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Analysis of a database for anthropogenic sinkhole triggering and zonation in the Naples hinterland (Southern Italy)

机译:那不勒斯腹地(意大利南部)的人为污水触发和区划数据库分析

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摘要

Anthropogenic sinkholes are generally due to the collapse of man-made underground caves and represent a major threat, especially in urban contexts, where they could cause damage to people, buildings and lifelines. The hinterland of Naples (Campania, Southern Italy) is one of the most urbanized areas of Italy and is historically affected by frequent sinkhole phenomena. This study analyzes a database of both man-made caves and sinkholes collected by the authors over several years. The aim is to comprehend the predisposing and triggering factors of sinkholes in order to attempt a zonation of occurrence. The predisposing factor resulted to be the presence of a preexisting network of caves within the Campanian Ignimbrite tuff and their geometric features. Generally, the shallower the depth of the chamber roof and the lower the thickness of the vault, the higher is the frequency of sinkholes. Furthermore, an intrinsic fragility is represented by the access shafts of vertical wells, usually filled in and abandoned. Meanwhile, the main triggering mechanism identified consists in saturation of the subsoil, due to water leaks coming from buried sewage and water pipelines. The macrozonation of sinkhole occurrence shows that the highest class is achieved where the tuff is shallow and both man-made caves and historical sinkholes are present.
机译:人为的污水露通常是由于人造地下洞穴的崩溃,代表了主要威胁,特别是在城市环境中,他们可能会对人们,建筑物和生活造成损害。那不勒斯的腹地(南部意大利南部)是意大利最城市化的地区之一,历史上受到频繁的污水现象。本研究分析了作者在几年内收集的人造洞穴和下沉孔的数据库。目的是理解下沉和触发污水洞的因素,以便尝试分区发生。概述因素导致坎帕尼亚可燃性凝灰岩内的洞穴预测网络及其几何特征存在。一般来说,较浅的腔室屋顶的深度和拱顶的厚度越低,下沉孔的频率越高。此外,内在脆性由垂直孔的进入轴表示,通常填充并被抛弃。同时,鉴定的主要触发机制由埋藏污水和水管道泄漏的漏水引起的亚静脉。污水孔的宏观发生表明,最高阶级是实现的,其中凝灰岩浅,存在人造洞穴和历史下沉孔。

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