Landslides Rainfall One of the Main Triggering Factors in the Mountainous Regions of Puebla, Mexico

Cuanalo Campos Oscar Andrés
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Abstract

The rains are one of the main triggers of landslide phenomena in the mountainous region of Puebla, which values reach up 4500 mm/year in some places in this area. Rainfalls combined with other factors such as morphology (mountainous topographic relief with strong inclinations), strongly folded sedimentary rocks (conglomerates, sandstones, siltstones, and limestones), rock discontinuities (fissures, cracks, joints, stratigraphic planes, etc.) and human activity (cuts, excavations, overloads, mining, water discharge, deforestation, land use change, etc.), offer a scenario prone to landslide phenomena that cause human casualties, economic and environmental losses. The landslides disasters have affected many social sectors from these communities (housing, education, health, hydraulic infrastructure, electricity, communication, transportation, public services, agriculture, forestry, etc.), observing that in these sites there are communities of ethnic groups Nahuatls, Totonacs, Otomies and Tepehuas who build their houses out of sheet metal, cardboard, plastic and wood where any natural phenomenon represents a true disaster. This article presents the relationship between hurricanes and torrential rains with the disasters caused in communities in the mountainous region of Puebla. From the analysis of the data obtained from the different meteorological stations installed in the region of interest during a period of 20 years (1999 – 2019), an empirical rainfall threshold of 100 mm/day was determined as a trigger for landslides in the region of study. The aforementioned value is very important data for Civil Protection Government Authorities in order to establish actions and strategies for mitigation and risk management due to landslides. From this rain threshold, evacuation actions are put into operation to reduce the vulnerability of exposed and fragile communities which are immediately transferred to protection shelters
墨西哥普埃布拉州山区山体滑坡的主要诱发因素之一是降雨
降雨是普埃布拉山区山体滑坡现象的主要诱因之一,该地区某些地方的降雨量高达 4500 毫米/年。降雨量加上其他因素,如形态(具有强烈倾斜的山地地形)、强烈褶皱的沉积岩(砾岩、砂岩、粉砂岩和石灰岩)、岩石的不连续性(裂缝、裂隙、节理、地层平面等)以及人类活动(切割、翻越等)。人类活动(切割、挖掘、超载、采矿、排水、砍伐森林、改变土地用途等),这些因素都容易导致山体滑坡现象,造成人员伤亡、经济和环境损失。山体滑坡灾害影响了这些社区的许多社会部门(住房、教育、卫生、水利基础设施、电力、通信、交通、公共服务、农业、林业等),在这些地方还有纳瓦特人、托托纳克人、奥托米人和特佩华人等少数民族社区,他们用金属板、纸板、塑料和木材建造房屋,任何自然现象都是一场真正的灾难。本文介绍了飓风和暴雨与普埃布拉山区社区所遭受灾害之间的关系。通过对 20 年间(1999-2019 年)在相关地区安装的不同气象站获得的数据进行分析,确定了 100 毫米/天的经验降雨阈值,作为研究地区山体滑坡的触发因素。对于民防政府当局来说,上述数值是非常重要的数据,有助于制定缓解和管理山体滑坡风险的行动和战略。从这一降雨阈值开始,疏散行动便开始实施,以降低暴露在外的脆弱社区的脆弱性,并立即将其转移到保护庇护所
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