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Naslov:Vloga mineralogije v mehaniki zemljin
Avtorji:ID Dolinar, Bojana (Avtor)
Datoteke:.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
 
Jezik:Slovenski jezik
Vrsta gradiva:Znanstveno delo
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:FGPA - Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo
Opis: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.
Ključne besede:mehanika zemljin, mineralogija, konsistenčne meje, lastnosti zemljin
Status publikacije:Objavljeno
Verzija publikacije:Objavljena publikacija
Leto izida:2002
Št. strani:str. 347-352
Številčenje:Letn. 45, št. 2
PID:20.500.12556/DKUM-53123 Novo okno
ISSN:0016-7789
UDK:624.131:549
COBISS.SI-ID:7750934 Novo okno
DOI:10.5474/geologija.2002.031 Novo okno
ISSN pri članku:0016-7789
NUK URN:URN:SI:UM:DK:GRSVVWMY
Datum objave v DKUM:10.07.2015
Število ogledov:1340
Število prenosov:214
Metapodatki:XML RDF-CHPDL DC-XML DC-RDF
Področja:Ostalo
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Gradivo je del revije

Naslov:Geologija
Založnik:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 Novo okno

Licence

Licenca:CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.
Začetek licenciranja:10.07.2015

Sekundarni jezik

Jezik:Angleški jezik
Naslov:Significance of mineralogy in soil mechanics
Opis: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.
Ključne besede:soil mechanics, mineralogy, consistency limits, soil properties


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