Noriega Carlos E D, Araujo Moacyr
Laboratório de Oceanografia Física Estuarina e Costeira, Departamento de Oceanografia, Universidade Federal de Pernambuco, Recife, PE, Brasil.
An Acad Bras Cienc. 2011 Jun;83(2):441-56. doi: 10.1590/s0001-37652011000200007.
This paper focuses on the nutrient dynamics of a tropical estuary on the northeastern Brazilian coast, studied using the LOICZ biogeochemical budgeting protocol. We describe the methodology and assumptions underlying this model. Input data (monthly for rainfall, evaporation, river discharge, and concentrations of salt, phosphorus and nitrogen) were obtained during field campaigns in the Barra das Jangadas Estuary (BJE) over a 5 years period (1999 to 2003). Mass balance results indicate large inputs of nutrients to the system. The model shows that the seasonal variation of the Net Ecosystem Metabolism (NEM) indicates that the system passes from a stage of organic matter liquid production and mineralization during the dry season (-0.5 mmoles C m(-2) d(-1)) to liquid mineralization during the rainy season (-19 mmoles C m(-2) d(-1)). We suggest that the system varies slightly between autotrophy and heterotrophy during the year due to the rainfall regime, human activities in the basin (density population and sugarcane plantations), and associated DIP riverine loads. High per capita loads of N and P indicate a high population density and high runoff. The application of flux balance modeling was useful to understand the nutrient dynamics of this typical small tropical estuary.
本文聚焦于巴西东北海岸一个热带河口的营养动力学,采用国际地圈-生物圈计划(LOICZ)生物地球化学预算协议进行研究。我们描述了该模型的方法和假设。输入数据(降雨、蒸发、河流流量以及盐、磷和氮浓度的月度数据)是在5年期间(1999年至2003年)对雅加达达斯河口(BJE)进行实地考察时获得的。质量平衡结果表明该系统有大量的营养物质输入。该模型显示,净生态系统代谢(NEM)的季节变化表明,该系统从旱季的有机物液体生产和矿化阶段(-0.5毫摩尔碳/平方米·天)转变为雨季的液体矿化阶段(-19毫摩尔碳/平方米·天)。我们认为,由于降雨模式、流域内的人类活动(人口密度和甘蔗种植园)以及相关的溶解性无机磷河流负荷,该系统在一年中自养和异养之间略有变化。高人均氮和磷负荷表明人口密度高和径流量大。通量平衡模型的应用有助于理解这个典型的小型热带河口的营养动力学。