同位素研究用于评估地中海沿海岩环境中复杂的地下水循环模式,水文地质区划和水岩相互作用
M Salvadori1, M Pennisi1, R Masciale2
1Institute of Geosciences and Earth Resources, National Research Council (IGG-CNR), 56124 Pisa, Italy.
The Science of the total environment
|October 13, 2024
概括
意大利穆尔吉亚含水层的地下水在三个部门显示出明显的循环模式和岩石相互作用. 西部部门有较长的流动路径,而东部部门则表现出较短的流动路径和直接充电,由于岩特征.
科学领域:
- 水文地质学 水文地质学
- 同位素地质化学 同位素地质化学
- 环境科学环境科学
背景情况:
- 意大利东南部的Murgia水层是一个沿海岩碳酸盐系统.
- 了解地下水的来源和循环对于水资源管理至关重要.
研究的目的:
- 评估地下水的来源,循环和岩石相互作用过程.
- 为了划定水文地质区分和循环模式在Murgia水层.
- 调查地特征对地下水动态的影响.
主要方法:
- 在地下水中的化学和同位素特征 (O,H,Sr,B) 的空间分析.
- 水地质数据与地下水质量监测的整合.
- 根据循环模式和停留时间区分地下水部门.
主要成果:
- 在Murgia含水层中发现了三个不同的部门,由内部充电区供水.
- 西部部门显示了显著的水岩相互作用的证据,表明长流路径.
- 东部部门的特点是短暂的停留时间和通过地特征直接充电,水岩相互作用有限.
结论:
- 地下水的循环和停留时间在Murgia含水层部门之间有很大差异.
- 卡斯特形态强烈影响地下水的动态和充电在东部部门.
- 透水的混合发生在中央部门,对于同位素签名的获取居住时间不足.
相关概念视频
Precipitation and Co-precipitation
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
Microbes and Other Elemental Cycles
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
Deep Sea Microbial Ecology
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...
Soil Microbial Ecology
Soil microbial ecology is defined by highly diverse, spatially structured communities that drive nutrient cycling, organic matter turnover, and overall ecosystem stability. Although a gram of soil can contain thousands of bacterial and archaeal taxa, the ecological processes they mediate are even more crucial for sustaining terrestrial life.Microhabitats and NichesSoil is a heterogeneous mixture of minerals, organic matter, water, and air. Microbes inhabit distinct microhabitats formed by...


