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Multidisciplinary Study of Subsidence and Sinkhole Occurrences in the Acque Albule Basin (Roma, Italy)

机译:Acce albule盆地沉降和污水井下发生的多学科研究(罗马,意大利)

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We present the results of a combined analysis of remote sensing and geophysical‐geotechnical data carried out in the Acque Albule Basin, a sinkhole prone area located close to the city of Roma, where a wide travertine wedge is present. We carried out geophysical measurements and borehole drillings over two test areas to image the subsoil where paroxysmal surficial dynamics occur. One site is marked by subsidence occurring at least since the early 2000s, whereas the other site hosts the “La Regina” and “Colonnelle” sinkhole lakes, which discharge sulfur‐carbonated waters. The stability of these two sites threatens highway, railway, and airport facilities, and this study helps to assess the geological hazard. For example, InSAR and LiDAR data helped define wide scale subsidence over the last 20?years and previously undetected small‐scale morphologies. Geophysical measurements of the latter revealed shallow and deep dissolution affecting the travertine and driving surficial paroxysmal events. Both study sites were found to lie inside a large depression located at the junction between Jurassic carbonate and Plio‐Pleistocene units in association with paleo karst morphologies in the travertine deposits and affected by the present‐past spillage of sulfurous waters. Given these elements, multidisciplinary geophysical observations are crucial for assessing and mitigating the geological risk and guiding land use planning and management. Plain Language Summary The Acque Albule Basin is a sinkhole prone area of carbonate rocks. The lithoid travertine has been quarried since the Etruscans time and represented the main building material during ancient Roman time (Lapis Tiburtinus). Currently, this region is actively mined and also exhibits frequent sinkhole activity. However, urban development has notably increased over the last decades, subjecting the infrastructure and population to high geologic risk and complicating effective geological and geophysical investigations due to the lack of access and anthropogenic noise. Thus, we used remote sensing to identify a wide subsiding sector involving also urban centers and a geophysical‐geotechnical study to assess the predisposing factors affecting the travertine and generating surficial paroxysmal events that may affect the farmlands and nearby cities. The integrated approach used in this study provides a guideline for geological risk assessment and rational urban planning.
机译:我们介绍了Acce Albule Basin的遥感和地球物理 - 岩土技术数据的综合分析结果,位于罗马市靠近罗马市的污水俯卧区,存在宽阔的石灰华楔。我们在两个测试区域进行了地球物理测量和钻孔钻孔,以将围绕派生结构动态发生的底层进行成像。一个网站以自2000年代初以来至少发生的沉降,而另一个网站主持“La Regina”和“Colonnelle”污水湖泊,其中排出硫磺碳酸盐水域。这两个地点的稳定性威胁着公路,铁路和机场设施,这项研究有助于评估地质危害。例如,INSAR和LIDAR数据有助于在过去的20年内定义广泛的抑制率?年份和以前未被检测的小规模形态。后者的地球物理测量揭示了影响石斑鱼和驱动表演阵发性事件的浅层和深度溶解。发现两个研究遗址位于位于侏罗纪碳酸盐和PloIo-alioistocene单位的交界处的大萧条内部,与古老的岩溶沉积物中的古老喀斯特形态以及受到硫磺水域的目前过度的溢出影响。鉴于这些要素,多学科地球物理观察对于评估和减轻地质风险和指导土地利用规划和管理至关重要。普通语言摘要ACCEAL型盆地是碳酸盐岩的污水区。由于伊特鲁斯人的时间以来,Lithoid Traburtine已经被调查,并在古罗马时代(Lapis Tiburtinus)期间代表了主要的建筑材料。目前,该地区积极开采,也表现出频繁的污水孔活动。然而,由于缺乏接入和人为噪声,城市发展在过去几十年中,在过去的几十年中,将基础设施和人口达到高地质风险,并使有效的地质和地球物理调查复杂化。因此,我们使用遥感来确定涉及城市中心的广泛子学区和地球物理 - 岩土学研究,以评估影响石灰华和产生可能影响农田和附近城市的表观阵发性事件的易受诱惑因素。本研究中使用的综合方法为地质风险评估和理性城市规划提供了指导。

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