区域与地方同位素梯度:来自意大利中部中山地区的洞察和建模
Alberto Tazioli1, Davide Fronzi, Stefano Palpacelli2
1Department of Science and Matter Engineering, Environment and Urban Planning (SIMAU), Università Politecnica delle Marche, Via Brecce Bianche 12, 60131, Ancona, Italy.
Ground water
|February 16, 2024
概括
这项研究引入了一种新的同位素数据处理方法,以精确确定复杂的山地地形中的弹和井充电区. 该方法提高了意大利阿宁山脉地下水系统的理解.
科学领域:
- 水文地质学 水文地质学
- 同位素水文学 同位素水文学
- 环境科学 环境科学
背景情况:
- 复杂的山地地形和含水层接触挑战了传统的同位素水文学.
- 了解这些地区的地下水充电对于水资源管理至关重要.
研究的目的:
- 开发和应用一种原始的同位素数据处理方法,用于识别喷泉和井的可能充电区域.
- 评估同位素建模与山区水文地质环境之间的一致性.
主要方法:
- 一个两步的方法,涉及计算的同位素充电高度和先进的三角洲18O沉分布模型.
- 基于统计和GIS的程序,包括剪切降水三角洲18O值和计算重叠分布.
- 定义一个新的区域三角洲18O梯度,并推导当地的降水-海拔关系.
主要成果:
- 为意大利中部定义了一个新的区域三角洲18O梯度.
- 获得了7个局部降水-海拔关系和LMWL.
- 评估了喷泉和井的充电区域的平均高度,验证了新的同位素建模方法.
结论:
- 开发的同位素建模方法有效地识别了复杂的山地地形中可能的地下水充电区域.
- 这项研究证实了稳定的氧同位素在阿佩宁链内的地下水系统的特征化中的实用性.
- 这种方法为在具有挑战性的环境中进行水文地质调查提供了有价值的工具.
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