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对卡拉巴尔(尼日利亚东南部)河流和地下水的物理参数进行监测以及对其化学成分进行评估。

Monitoring of the physical parameters and evaluation of the chemical composition of river and groundwater in Calabar (Southeastern Nigeria).

作者信息

Edet Aniekan, Worden Richard H

机构信息

Department of Earth and Ocean Sciences, University of Liverpool, 4 Brownlow Street, Liverpool, L69 3GP, UK.

出版信息

Environ Monit Assess. 2009 Oct;157(1-4):243-58. doi: 10.1007/s10661-008-0532-y. Epub 2008 Sep 27.

Abstract

A 12-month study was carried to assess the seasonal and tidal effects on the physical parameters of river and groundwater, which constitute the major potable water sources in Calabar (Nigeria). The study also included an evaluation of the chemical composition of the different water bodies and their relationship. The results show that there was a significant seasonal effect on dissolved oxygen (DO) and nitrate in groundwater on one hand, and on temperature, redox potential (Eh), and DO in river water on the other. Also, a significant tidal influence exists on DO in both river-and groundwater. Comparison between groundwater and river water show statistically significant difference in EC, TDS, Eh, DO, Na, Cl and NO(3). The significant differences in EC, TDS, Na and Cl are due to tidal flushing. The difference in Eh is due to geology of the area while, NO(3) is as a result of anthropogenic pollution. The concentrations of ions in the river and groundwater for the different seasons and tidal cycles show an inverse relationship, while the river water is generally more concentrated than the groundwater. Using a binary mixing model, estimates show that the degree of mixing of river water and groundwater is low, with values of between 1.93% and 2.76% respectively, in the western and eastern parts of the study area. The study concludes that tidal flushing, anthropogenic effects and oxygen supply during recharge contribute to the shaping of water chemistry in the area.

摘要

开展了一项为期12个月的研究,以评估季节和潮汐对河流及地下水物理参数的影响,河流及地下水是(尼日利亚)卡拉巴尔主要的饮用水源。该研究还包括对不同水体化学成分及其关系的评估。结果表明,一方面,季节对地下水中的溶解氧(DO)和硝酸盐有显著影响,另一方面,对河水中的温度、氧化还原电位(Eh)和溶解氧也有显著影响。此外,潮汐对河水和地下水中的溶解氧均有显著影响。地下水与河水的比较显示,二者在电导率(EC)、总溶解固体(TDS)、Eh、溶解氧、钠、氯和硝酸盐方面存在统计学上的显著差异。电导率、总溶解固体、钠和氯的显著差异是由于潮汐冲刷。Eh的差异是由于该地区的地质情况,而硝酸盐则是人为污染的结果。不同季节和潮汐周期下河流及地下水中离子的浓度呈反比关系,且河水通常比地下水的浓度更高。使用二元混合模型进行估算表明,研究区域西部和东部河水与地下水的混合程度较低,分别为1.93%至2.76%。该研究得出结论,潮汐冲刷、人为影响以及补给期间的氧气供应对该地区水化学特征的形成起到了作用。

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