Modeling pH changes and electrical conductivity in surface water as a result of mining activities

Q3 Engineering
K. C. Aluwong, M. H. M. Hashim, S. Ismail, S. A. Shehu
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Abstract

Purpose. To develop comprehensive models for predicting the pH and electrical conductivity of surface water in Maiganga coal mine and environs affected by mining activities. Methodology. The research utilizes a combination of in-situ measurement, laboratory analysis, modeling technique using Ansys Workbench and Linear Regression for predicting the content of pollutants. In-situ measurement/data collection in the upstream and downstream were carried out to evaluate the potential impact of mining activities on surface and ground water quality. Electrical conductivity and pH were measured on the samples that were collected using Oakton 5/6 pH meter and TDS/EC meter. Findings. According to the results, the regression statistics model of pH and electrical conductivity (EC) shows that the predicted values have a pH range of 4.7–7.05 and a mean pH value of 5.5. In contrast, while the EC ranges from 454.52 to 2,720.68 s/cm (EC) with a mean value of 905 µs/cm of the downstream flow which is completely dependent on the mine inlet (pH-in and EC-in). The findings show a direct correlation between surface water pH, electrical conductivity, and mining activities in the Maiganga coal mine area and their detrimental effects on the ecosystem and water quality. Originality. The results were obtained directly from the mine site during field visit and can be compared to data from active coal mine sites. Practical value. The detrimental effect of the results of mining activities can be controlled if monitoring sensors are introduced at mines’ effluent outlet to alert the mine management of possible danger in real time.
模拟采矿活动导致的地表水 pH 值变化和电导率变化
目的建立预测 Maiganga 煤矿及受采矿活动影响的周边地区地表水 pH 值和导电率的综合模型。方法。这项研究综合利用了现场测量、实验室分析、使用 Ansys Workbench 的建模技术和线性回归技术来预测污染物的含量。在上游和下游进行了现场测量/数据收集,以评估采矿活动对地表水和地下水水质的潜在影响。使用 Oakton 5/6 pH 计和 TDS/EC 计对采集的样本进行了电导率和 pH 值测量。研究结果。结果显示,pH 值和导电率(EC)的回归统计模型显示,预测值的 pH 值范围为 4.7-7.05,平均 pH 值为 5.5。相反,下游水流的导电率范围为 454.52 至 2,720.68 s/cm (EC),平均值为 905 µs/cm,这完全取决于矿井入口(pH-in 和 EC-in)。研究结果表明,地表水 pH 值、导电率与 Maiganga 煤矿区的采矿活动及其对生态系统和水质的不利影响直接相关。原创性。结果是在实地考察矿区时直接获得的,可与活跃煤矿区的数据进行比较。实用价值。如果在矿井排污口引入监测传感器,实时提醒矿井管理部门可能存在的危险,就可以控制采矿活动结果的有害影响。
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来源期刊
CiteScore
1.70
自引率
0.00%
发文量
148
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