在典型的大沉积平原中,封闭地下水的水地化学特征,起源和质量评估
Yuqing Zhang1, Yong Xiao1,2,3, Hongjie Yang1,4
1Faculty of Geosciences and Engineering, Southwest Jiaotong University, Chengdu, China.
概括
干旱平原的地下水提取对水化质量产生影响,其中97%的化物标准超过,造成健康风险. 可持续使用需要差异化的水资源管理,避免因盐化风险而灌.
科学领域:
- 水文地质学 水文地质学
- 环境科学 环境科学
- 水资源管理 水资源管理
背景情况:
- 长期的人为开采已经扰乱了干旱沉积平原的封闭地下水.
- 评估水化品质量对于可持续发展和识别潜在的健康威胁至关重要.
研究的目的:
- 调查中部北中国平原的水化特征和封闭地下水的形成.
- 评估水质是否适用于家庭和灌用途.
- 评估与地下水质量相关的潜在健康风险.
主要方法:
- 封闭地下水样本的水化分析.
- 评估水岩相互作用 (溶解,阴离子交换).
- 使用值加权水质指数 (EWQI).
- 评估非致癌性健康风险.
主要成果:
- 地下水略有性,以Cl-Na和HCO3-Na类型为主.
- 水的化学作用是由水与岩石的相互作用控制的.
- 97%的样本超过了化物 (F-) 标准,主要是由于地质因素和开采.
- 高化物对90%以上的人口构成中等至高的非致癌风险.
- 97%的地下水根据EWQI适合家庭使用,但化物风险仍然存在.
结论:
- 北中国平原的封闭地下水表现出高化物水平,对健康构成重大风险,特别是对儿童.
- 由于盐化和透风险,应避免长期使用灌.
- 为科学和合理的地下水资源管理,建议采用不同的供水策略.
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