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Loess in China and landslides in loess slopes

机译:中国的黄土和黄土斜坡的滑坡

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Loess in china is outstanding for its stratigraphical intactness,huge thickness,vast expanse ofdistribution and metastable geotechnical properties. During the Quaternary Period the arid,semi-arid climaticenvironment provided the stage on which material sources came into being,grain particles were wind-transportedand deposited and loess strata were thus formed. The paper puts emphasis on the granulometry and engineeringproperties peculiar to loessial deposits as well as the role they might play in the initiation and evolution of loesslandslides. From this,the paper proceeds to such problems as geomorphological zonation,landslide distribution,morphological and structural features of loess landslides as well as landslide classifications,giving due attentionto seismic landslides. This is followed by a summing-up of the methods of landslide prevention and remediation.Finally,the issues that need more attention and further in-depth research are raised.
机译:中国的黄土以其地层完好,厚度大,分布广,亚稳岩土特性而著称。在第四纪时期,干旱,半干旱的气候环境提供了物质来源形成,风粒输送和沉积,形成黄土地层的阶段。本文重点介绍了黄土沉积物特有的粒度和工程性质,以及它们在黄土滑坡的形成和演化中可能发挥的作用。据此,本文提出了黄土滑坡的地貌分区,滑坡分布,形态结构特征以及滑坡分类等问题,引起了地震滑坡的重视。最后对滑坡的防治方法进行了总结。最后,提出了需要进一步重视和深入研究的问题。

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