20.500.12556/DKUM-53123 Vloga mineralogije v mehaniki zemljin Significance of mineralogy in soil mechanics The research of consistency of limits according to Atterberg is of key importance in soil mechanics because it determines, in a simple way, the results of interactions between solid and liquid phases in soils, and thus provides possibility to classify them in groups with similar mechanical properties. In most cases, the results of these investigations provide a good basis for predicting other properties, such as deformability, expansion, hydraulic conductivity and strength of soils. This proves that the basis factors influencing the values of consistency limits and other mechanical properties are the same. It is known that the values of consistency limits depend on the type and quantity of clay minerals in soils. The article focuses on experimental evidence of dependence between the quantity of water at the liquid limit for soils and type, portion and specific surface of clay grains. Experiments were performed with nonmineral materilas, their mixtures and samples composed of clay- and non-clay components. It was established that in parallel orientation of clay particles the quantity of water between graind and liquid limit is dependent on their external specific surface. The research of consistency limits according to Atterberg is of key importance in soil mechanics because it determines, in a simple way, results of interactions between solid and liquid phases in soils, and thus provides possibility to classify them in groups with similar mechanic properties. In most cases, the results of these investigations provide a good basis for predicting other properties such as deformability, expansion, hydraulic conductivity and strength of soils. This proves that basis factors influencing the values of consistency limits and other mechanic properties are the same. It is known that the values of consistency limits primarily depend on the type and quantity of clay minerals in soils. The article focuses on experimental evidence of dependence between the quantity of water at the liquid limit for soils and type, portion and specific surface of clay grains. Experiments were performed with monomineral soils, their mixtures and composed samples of clay- and non-clay components. It was established that in parallel orientation of clay particles the quantity of water between grains at liquid limit is dependent on their external specific surface. mehanika zemljin mineralogija konsistenčne meje lastnosti zemljin soil mechanics mineralogy consistency limits soil properties true false true Slovenski jezik Angleški jezik Znanstveno delo 2015-07-10 19:23:53 2015-07-10 19:23:53 2022-06-02 03:09:06 2021-05-10 03:34:21 2002 0 0 str. 347-352 št. 2 Letn. 45 2002 0000-00-00 Zaloznikova Objavljeno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 0016-7789 624.131:549 5636866 7750934 10.5474/geologija.2002.031 0016-7789 URN:SI:UM:DK:GRSVVWMY Geologija_2002_Dolinar_Vloga_mineralogije_v_mehaniki_zemljin.pdf Geologija_2002_Dolinar_Vloga_mineralogije_v_mehaniki_zemljin.pdf 1 459A9989A395FAF560D0FD8957B0A19C 18c9d61f4f9ef8a9ba508f6dae738508a9b858739ed001c4b01d9ca264d778f7 71f3e896-7c0e-11eb-bb7a-00155d0001ca https://dk.um.si/Dokument.php?lang=slv&id=114486 http://www.geologija-revija.si/dokument.aspx?id=629 1 https://dk.um.si/Dokument.php?lang=slv&id=77683 Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo 0 0 0