Changes of water chemistry from rainfall to stream flow in Obagbile Catchment, Southwest Nigeria

Q1 Social Sciences
Mojisola Hannah Omogbehin, Isaac Ayo Oluwatimilehin
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引用次数: 1

Abstract

Water chemistry changes when it flows through different pathways. This study aims to characterize the differences of water chemistry of five kinds of water in Obagbile Catchment including rainwater, overland flow, soil water, groundwater, and stream water, determine the changes in water chemistry that occur as the water moves from one pathway to another, and identify the factors responsible for the water chemistry changes. To do these, we collected 50 water samples from 10 heavy storms whose rainfall are equal to or more than 10 ​mm within an hour to test the changes of water properties across various pathways in this study. The results show that the overland flow had the highest pH and electrical conductivity (EC) and the rainwater had the lowest value of the two parameters. Ca2+, Mg2+, Clˉ, and HCOŌ were found to have their highest concentrations in stream water; meanwhile, NO3, NH4+, and SO42− were found to have almost same low concentrations in all the water samples. K+ was only dominant in stream water; while dissolved organic carbon (DOC) was lowest in rainwater, same in overland flow, soil water, and groundwater samples, and highest in stream flow. Principal Component Analysis (PCA) showed that for all the water samples from different pathways, two factors mainly accounted for the total variances. The two factors were related to the crustal and anthropogenic sources in rainwater suggesting that the high loadings of major cations (e.g., Ca2+ and Mg2+) in rainwater samples are soil-derived. The PCA for the overland flow and soil water showed strong correlations between pH, EC, and the concentrations of Na+, Mg2+, HCOO, and CH3COO, while the high loadings of all the parameters and the strong correlations among each other were evident in the stream water. In conclusion, the chemical constituents found in water are also the constituents of pathways through which the water flows. The major factors responsible for the change in the physico-chemical properties of water in Obagbile Catchment are weathering and anthropogenic activities.

尼日利亚西南部Obagbile流域从降雨到水流的水化学变化
当水流经不同的路径时,水的化学成分会发生变化。本研究旨在表征Obagbile流域雨水、坡面流、土壤水、地下水和溪水五种水的水化学差异,确定水从一条路径流向另一条路径时发生的水化学变化,并确定导致水化学变化的因素。为此,我们在一小时内收集了10次降雨量等于或大于10毫米的暴雨中的50个水样,以测试本研究中不同途径的水性质变化。结果表明:坡面流pH和电导率最高,雨水pH和电导率最低;其中,Ca2+、Mg2+、Cl - 2+和HCOŌ的浓度最高;同时,NO3−、NH4+和SO42−在所有水样中的低浓度几乎相同。K+仅在溪水中占优势;溶解有机碳(DOC)在雨水中最低,在坡面流、土壤水和地下水中最低,在溪流中最高。主成分分析(PCA)表明,对于所有不同途径的水样,总方差主要由两个因素造成。这两个因素与雨水中的地壳和人为来源有关,表明雨水样品中主要阳离子(如Ca2+和Mg2+)的高负荷是土壤来源的。坡面水流和土壤水的主成分分析结果表明,pH、EC与Na+、Mg2+、HCOO−和CH3COO−浓度之间存在较强的相关性,而河流水体中各参数均具有较高的负荷,且各参数之间存在较强的相关性。总之,在水中发现的化学成分也是水流动途径的成分。造成奥巴比尔流域水理化性质变化的主要因素是风化和人为活动。
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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来源期刊
Regional Sustainability
Regional Sustainability Social Sciences-Urban Studies
CiteScore
3.70
自引率
0.00%
发文量
20
审稿时长
21 weeks
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