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首页> 外文期刊>Natural Hazards and Earth System Sciences Discussions >Relationship between rainfall and shallow landslides in the southern Apuan Alps (Italy)
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Relationship between rainfall and shallow landslides in the southern Apuan Alps (Italy)

机译:南方扶盟降雨与浅层滑坡(意大利)的关系

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The Apuan Alps region is one of the rainiest areas in Italy (more than 3000 mm/year), in which frequently heavy and concentrated rainfall occurs. This is particularly due to its geographical position and conformation: the Apuan chain is located along the northern Tuscan coast, close to the Ligurian Sea, and the main peaks reach almost 2000 m. In several cases, the storms that hit the area have triggered many shallow landslides (soil slip-debris flows), which exposed the population to serious risks (during the 19 June 1996 rainstorm about 1000 landslides were triggered and 14 people died). The assessment of the rainfall thresholds is very important in order to prepare efficient alarm systems in a region particularly dedicated to tourism and marble activities. With the aim of contributing to the landslide hazard evaluation of the southern Apuan Alps territory (upper Versilia area), a detailed analysis of the main pluviometric events was carried out. The data recorded at the main rain gauge of the area from 1975 to 2002 were analysed and compared with the occurrence of soil slips, in order to examine the relationship between soil slip initiation and rainfall. The most important rainstorms which triggered shallow landslides occurred in 1984, 1992, 1994, 1996, 1998 and 2000. Many attempts were made to obtain a possible correlation between rainfall parameters and the occurrence of soil slip phenomena and to identify the local rainfall threshold for triggering shallow landslides. A threshold for soil slip activity in terms of mean intensity, duration and mean annual precipitation (MAP) was defined for the study area. The thresholds obtained for the southern Apuan Alps were also compared with those proposed by other authors for several regions in the world. This emphasized the high value of the rain threshold for shallow landslide activity in the Apuan area. The high threshold is probably also linked to the high mean annual precipitation and to the high frequency of rainstorms.
机译:扶盟阿尔卑斯地区是意大利最衰落的地区之一(超过3000毫米/年),其中经常发生重大和集中的降雨。这尤其是由于其地理位置和构象:APUAN链位于北托斯卡纳海岸,靠近利古里亚海,主要峰值达到近2000米。在几个案例中,袭击该地区的风暴引发了许多浅层滑坡(土壤湿润碎片流量),这将人口暴露于严重风险(1996年6月19日1996年6月1996年6月触发了1000次滑坡和14人死亡)。降雨阈值的评估非常重要,以便在特别致力于旅游和大理石活动的区域中准备高效的报警系统。旨在为南方扶盟阿尔卑斯州境内(上部Versilia地区)的滑坡危害评估有所贡献,进行了对主要的Pluviometric事件的详细分析。分析了1975年至2002年的主要雨量计的数据,并与土壤滑动的发生进行了比较,以检查土壤滑坡启动与降雨之间的关系。 1984年,1992年,1994年,1996年,1998年,1998年,2000年引发了浅层滑坡最重要的暴雨。许多尝试是在降雨参数和土壤滑移现象的发生方面获得可能的相关性,并确定触发的局部降雨阈值浅山体滑坡。在平均强度,持续时间和平均年降水(MAP)方面,对研究区域定义了土壤滑移活性的阈值。与世界上几个地区的其他作者提出的那些相比,为南方扶盟获得的门槛也被比较。这强调了避难区浅层滑坡活动的雨阈值的高价值。高阈值可能也与高平均年降水量和暴雨的高频相连。

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