Effect of temperature on D.O and T.D.S: A measure of Ground and Surface Water Interaction

Q2 Environmental Science Water Science Pub Date : 2021-01-01 DOI:10.1080/11104929.2020.1860276
E. Thomas
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引用次数: 3

Abstract

ABSTRACT To statistically quantify ground and surface water interaction using temperature as a tracer and its effect on chemical properties of rivers, a total number of 30 sample points were selected at regular intervals along the profile of the two rivers. Ten points on the upper Ona River, and ten on the Alaro River, the remaining ten on the lower section of the river. Also, a corresponding number of nearby groundwater samples were obtained from a parallel source, for each of the surface water sample points so as to aid comparison. The coordinates of the sample points along the river profile were obtained using a global positioning system (GPS) device. The result of the investigation showed that two of the properties (Total Dissolved Solid and Dissolved Oxygen) of surface water vary significantly while the third (Temperature) does not vary significantly across the river profile extending from the upstream section to the downstream section. It was further observed that the underlying geology in terms of rock types have a significant influence on the properties of the surface water body, this was corroborated through comparison of the groundwater properties against that of the surface water. No significant correlation was observed between temperature and total dissolved solids and dissolved oxygen, thus inferring no form of noteworthy influence from temperature on the considered parameters in this study. The analysis of temperature gradients along a river profile and its effect on water properties provided an insight to the quantitative estimates of rates of interaction through the use of statistics and a possible inferred direction.
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温度对D.O和T.D.S的影响:地下水和地表水相互作用的测量
摘要为了以温度为示踪剂对地下水和地表水的相互作用及其对河流化学性质的影响进行统计量化,沿两条河流的剖面以规则的间隔选择了总共30个样本点。奥纳河上游有10个点,阿拉罗河上有10个,其余10个在河的下游。此外,对于每个地表水样本点,从平行来源获得相应数量的附近地下水样本,以帮助进行比较。使用全球定位系统(GPS)设备获得沿河流剖面的采样点的坐标。调查结果表明,地表水的两种性质(总溶解固体和溶解氧)变化很大,而第三种性质(温度)在从上游段延伸到下游段的河流剖面上变化不大。进一步观察到,就岩石类型而言,底层地质对地表水体的性质有重大影响,这一点通过地下水性质与地表水性质的比较得到了证实。在温度与总溶解固体和溶解氧之间没有观察到显著的相关性,因此推断出温度对本研究中考虑的参数没有任何形式的显著影响。对河流剖面温度梯度及其对水特性的影响的分析,通过使用统计数据和可能的推断方向,为相互作用速率的定量估计提供了见解。
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来源期刊
Water Science
Water Science Environmental Science-Ecology
CiteScore
3.00
自引率
0.00%
发文量
12
审稿时长
18 weeks
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