希腊热水和矿泉水中的微量元素的表征
Lorenza Li Vigni1, Kyriaki Daskalopoulou2,3, Sergio Calabrese1,4
1DiSTeM, University of Palermo, Via Archirafi 36, Palermo, Italy.
概括
希腊热矿泉水表现出不同微量元素度,受温度和pH值的影响. 由于超出安全限值,一些元素会造成环境和健康风险.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 水文地质学 水文地质学
背景情况:
- 希腊自然热水和矿泉水普遍存在,这与其地力学环境有关.
- 多样化的地质和构造条件导致水的化学成分和同位素成分多样化.
研究的目的:
- 为了分析来自希腊276个热矿泉水源的微量元素数据.
- 研究控制元素度及其地理分布的来源和过程.
主要方法:
- 汇编和分析了276个已公布和未公布的微量元素水数据.
- 根据温度和pH标准对数据进行分组.
- 评估微量元素,温度,pH,氧化还原条件和盐度之间的相关性.
主要成果:
- 微量元素的度差异很大,受溶解度,温度,酸度,氧化还原和盐度的影响.
- 诸如,Ti,Sr,As和Tl这样的元素与温度正相关,通常是由于水与岩石的相互作用.
- 其他元素 (Be,Al,Cu,Se,Cd) 与温度没有或相反的相关性,可能是由于过度和.
- 大多数微量元素与pH呈反相关性;与Eh没有发现关系.
- 海水污染和水岩相互作用是盐度和元素含量的关键驱动因素.
结论:
- 希腊热矿泉水表现出复杂的微量元素行为,受多种环境因素的影响.
- 偶尔超出被接受的限值表明,通过水循环,可能对环境造成损害,对人类健康有间接风险.
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