Temporal changes in limno-morphometric characteristics in a floodplain lake within Cross River ecosystem during low water period

G. Nwonumara, O. I. Okogwu
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Abstract

Iyieke Lake is one of the floodplain lakes within the middle reaches of the Cross River, it is a major foraging and breeding site of several fish species. It is not directly connected to any river, so the water level depends on seasonal inundation by the Cross River. With gradual changes in precipitation and consequent alteration in flooding pattern, and increased agricultural activities around the lake, there are indications of steady annual decline in water level and quality, and lake area. In order to understand the effect of these changes on the aquatic biota, the morphology and some limnological parameters of the lake were studied during low water period (March-May) in 2005, 2011 and 2019 at interval of 6.5 years. Water samples were collected from the lake and the limno-morphological parameters measured at the littoral and limnetic zones of the lake following standard procedures. The results showed that monthly rainfall was significantly (p<0.05) lower in 2019 compared to 2005 and 2011, while minimum and maximum temperature trended conversely (p<0.05). The mean total dissolved solids (TDS) increased from 13.00mg/l in 2005 to 39.33mg/l in 2019 and conductivity trended the same. Mean nitrate (0.92mg/l) and phosphate (1.78mg/l) were higher in 2019 compared to 2005 and 2011. Contrarily, transparency decreased from 0.45m in 2005 to 0.19m in 2019. Similarly, mean dissolved oxygen (3.80mg/l), maximum length (443.20m) and width (314.50m) declined significantly toward 2019 (p<0.05). Lake length, transparency, conductivity and TDS that were seemingly good predictors of water deterioration could be useful in modelling, which is vital in conserving the biodiversity of the Cross River floodplain ecosystem.
克洛斯河洪泛区湖泊生态系统低潮期湖底形态特征的时间变化
伊耶克克湖是克罗斯河中游河漫滩湖泊之一,是多种鱼类的主要觅食和繁殖地。它没有直接与任何河流相连,因此水位取决于克罗斯河的季节性淹没。随着降水的逐渐变化和由此引起的洪水格局的改变,以及周围农业活动的增加,有迹象表明水位、水质和湖泊面积逐年稳步下降。为了了解这些变化对水生生物群的影响,研究了2005年、2011年和2019年3月至5月的淡水期湖泊形态和部分湖泊参数,间隔6.5 a。按照标准程序从湖泊中采集水样,并在湖泊的沿岸区和沿岸区测量湖泊形态参数。结果表明:与2005年和2011年相比,2019年的月降雨量显著减少(p<0.05),最低气温和最高气温呈相反趋势(p<0.05)。平均总溶解固形物(TDS)从2005年的13.00mg/l增加到2019年的39.33mg/l,电导率也呈相同趋势。与2005年和2011年相比,2019年的平均硝酸盐(0.92mg/l)和磷酸盐(1.78mg/l)更高。相反,透明度从2005年的0.45万下降到2019年的0.19万。2019年平均溶解氧(3.80mg/l)、最大长度(443.2 m)和宽度(314.50m)也显著下降(p<0.05)。湖泊长度、透明度、电导率和TDS看似是水质恶化的良好预测指标,可用于建模,这对保护克罗斯河洪泛区生态系统的生物多样性至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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