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Title:The influence of porosity on geomechanical characteristics of snail soil in the Ljubljana Marsh
Authors:ID Žlender, Bojan (Author)
ID Trauner, Ludvik (Author)
ID Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo Univerze v Mariboru (Copyright holder)
Files:.pdf Acta_geotechnica_Slovenica_2006_Zlender,_Trauner_The_influence_of_porosity_on_geomechanical_characteristics_of_snail_soil_in_the_Ljublja.pdf (486,06 KB)
MD5: 689A1447E20F2E38D96CE70206864EB4
PID: 20.500.12556/dkum/43d2a82f-9250-40e9-9071-c44e9783712d
 
URL http://fgserver3.fg.um.si/journal-ags/2006-2/article-3.asp
 
Language:English
Work type:Scientific work
Typology:1.01 - Original Scientific Article
Organization:FGPA - Faculty of Civil Engineering, Transportation Engineering and Architecture
Abstract:This article focusses on mineralogical and physical characteristics of snail soil and their influence on parameter values of geomechanical characteristics.Snail soil, which got its name from fossil remains, is a typical layer observed in the Ljubljana marsh. It is distincltly porous, saturated and in a liquid consistency state. Snail soil was investigated for mineralogical and physical characteristics in the Laboratory of Soil Mechanics, Faculty of Civil Engineering of the University in Maribor. Mineral and chemical composition, visual appearance, specific surface and grain property were determined. Physical characyteristics show that snail soil is saturated in nature, highly porous and almost liquid. Geomechanical characteristics were investigated for their interdependency on physical characteristics. A series of triaxial tests were performed on snail soil samples of different porosity, density and water content. Cylindrical samples of the height of 100 mm and the diameter of 50 mm were tested using three-axial testing apparatus. The results of the tests show that interdependency exists between geomechanical characteristics and porosity. These relationships can be expressed as functions of density, porosity or water content. It is evident from the results that changes of the coefficient of permeability, the coefficient of consolidation, and the coefficient of volume compressibility are nonlinear with respect to changes in porosity. Changes of mechanical parameters, such as Young`s modulus, Poisson`s ratio andfriction angle are indistinct and almost linear at lower changes of porosity.
Keywords:geomechanics, properties of soils, snail soil, triaxial testing, porosity, permeability, consolidation, Young`s modulus, Poisson`s ratio, shear angle
Publication status:Published
Publication version:Version of Record
Year of publishing:2006
Number of pages:str. 35-42
Numbering:Letn. 3, št. 2
PID:20.500.12556/DKUM-70508 New window
ISSN:1854-0171
UDC:624.131.3/.4
ISSN on article:1854-0171
COBISS.SI-ID:11078678 New window
NUK URN:URN:SI:UM:DK:U7VNGCLQ
Copyright:Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo Univerze v Mariboru
Publication date in DKUM:17.05.2018
Views:1623
Downloads:87
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Categories:Misc.
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Record is a part of a journal

Title:Acta geotechnica Slovenica
Shortened title:Acta geotech. Slov.
Publisher:Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo Univerze v Mariboru
ISSN:1854-0171
COBISS.SI-ID:215987712 New window

Secondary language

Language:Slovenian
Title:Vpliv poroznosti na geomehanske lastnosti polžarice iz Ljubljanskega barja
Abstract:Prispevek obravnava mineraloške in fizikalne lastnosti polžarice in njihov vpliv na vrednosti parametrov geomehanskih lastnosti. Polžarica, ime je dobila po vsebovanih fosilih, je tipični sloj Ljubljanskega barja. Je izrazito porozna, zasičena in se nahaja v židkem konsistentnem stanju. V Laboratoriju za mehaniko tal (LMT), Fakultete za gradbeništvo, Univerze v Mariboru je bila izvedena raziskava polžarice s preiskavo mineraloških in fizikalnih lastnosti. Za raziskavo je bil odvzet niz vzorcev na jugozahodni lokaciji Ljubljanskega barja. V Centru za elektronsko mikroskopijo Fakultete za strojništvo, Univerze v Mariboru sta bila raziskana kemična sestava in optični izgled. Kemična sestava je bila določena z visokoločljivim vrstičnim elektronskim mikroskopom SIRION. Optični izgled treh vzorcev polžarice je bil preiskan z okoljskim vrstičnim elektronskim mikroskopom QUANTA 200 3D. Mineralna sestava in zrnatost polžarice sta bila določena na Geološkem zavodu Slovenije. Mineralna sestava je bila določena z rentgenskim difraktometrom. Zrnatost polžarice je bila določena s pomočjo laserskega analizatorja Fritsch particle sizer analysette 22. Specifična površina je bila določena na Kemijskem inštitutu Slovenije, s pettočkovno BET metodo, za meritve je bil uporabljen avtomatski plinski adsorbcijski analizator TriStar 3000, proizvajalca Micromeritics Instrument Corporation, Norcross, ZDA. Ostale fizikalne lastnosti polžarice so bile določene v LMT. Raziskane fizikalne lastnosti kažejo, da je polžarica v naravi zasičena, zelo porozna in skoraj tekoča meljna zemljina. Preiskava stisljivosti kaže, da je polžarica izrazito stisljiva, volumenske spremembe so velike že ob malih spremembah napetosti. Parametri trdnosti imajo značilno nizke vrednosti, ki se ujemajo s predhodnimi raziskavami. Raziskava geomehanskih lastnosti je bila izvedena s poudarkom na sovisnosti fizikalnih lastnosti. Izveden je bil niz triosnih preizkusov polžarice različne gostote oz. vlažnosti in poroznosti. Preizkusi so bili izvedeni v triosnih aparatih na valjastih preizkušancih višine 100 mm in premera 50 mm. Rezultati raziskave kažejo na sovisnost geomehanskih lastnosti in poroznosti. Odnose lahko izrazimo kot funkcije gostote oz. poroznosti ali vlažnosti. Iz rezultatov je razvidno, da so spremembe vodoprepustnosti, konsolidacije in stisljivosti nelinearno odvisne od sprememb poroznosti. Spremembe mehanskih parametrov kot so elastični modul, Poissonov količnik in strižni kot, so pri manjših spremembah poroznosti neizrazite in skoraj linearne.
Keywords:geomehanika, lastnosti tal, polžarica, triosni preizkus, poroznost, vodoprepustnost, konsolidacija, Youngov modul, Poissonov količnik, strižni kot


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