尼日利亚中部比达盆地两个湿地沉积物的有机碳(OC)和有机质(OM

Ahmed Aliyu Sidi, Ipoola Ajani Okunlola, Nuhu Musa Waziri
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摘要

利用简易螺旋沉淀物取样器在比达盆地北部两个湿地的浅层处收集沉淀物进行实验室研究,以确定这两个湿地对地下水化学质量的影响。水中溶解有机碳含量是影响地下水水质元素地球化学循环的重要组成部分。根据颗粒大小的特征,沉积物作为元素运输的管道和途径,在评估途径内的污染物流动性时要考虑。采集了具有代表性的岩心沉积物样品,进行了粒径表征和有机质(OM)、有机碳(OC)、含水率(MC)的化学分析。比重计结果表明,两处沉积物粒径大小均为砂土>粘土>粉砂,少数例外。这代表了该地区的地质情况(砂岩)。egabako部分地区沉积物中OC和OM的平均值分别为1.14%和1.98%。相比之下,Bida部分沉积物中OC和OM的平均值分别为1.72%和2.97%。两个湿地沉积物的OC和OM值较低,可能是沿地下水通道进入含水层而溶解的。沉积物中分析的其他理化参数相关性较差。在Bida和Egbako部分薄片上,OM与OC呈极显著正相关,R2分别为1和0.9。两个研究地点的沉积物酸度较低,Egbako和Bida的平均pH值分别为5.64和5.13。沉积物的低酸性以及OM和OC组成可能会影响沉积物中的生物地球化学过程,并可能影响这两个研究地点的地下水化学质量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Organic Carbon (OC) and Organic Matter (OM) in Sediments Collected from Two Wetlands in Central Bida Basin, Nigeria
An improvised auger sediment sampler was used to collect sediments at shallow depths from two wetlands in the Northern Bida Basin for laboratory studies in order to ascertain the impact on the chemical quality of groundwater within these two studied locations. The dissolved organic carbon content of water is an important component of the geochemical cycling of elements capable of affecting groundwater quality. The sediments which serve as a conduit and pathways for the elements’ transport depending on the characteristics of the particle sizes are to be considered in the evaluation of contaminant mobility within the pathways. Representative cored sediment samples were collected and their particle size characterization and chemical analysis for Organic Matter (OM), Organic Carbon (OC) and Moisture Content (MC) were carried out. The hydrometer results show that the sediment particle sizes are in the order of sand > clay > silt in both locations with few exceptions. This represents the geology of the area (sandstone). The Mean values of 1.14% and 1.98% of OC and OM respectively were recorded in the sediment samples collected in parts of Ebgako. In contrast, 1.72% and 2.97% mean values were recorded in sediments collected in part of Bida for OC and OM respectively. The values of the OC and OM in the sediments from the two wetlands are low and may have been dissolved along the groundwater pathways to the aquifer. Other physicochemical parameters analysed in the sediments showed poor correlation. OM and OC were strongly positively correlated and showed an R2 value of 1 and 0.9 respectively for parts of the Bida and Egbako sheets. There is low acidity of the sediments from the two study locations with a mean pH value of 5.64 and 5.13 respectively for Egbako and Bida. The low acidic nature of the sediments and the OM and OC composition have the potential to influence biogeochemical processes in the sediments and can affect the chemical quality of the groundwater in these two study locations.
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