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Seasonal dissolved inorganic nitrogen and phosphorus budgets for two sub-tropical estuaries in south Florida, USA

机译:美国南佛罗里达州两个亚热带河口的季节性溶解无机氮和磷预算

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摘要

Interactions among geomorphology, circulation, and biogeochemical cycling determine estuary responses to external nutrient loading. In order to better manage watershed nutrient inputs, the goal of this study was to develop seasonal dissolved inorganic nitrogen (DIN) and phosphorus (DIP) budgets for the two estuaries in south Florida, the Caloosahatchee River estuary (CRE) and the St. Lucie Estuary (SLE), from 2002 to 2008. The Land-Ocean Interactions in the Coastal Zone (LOICZ) approach was used to generate water, salt, and DIN and DIP budgets. Results suggested that internal DIN production increases with increased DIN loading to the CRE in the wet season. There were hydrodynamic effects as water column concentrations and ecosystem nutrient processing stabilized in both estuaries as flushing time increased to >10 d. The CRE demonstrated heterotrophy (net ecosystem metabolism or NEM < 0.0) across all wet and dry season budgets. While the SLE was sensitive to DIN loading, system autotrophy (NEM > 0.0) increased significantly with external DIP loading. This included DIP consumption and a bloom of a cyanobacterium (Microcystis aeruginosa) following hurricane-induced discharge to the SLE in 2005. Additionally, while denitrification provided a microbially-mediated N loss pathway for the CRE, this potential was not evident for the SLE where N2 fixation was favored. Disparities between total and inorganic loading ratios suggested that the role of dissolved organic nitrogen (DON) should be assessed for both estuaries. Nutrient budgets indicated that net internal production or consumption of DIN and DIP fluctuated with inter- and intra-annual variations in freshwater inflow, hydrodynamic flushing, and primary production. The results of this study should be included in watershed management plans in order to maintain favorable conditions of external loading relative to internal material cycling in both dry and wet seasons.
机译:地貌,循环和生物地球化学循环之间的相互作用决定了河口对外部养分负荷的响应。为了更好地管理流域的养分输入,本研究的目的是为佛罗里达州南部两个河口,卡卢萨哈奇河河口(CRE)和圣露西河制定季节性溶解无机氮(DIN)和磷(DIP)预算。从2002年到2008年是河口(SLE)。沿海地区的陆海相互作用(LOICZ)方法用于生成水,盐以及DIN和DIP预算。结果表明,在雨季,内部DIN的产生随着DIN对CRE的负载增加而增加。随着冲洗时间增加至> 10 d,两个河口的水柱浓度和生态系统养分处理均趋于稳定,从而产生了水动力效应。在所有湿季和干季预算中,CRE均显示出异养(生态系统净代谢或NEM <0.0)。尽管SLE对DIN负载敏感,但随着外部DIP负载,系统自养(NEM> 0.0)显着增加。这包括DIP消耗和2005年飓风诱导的SLE排放后蓝藻细菌的繁殖(铜绿微囊藻)。此外,尽管反硝化作用为CRE提供了微生物介导的N损失途径,但对于SLE而言,这种潜力并不明显N2固定受到支持。总和无机负载比之间的差异表明,应同时评估两个河口的溶解性有机氮(DON)的作用。营养预算表明,DIN和DIP的净内部生产或消耗量随着淡水流入量,水力冲洗和初级生产的年内和年内变化而波动。该研究的结果应包括在流域管理计划中,以便相对于干旱和潮湿季节的内部物料循环保持外部装载的有利条件。

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