Detecting the flow relationships between deep and shallow aquifers in an exploited groundwater system, using long‐term monitoring data and quantitative hydrogeology: the Acque Albule basin case (Rome, Italy)
Detecting the flow relationships between deep and shallow aquifers in an exploited groundwater system, using long‐term monitoring data and quantitative hydrogeology: the Acque Albule basin case (Rome, Italy)
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利用长期监测数据和定量水文地质学检测已开发地下水系统中深层和浅层含水层之间的流动关系：Acque Albule 盆地案例（意大利罗马）
DOI：
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发表时间：
2012
期刊：
影响因子：
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通讯作者：
G. Capelli
中科院分区：
文献类型：
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作者：
F. La Vigna;R. Mazza;G. Capelli
在Acque Albule盆地（AAB）复杂的水文地质系统中进行了五年的水文地质监测和实地活动，以确定水文地质背景、深层和浅层含水层之间的关系以及使用常规定量技术确定该开采区的概念性地下水流模型。该盆地位于亚平宁山脉西侧靠近罗马（意大利）和科利阿尔巴尼火山以北，在南北向断层系统（约115 000年前）发育后沉降。AAB经历了强烈的热液活动，产生了一个大型的钙钛矿存款（80米厚）。地下水存款构成了一个断裂含水层，这是超过5 m3 s-1的水的最终目的地，并通过采石场活动强烈脱水。
Five years of hydrogeological monitoring and field activities performed in the complex hydrogeological system of the Acque Albule basin (AAB) were conducted to define the hydrogeological setting, the relationship between deep and shallow aquifers and a conceptual groundwater flow model of this exploited area using conventional quantitative techniques. The basin, which is located close to Rome (Italy) on the west side of the Apennine chain and just north of the Colli Albani volcano, subsided after development of a north–south fault system (about 115 000 y bp). The AAB experiences intense hydrothermal activity, which has produced a large travertine deposit (80‐m thick). The travertine deposit constitutes a fractured aquifer that is the final destination of more than 5 m3 s‐1 of water and is strongly dewatered by quarry activities.