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首页> 外文期刊>Revista de la Asociación Geológica Argentina >Estudio de las condiciones del techo del permafrost y de la capa activa del terraplén de asentamiento del Museo Otto Nordenskj?ld, Isla Cerro Nevado, Antártida
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Estudio de las condiciones del techo del permafrost y de la capa activa del terraplén de asentamiento del Museo Otto Nordenskj?ld, Isla Cerro Nevado, Antártida

机译:南极塞罗内华达岛奥托·诺登斯凯尔德博物馆的多年冻土顶和沉降路堤活动层条件研究

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Study of current conditions of the active layer and top of permafrost of the embankment under the Otto Nordenskj?ld Museum, Cerro NevadoIsland, AntarcticaThe Otto Nordenskj?ld hut was built in Cerro Nevado Island, Antarctica, in 1902. It was named as Historic Site and Monument No. 38 by the AntarcticTreaty and as National Historic Monument by a decree of the Argentinian government (07/26/1965). For this, Argentina must preserve the hut from thenatural deterioration which is subject. In this work, a topographical survey is conducted together with the assessment of the mitigation techniques usedin the area from 1980 to the present in order to prevent permafrost degradation under the museum. Besides, the thermal regime and the spatialdistribution of the active layer and the top of permafrost and their interaction with different topographic variables are analyzed. The studies conducted inthe area showed the close surface location of the frozen ground favours the surface subsidence by melting of the underground ice. This phenomenoncreates concavities where the snow is trapped. When it is melted, it transfers heat to the environment increasing shallow frozen ground degradation.These processes occur near the hut Otto Nordenskj?ld Museum, so a fast intervention was necessary. Prevention works were made by MUSEOANTARprogram during the 2014-2015 Antarctic summer fieldwork and they were focus on the NE-SW embankment slope according to the achieved results.Vertical sheet piles and horizontal gabions were used to fill the depressions with sediments of different grain size in order to raise the average level of thesurface, smooth all sites of snow accumulation and promote cold air circulation.
机译:研究南极​​塞罗内华达州奥托·诺登斯凯尔德博物馆下的路堤活动层和永久冻土层的当前状况奥托诺登斯凯德的小屋建于1902年,位于南极洲塞罗·内华多岛。和南极条约第38号纪念碑,以及阿根廷政府法令(07/26/1965)作为国家历史纪念碑。为此,阿根廷必须保护小屋免受自然退化的影响。在这项工作中,为了防止博物馆下的多年冻土退化,进行了地形调查并评估了该地区从1980年至今使用的缓解技术。此外,还分析了活性层和永久冻土顶的热力状态,空间分布以及它们与不同地形变量的相互作用。在该地区进行的研究表明,由于地下冰层的融化,冰冻地面的靠近地面位置有利于地面沉降。这种现象会在凹陷处形成积雪。当它融化时,它会将热量转移到环境中,从而加剧了浅层冻结地面的退化。这些过程发生在小屋Otto Nordenskjld博物馆附近,因此必须进行快速干预。 MUSEOANTARprogram在2014-2015年南极夏季野外工作期间进行了预防工作,根据取得的成果将其重点放在NE-SW路堤边坡上。为了提高表面的平均水平,使积雪的所有部位变得光滑,并促进冷空气循环。

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