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Influence of composition and grain size distribution on the properties of limestone and dolomite asphalt fillers

机译:组成和粒度分布对石灰石和白云石沥青填料性能的影响

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The aim of the present research work is to examine the influence of mineral composition and grain size distribution on the properties of limestone and dolomite mineral fillers used in Hungarian road construction. Since these properties fundamentally define the features of asphalt pavements, our research goals were assigned accordingly. Different fractions of two mineral fillers (limestone from Alsozsolca and dolomite from Pilisvoeroesvar) were compared. We have observed deviations in the grain size distribution of some fractions of fillers that were free of contaminations. While limestone consists of a great amount of fines and a relatively small amount of coarse grains, in case of dolomite it is the opposite, that is, small amount of fines and greater amount of coarse grains. The decrease of the grain size of fractions resulted in a slight increase of specific surface area of fillers. We have observed that by the decrease of the grain size of fillers, the hydrophilic coefficient has also decreased. The increasing presence of fines however, resulted in the decrease of the hydrophilic coefficient.
机译:本研究工作的目的是研究矿物组成和粒度分布对匈牙利道路建设中使用的石灰石和白云石矿物填料性能的影响。由于这些特性从根本上定义了沥青路面的特征,因此我们的研究目标也相应地确定了。比较了两种矿物填料(Alszsolca的石灰石和Pilisvoeroesvar的白云石)的不同馏分。我们已经观察到一些不含污染物的部分填料的晶粒尺寸分布存在偏差。石灰石由大量的细颗粒和相对少量的粗颗粒组成,而在白云岩的情况下则相反,也就是说,细的颗粒细颗粒和大量的粗颗粒。馏分的晶粒尺寸的减小导致填料的比表面积略有增加。我们已经观察到,通过减小填料的晶粒尺寸,亲水系数也减小了。然而,细粉的存在增加导致亲水系数降低。

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