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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岩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成分和晶粒尺寸分布对匈牙利道路建设中使用的石灰石和白云岩矿物填料的性能。由于这些属性从根本上定义了沥青路面的特征,因此我们的研究目标得到了相应的分配。比较了两种矿物质填料的不同部分(来自苏醒肠和来自Pilisvoeroevar的白云石的石灰石)。我们已经观察到晶粒尺寸分布的偏差,这些填料的一部分没有污染物。虽然石灰石由大量的细粒和相对少量的粗粒组成,但在白云石的情况下,它是相反的,即少量细粒和更大的粗粒。馏分的晶粒尺寸的降低导致填料的比表面积略有增加。我们观察到,通过填料的晶粒尺寸的降低,亲水系数也降低了。然而,粒度的增加导致亲水系数的降低。

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