高化物地下水的水地化学特性,来源来源,分布和健康风险:地化学控制和来源分配
Muhammad Ayub1, Hira Javed1, Abdur Rashid2
1Department of Botany, Hazara University, Mansehra, PO 21300, Pakistan.
Environmental pollution (Barking, Essex : 1987)
|September 23, 2024
概括
巴基斯坦萨尔戈达的高化物水平.
科学领域:
- 环境科学 环境科学
- 水文地质学 水文地质学
- 地质化学 地质化学
背景情况:
- 地下水被化物 (F−) 污染是一个重大的全球健康问题.
- 饮用水中的高化物度可能导致各种健康问题,包括牙和骨化.
- 了解地下水中化物的来源和控制因素对于风险评估和管理至关重要.
研究的目的:
- 评估巴基斯坦地下水Sargodha的高化物水平,其来源,分布和健康风险.
- 为了确定控制化物缩的水地化学过程.
- 执行源分配并评估地下水适合各种用途的适用性.
主要方法:
- 使用离子染色学收集和分析48个地下水样本.
- 水地化学面积分析和统计相关性.
- 用于污染评估的集群分析 (CA).
- 主要组件分析-多变量线性回归 (PCAMLR) 用于源分配.
- 儿童和成人健康风险评估.
主要成果:
- 43.76%的地下水样本超过了世界卫生组织 (WHO) 的1.5毫克/升的限制,度高达5.8毫克/升.
- 水地化学分析表明,性pH,高Na+和HCO3−,低Ca含量的含水层促进了化物溶解.
- 集群分析显示了三个污染水平:10.4%的污染程度较低,39.5%的污染程度中等,50%的污染程度严重.
- PCAMLR模型确定了F含量矿物质,离子交换,岩石水相互作用和人类活动作为主要来源.
- 与成年人相比,儿童面临的化物毒性的健康风险更高.
结论:
- 萨尔戈达的地下水受到高化物度的严重影响,对健康构成风险.
- 地化学过程,包括碳酸盐贫乏含水层中的阴离子交换和矿物溶解,是化丰富的关键驱动因素.
- 由于化物毒性,地下水不适合饮用,家用和农业用途.
- 需要有效的水资源管理策略来缓解化物污染并保护公共卫生.
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