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Title:Vloga mineralogije v mehaniki zemljin
Authors:ID Dolinar, Bojana (Author)
Files:.pdf Geologija_2002_Dolinar_Vloga_mineralogije_v_mehaniki_zemljin.pdf (637,85 KB)
MD5: 459A9989A395FAF560D0FD8957B0A19C
 
URL http://www.geologija-revija.si/dokument.aspx?id=629
 
Language:Slovenian
Work type:Scientific work
Typology:1.01 - Original Scientific Article
Organization:FGPA - Faculty of Civil Engineering, Transportation Engineering and Architecture
Abstract: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.
Keywords:mehanika zemljin, mineralogija, konsistenčne meje, lastnosti zemljin
Publication status:Published
Publication version:Version of Record
Year of publishing:2002
Number of pages:str. 347-352
Numbering:Letn. 45, št. 2
PID:20.500.12556/DKUM-53123 New window
ISSN:0016-7789
UDC:624.131:549
ISSN on article:0016-7789
COBISS.SI-ID:7750934 New window
DOI:10.5474/geologija.2002.031 New window
NUK URN:URN:SI:UM:DK:GRSVVWMY
Publication date in DKUM:10.07.2015
Views:1554
Downloads:265
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Categories:Misc.
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Record is a part of a journal

Title:Geologija
Publisher:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 New window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.
Licensing start date:10.07.2015

Secondary language

Language:English
Title:Significance of mineralogy in soil mechanics
Abstract: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.
Keywords:soil mechanics, mineralogy, consistency limits, soil properties


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