热带河口的潮汐动力学和物理化学参数:尼日利亚东南海岸夸伊博河河口

Emeka V I, Emeka C N, Ebong E D, Ojong R A, Chikezie P C
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引用次数: 1

摘要

河口是重要的生态系统,支持生物多样性并影响其所占地区的经济。对尼日利亚尼日尔三角洲夸伊博河口生态系统质量进行了主要理化指标评价。考察了潮流对入海口物理化学参数空间分布的影响。在旱季现场测量了其理化参数,包括透明度、温度、盐度、溶解氧、密度和pH。利用langagian方法对春潮和小潮周期的潮流速度进行了监测,结果表明退潮占优势。采用Pearson相关矩阵对理化参数之间的关系进行统计分析。基于Pearson相关,密度呈现显著相关(p <0.05),与温度、pH和盐度有关。地表和底水温度显著相关(p <利用ArcGIS Pro软件绘制理化参数的空间分布图。利用聚类分析解释了地底水参数的异同。结果显示,在研究区有两组反映了不同的物理化学特征。第一组,代表河口的上部和中部部分,由低碱性到低盐,微酸性到低溶解氧(4mg/l)条件下的中性水域定义。由于夸伊博河的强河流输入,河口上游表现为沼泽条件。第二组为下河口,以中咸水至正常海水为特征;pH值中性至微碱性,溶解氧低(<4 mg / l)条件。本研究对今后河口及类似潮汐生态系统的监测与评价具有一定的指导意义。& # x0D;
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Tidal Dynamics And Physicochemical Parameters In A Tropical Estuary: Qua-Iboe River Estuary, Southeast Coast Of Nigeria
Estuaries are important ecosystems that support biodiversity and influence the economy of the regions they occupy. Major physicochemical variables of Qua-Iboe River estuary in the Niger Delta region of Nigeria were assessed for ecosystem quality. The influence of tidal current on the spatial distribution of physicochemical parameters in the estuary was examined. Physicochemical parameters, including transparency, temperature, salinity, dissolved oxygen, density and pH were measured in-situ during the dry season. Tidal current velocities were monitored over spring and neap tidal cycles using the Langragian method and results indicated ebb dominance. The relationships between physicochemical parameters were statistically analyzed using Pearson’s correlation matrix. Based on Pearson’s correlation, density showed significant correlations (p < 0.05) with temperature, pH and salinity. Surface and bottom water temperatures significantly correlated (p < 0.05) with density, salinity, dissolved oxygen and pH. Spatial distribution maps of physicochemical parameters were plotted using ArcGIS Pro. Similarities and dissimilarities of surface and bottom water parameters were interpreted using cluster analysis. Results revealed two groups reflecting distinct physicochemical characteristics in the study area. Group one, representing upper and central portions of the estuary is defined by waters which are limnetic to oligohaline, slightly acidic to neutral with low dissolved oxygen (<4mg/l) conditions. The estuary showed limnetic conditions at the upper reaches due to the strong fluvial input by the Qua-Iboe River. Group two, representing the lower estuary, is characterized by mesohaline to normal marine waters; neutral to slightly alkaline pH, and low dissolved oxygen (< 4mg/l) conditions. This study is relevant for future monitoring and assessment of the estuary and similar tidal ecosystems.
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