论文标题

温度连续控制粘土斜率的稳定性

Temperature continuously controls the stability of clay slopes

论文作者

Loche, Marco, Scaringi, Gianvito

论文摘要

随着气候变化,我们期望在全球许多地区发生更频繁的极端天气事件。这些事件会引发破坏性,致命的自然危害,这引起了媒体的注意并提高公民和政策制定者的认识。洪水,野火,滑坡是大量研究的对象。但是,它们仍然很难预测和处理。气候变化也意味着温度更高,尤其是在陆地上。冰川融化,永久冻结。到处都是,地面变得越来越温暖,深度越来越高。乍一看,没什么大不了的。几个额外的学位可以做什么?微生物和真菌变得更加活跃,化学平衡转移。即使是科学家,无声的变化也没有注意到。在滑坡研究中,斜坡的稳定性是重量,水压和机械强度的平衡。在冰点之上,温度被排除在外,但不应该。在土壤中经常丰富的粘土的强度对温度敏感。通过简单的数值练习,我们显示温度在多大程度上可以调节,甚至破坏了整个季节和全球变暖的粘土斜率的稳定性。可能导致非极端天气事件的沉默变化会带来更严重的后果。

With climate change, we are expecting more frequent extreme weather events in many regions worldwide. These events can trigger disruptive, deadly natural hazards, which catch the attention of the media and raise awareness in citizens and policymakers. Floods, wildfires, landslides are the object of a great deal of research. Yet, they remain difficult to predict and handle. Climate change also means warmer temperatures, especially on land. Glaciers melt, permafrost thaws. Everywhere, the ground gets warmer down to increasing depths. At first sight, not a big deal. What can a few extra degrees do? Microbes and fungi becomes more active, chemical equilibria shift. Silent changes are left unnoticed, even by scientists. In landslide studies, the stability of slopes is a balance of weights, water pressures, and mechanical strengths. Above freezing, temperature is left out, yet it should not be. The strength of clays, which frequently are abundant in soils, is sensitive to temperature. With a simple numerical exercise, we show to what extent temperature can condition and even undermine the stability of clay-bearing slopes, across the seasons and under global warming. A silent change that could make a non-extreme weather event have much more severe consequences.

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