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Expansivity of Neogene clays and glacial tills from central Poland

机译:来自波兰中部的新近纪粘土和冰川耕作的膨胀性

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The revision of classification methodologies for determination of soil expansivity revealed that parameters most frequently used for this purpose are: the liquid limit, plasticity index and swelling parameters which also predominate in older systems of expansive soil assessment, regarded as classical. Seventy-nine soil samples, including Neogene clays and glaciall tills from central Poland, with a wide range of plasticity were examined for a comparative analysis of soil expansivity with a use of eight empirical methods. The study revealed that Neogene clays are mostly highly and very highly expansive, while glacial tills exhibit low to medium expansivity. Compared to classifications considering soil mineralogy indicators, those correlated solely to Atterberg limits and related parameters were found to overestimate soil expansivity. It is evident that the classifications are in better agreement for glacial tills than for clays. The comparison of mineral composition measured and predicted from swelling tests yielded consistent results.
机译:对用于确定土壤膨胀性的分类方法的修订表明,最常用于此目的的参数为:液体极限,可塑性指数和溶胀参数,这些参数在旧的膨胀土壤评估系统中也占主导地位,被认为是经典的。使用八种经验方法,对79种土壤样品(包括来自波兰中部的Neogene黏土和冰川耕地)进行了广泛的可塑性分析,以比较分析土壤的膨胀性。研究表明,新近纪粘土大多具有很高的膨胀性,而冰川耕种的膨胀性低至中等。与考虑土壤矿物学指标的分类相比,仅与阿特伯格限值和相关参数有关的分类被高估了土壤膨胀性。显然,冰川耕作的分类比粘土更好。溶胀试验测得的和预测的矿物成分的比较得出一致的结果。

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