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首页> 外文期刊>Landslides >On the landslide event in 2010 in the Monarch Butterfly Biosphere Reserve, Angangueo, Michoacán, Mexico
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On the landslide event in 2010 in the Monarch Butterfly Biosphere Reserve, Angangueo, Michoacán, Mexico

机译:关于2010年在墨西哥米却肯州Angangueo的帝王蝶生物圈保护区发生的滑坡事件

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摘要

In February 2010, 19 fatalities and economic damage were caused by a regional landslide episode in the state of Michoacán, México. The municipalities of Angangueo, Ocampo, Tiquicheo de Nicolás Romero, Tuxpan, and Tuzantla were severely damaged, with Angangueo being the most affected. The event involved a series of debris flows, of which four were the most significant; these four caused 16 deaths in addition to considerable damage to roads, electricity, and the water supply system, with indirect consequences in crop production, cattle farming, and tourism. The area affected by these four flows was calculated as 282 km ~2, with an estimated 697,346 m ~3 of mobilized material. General observations indicated that the initiation sources of the debris flows were on deforested zones. The present research is concentrated on the Angangueo basin, an area situated within the Monarch Butterfly Biosphere Reserve. Given the lack of rain gauges in the area of interest, records from neighboring points were used to build a comprehensive overview of the extreme precipitation event that triggered the devastating debris flows. The nearest rain gauge, Laguna del Fresno, situated 21 km to the south, recorded 204 mm of rainfall from 1 to 5 February, equivalent to 30% of the mean annual rainfall. Moreover, during a 24-h period the El Bosque rain gauge recorded 144. 5 mm of precipitation, the equivalent of 2,270% of the mean rainfall for the same month (6. 36 mm). The occurrence of a hailstorm preceding the rainfall event is notable; conditions in the superficial soil layer would have included an increased pore water pressure. Presumably, before the 2,000-year return period extreme rainfall event, thawing of hail and consequent moisture and/or pore-pressure increase result in decreased frictional strength. This paper presents a spatial analysis of the distribution of these landslides, mainly debris flows, as well as general observations on the triggering mechanism, the strength properties of the materials involved, and the societal impact.
机译:2010年2月,墨西哥米却肯州发生区域性滑坡,造成19人死亡和经济损失。 Angangueo,Ocampo,Tiquicheo deNicolásRomero,Tuxpan和Tuzantla等城市受到严重破坏,其中Angangueo受影响最大。该事件涉及一系列泥石流,其中四个是最严重的。除了严重破坏道路,电力和供水系统外,这四人还造成16人死亡,对作物生产,养牛业和旅游业造成间接影响。受这四股水流影响的面积经计算为282 km〜2,估计有697,346 m〜3的动员材料。一般观察表明,泥石流的起始源位于森林砍伐区。目前的研究集中在位于帝王蝶生物圈保护区内的Angangueo盆地。鉴于感兴趣的地区缺乏雨量计,因此使用邻近点的记录来全面记录引发降雨的泥石流的极端降水事件。最近的雨量计Laguna del Fresno位于南部21公里处,2月1日至5日的降雨量为204毫米,相当于年平均降雨量的30%。此外,在24小时内,El Bosque雨量计记录到144. 5毫米的降雨量,相当于当月平均降雨量(6. 36毫米)的2270%。降雨事件发生前发生冰雹是很明显的。表层土壤层的条件可能包括增加的孔隙水压力。据推测,在2000年回归期之前的极端降雨事件之前,冰雹的融化以及随之而来的水分和/或孔隙压力的增加导致了摩擦强度的降低。本文对这些滑坡(主要是泥石流)的分布进行了空间分析,并对触发机理,所涉及材料的强度特性以及社会影响进行了一般性观察。

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