预测碎屑扇上泥石流沉积体积的统计方法

L. Franzi, G. Bianco
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引用次数: 24

摘要

本文旨在提供一种有用的方法来预测与高寒地区盆地末端扇上的泥石流相关的碎屑体积g。预测泥石流的发生和规模往往是一项非常困难的任务,因为必须考虑与泥石流的开始、传播和沉积有关的地质、水力和降水因素的可变性。这些因素以及它们对沉积在碎屑扇上的碎屑体积的影响都不容易量化。即使一些作者提出了一些有用的数学(和确定性)关系来预测可能的碎片体积,它们似乎也没有考虑到影响因素的高度可变性。由于这些原因,对g和盆地面积a之间的关系进行了统计调查。本文利用众所周知的统计方法,并利用大约200个数据样本(指高山地区),提出了一个预测可能Gs值的新准则。对于给定的流域,该值是根据任意选择的统计风险度获得的。还提出了一种概率方法,在没有对特定流域进行准确调查的结果时,这种方法可以为第一次危险区划分和减轻措施的设计提供合理的基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A statistical method to predict debris flow deposited volumes on a debris fan

The present paper aims to give a useful methodology to predict the debris volume Gs associated to a debris flow and deposited on the basin's terminal fan in the alpine region. Predicting the occurrence and the magnitude of a debris flow is often a very difficult task, as it is necessary to consider the variability of the geological, hydraulic and pluviometric factors connected to the beginning, propagation and deposition of a debris flow. These factors are not easily quantifiable, as well as their influence on the debris volumes deposited on the debris fan. Even if some useful mathematical (and deterministic) relations have been proposed by some authors to predict the likely debris volumes, they do not seem to take into account the high variability of the influencing factors. For these reasons a statistical investigation of the relationship between Gs and the basin area A has been undertaken. By means of well known statistical methodologies and by using a sample of about two hundred data (referred to the alpine region), a new criterion is proposed, in the present paper, for the prediction of a probable Gs value. For a given basin, this value is obtained on the basis of a statistical risk degree arbitrarily chosen. A probabilistic methodology is also proposed, which, when results of an accurate survey are not available for a particular basin, may provide a rational basis for a first hazard zonation and the design of mitigative measures.

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