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Niektoré problémy tvorby systémov v?asného varovania na zosuvoch

机译:在滑坡上建立预警系统的一些问题

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Prevention against landslides formation or activation is ensured by permanent monitoring of endangered areas, which is transferred to the landslide early warning systems in the socio-economically important sites. The paper describes general issues of the landslide warning systems creation, with an emphasis on their local level and the issues of the critical levels of landslide generating factors derivation. Since the state of the groundwater table level is usually the most important factor of the landslide activation, several methods of its critical level determination are used. The authors preferentially deal with the description of the model of parameters of groundwater regime, which was derived on the basis of their long-term experience in monitoring of landslides and other slope deformations. The model is based on the derivation of parameters characterizing the depth of the groundwater table level and duration of unfavorable conditions. The resulting parameters of the groundwater regime are compared with the indicators of kinetic activity of landslide masses (obtained by geodetic and inclinometer measurements). Provided there is a sufficiently close correlation between the groundwater regime and sliding activity of a landslide, the model can be applied in the definition of the critical levels of the groundwater table and to the prognosis of the expected motional activity of landslide. Practical application of this method is presented on example of slope stability development evaluation of the monitored landslide near the Okoli?né Village.
机译:通过对濒危地区的永久监测,可以防止滑坡的形成或活化,并将其转移到具有社会经济意义的地点的滑坡预警系统中。本文介绍了滑坡预警系统创建的一般性问题,重点是滑坡预警系统的局部性以及滑坡产生因子推导的临界级问题。由于地下水位的状态通常是滑坡活化最重要的因素,因此使用了几种确定其临界水位的方法。作者优先处理地下水状态参数模型的描述,该模型是基于他们在滑坡和其他边坡变形监测方面的长期经验而得出的。该模型基于表征地下水位深度和不利条件持续时间的参数的推导。将得到的地下水状况参数与滑坡体动力学活动指标(通过大地测量和倾角仪测量获得)进行比较。如果地下水状况与滑坡的滑动活动之间存在足够紧密的相关性,则该模型可以用于定义地下水位的临界水位以及预测滑坡的预期运动活动。在Okoli?né村附近被监测滑坡的边坡稳定性开发评估示例中介绍了该方法的实际应用。

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