是溶解氮和磷总量的主要成分(分别为64-97%和56-93%)。河口下部和地表水的特征是洋面值,表明所有支流下游的氮和磷都被去除。不同的流域和水文特征也决定了每个河口N和P池的形态不同。尽管最上层沿海水域的人为压力很高,但该沿海生态系统在人为干扰方面有自我调节作用;也就是说,大量的氮和磷负荷被保留在河口和近岸水域内而没有到达架子。

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