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On the Physico-chemistry and Nutrient Profile in theLagos Harbour

机译:拉各斯港的理化和营养状况

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Physico-chemical and nutrient distribution control lagoon biological productivity, however, focus has been on studies on surface and bottom distribution with little on the vertical profiling of nutrients. Yet it is important to validate physico-chemical properties with nutrients to successfully determine the biological variability and trend of the Lagos harbour. Here, the study was carried out during the rainy season in the months of August, September and October 2014 at surface, 2.6 m and 5.2 m depth to demonstrate quantitatively that variability of nutrients within the Lagos harbour is correlated with physic chemical parameters and depth. Water temperature (°C), pH, Conductivity (μS/cm} and salinity (‰) were measured in-situ. Dissolved oxygen, alkalinity, calcium and magnesium concentration were determined in the laboratory by titremetry, while chloride, sulphate, silicate, nitrate, nitrite and phosphate were determined by colorimetry. The result shows that temperature (23-27°C), pH (7.91-8.68) and dissolved oxygen (6.37-11.20 mg/l) were relatively constant as a result of mixing and the relatively shallow water. Conductivity and salinity were seen to increase down the depth across the months studied. The month of September had the highest physico-chemical and nutrient concentrations reflecting impact of decomposition of introduced macrophytes and high tides. Though nutrient variability as a function of depth was shown to have no significant difference p>0.05, variations down the depth in the months studied were attributed to factors such as tidal influence, chemical precipitation and decomposition. The result indicated that the dynamic in physical and chemical processes are probably the main variables that determine the instantaneous distribution of nutrients. However, subsequent studies are recommended in deeper areas of the harbour to understand and provide information on biological productivity of Lagoons.
机译:理化和养分分布控制泻湖的生物生产力,但是,研究的重点一直放在表面和底部的分布研究上,而很少进行养分的垂直分布分析。然而,重要的是要通过营养物验证其理化性质,以成功确定拉各斯港口的生物变异性和趋势。在这里,这项研究是在2014年8月,9月和10月的雨季期间进行的,深度分别为2.6 m和5.2 m,以定量证明拉各斯港内养分的变化与理化参数和深度有关。在现场测量水温(°C),pH,电导率(μS/ cm}和盐度(‰),并通过滴定法在实验室中测定溶解氧,碱度,钙和镁的浓度,而氯化物,硫酸盐,硅酸盐,用比色法测定硝酸盐,亚硝酸盐和磷酸盐,结果表明温度(23-27℃),pH(7.91-8.68)和溶解氧(6.37-11.20 mg / l)相对恒定。在研究的月份中,电导率和盐分的深度逐渐减小,9月的理化和养分浓度最高,反映了引入的大型植物分解和高潮的影响。结果表明,深度没有显着性差异,p> 0.05,研究月份中深度的下降归因于潮汐影响,化学沉淀和分解等因素。物理和化学过程的动态可能是决定营养素瞬时分布的主要变量。但是,建议在海港深处进行后续研究,以了解并提供有关泻湖生物生产力的信息。

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