在巴西的自来水中稳定的和氧同位素的空间变化
João P Sena-Souza1, Fábio J V Costa2, Tiago B Kisaka3
1Laboratório de Geografia Física, Departamento de Geociências, Universidade Estadual de Montes Claros, Montes Claros, Minas Gerais 39401-089, Brazil.
The Science of the total environment
|June 21, 2025
概括
这项研究为巴西提供了第一个详细的水同位素地图,揭示了自来水中明显的空间模式. 这些模式反映了影响全国各地降水量的主要天气系统.
科学领域:
- 水文学的水文学
- 同位素地球化学 同位素地球化学
- 气候学 气候学 气候学
背景情况:
- 与全球模型相比,区域水域异地图提供了更好的空间表现.
- 了解水源的起源对于水资源管理和气候研究至关重要.
- 巴西庞大的领土需要详细的区域同位素数据.
研究的目的:
- 用稳定的同位素为巴西创造了第一个全面的自来水同位素.
- 研究自来水同位素与地理/气候变量之间的关系.
- 在巴西的自来水中绘制 δ18O 和 δ2H 的空间分布图.
主要方法:
- 收集和分析了575个自来水样本,以检测 δ18O 和 δ2H.
- 使用热解与同位素比质谱相结合,用于精确的同位素确定.
- 采用多重线性回归和普通 kriging 进行空间插值和预测.
主要成果:
- 观察到的 δ2H 值在 -63.9 ‰ 到 15.4 ‰ 之间,而 δ18O 值在 -9.2 ‰ 到 3.7 ‰ 之间.
- 龙头水的同位素地图呈现出明显的梯度,稳定同位素值从西南到东北巴西不断增加.
- 空间模式与主要气象系统相关,如热带融合区 (ITCZ) 和南大西洋融合区 (SACZ).
结论:
- 开发的自来水异构图准确地代表了巴西各地的同位素变化.
- 龙头水中的同位素特征与当前的气象和水文过程密切相关.
- 这项研究为巴西未来的水资源和气候研究提供了基础数据集.
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