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首页> 外文期刊>Bulletin of engineering geology and the environment >Introducing a new classification of soft rocks based on the main geological and engineering aspects
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Introducing a new classification of soft rocks based on the main geological and engineering aspects

机译:基于主要地质和工程方面介绍了软岩的新分类

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Soft rock masses represent a significant percentage of rock material on the earth's crust. The engineering properties of these rocks are related to their composition, geological history, and degree of weathering. Mudrocks (claystone, mudstone, argillite), marl, shale, sandstone, and conglomerates with weak cementing material are the most common example of these rocks which can be subjected to a wide variation of their engineering properties. Generally, they can be grouped in a broad sense, as geological materials with very low intact rock properties, namely, high deformability and low strength that span the range between soils and hard rocks. This paper is organized to suggest a classification for these rocks, dealing with the main geological and engineering aspects and features that characterize these materials. The two indices of soft rock number (SRN) and soft rock activity (SRA) have been introduced in this classification. The SRN is obtained based on the geomechanical properties of soft rocks, and it is within a range from 0 to 100 (0 for very weak rocks and 100 for strong ones). On the other hand, the SRA index, which indicates how rocks respond to disturbance, is calculated using an empirical graph. This index can have values from 0 to 1. If the index is closer to 0, the rock mass will be less sensitive to disturbance. Based on the two indices, the weakest group of soft rocks, which is called swelling soft rocks, has SRNs less than 20 and SRAs higher than 0.8. Excavation of these rocks can be accompanied by various types of failures. Moreover, in high-strength soft rocks, SRNs and SRAs have values higher than 80 and lower than 0.25, respectively. These rocks have good geomechanical properties and the lowest sensitivity to disturbance, so excavation them results in the fewest failures.
机译:软岩体代表了地壳上的大量岩石材料。这些岩石的工程性质与它们的组成,地质历史和风化程度有关。 Mudrocks(Claystone,Mudstone,Argillite),Marl,页岩,砂岩和弱固结材料的砾岩是这些岩石中最常见的例子,可以受到其工程性质的广泛变化。通常,它们可以以广义分组,作为具有非常低的岩石性能的地质材料,即跨越土壤和硬岩之间的范围的高可变形性和低强度。本文组织,为这些岩石提出了分类,处理了这些材料的主要地质和工程方面和特征。在该分类中介绍了两种软岩数(SRN)和软岩活动(SRA)的指数。基于软岩石的地质力学获得SRN,它在0到100的范围内(对于非常弱的岩石,并且强力岩石100)。另一方面,使用经验图计算岩石的SRA指数,该指数指示岩石如何响应干扰。该索引可以具有0到1的值。如果索引更接近0,则岩体对干扰将不太敏感。基于两种指数,最弱的软岩组称为膨胀软岩,具有小于20的SRN,高于0.8的SRA。这些岩石的挖掘可以伴随着各种类型的故障。此外,在高强度软岩中,SRNS和SRA分别具有高于80且低于0.25的值。这些岩石具有良好的地质力学性质和对扰动的最低敏感性,因此挖掘它们导致最少的故障。

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