Investigation of the Sand Porosity via Oedometric Testing

Investigation of the porosity of Klaipėda sand by oedometric test is presented. The Klaipėda sand is typical Baltic see-shore sand consisting of grains the average diameter of which varies from 1.18 mm to 0.3 mm. Variation of the porosity during oedometric compression of the whole mixture of the san...

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Main Authors: Jonas Amšiejus, Rimantas Kačianauskas, Arnoldas Norkus, Liudas Tumonis
Format: Article
Language:English
Published: RTU Press 2010-09-01
Series:The Baltic Journal of Road and Bridge Engineering
Subjects:
Online Access:https://bjrbe-journals.rtu.lv/article/view/3788
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spelling doaj-fda7d98650da4df7b4a39ca9a8c5b45a2020-11-25T03:46:34ZengRTU PressThe Baltic Journal of Road and Bridge Engineering1822-427X1822-42882010-09-015313914710.3846/bjrbe.2010.202118Investigation of the Sand Porosity via Oedometric TestingJonas Amšiejus0Rimantas Kačianauskas1Arnoldas Norkus2Liudas Tumonis3Dept of Geotechnical Engineering, Vilnius Gediminas Technical University, Saulėtekio al. 11, 10223 Vilnius, LithuaniaDept of Strength of Materials, Vilnius Gediminas Technical University, Saulėtekio al.11, 10223 Vilnius, LithuaniaDept of Geotechnical Engineering, Vilnius Gediminas Technical University, Saulėtekio al. 11, 10223 Vilnius, LithuaniaDept of Geotechnical Engineering, Vilnius Gediminas Technical University, Saulėtekio al. 11, 10223 Vilnius, LithuaniaInvestigation of the porosity of Klaipėda sand by oedometric test is presented. The Klaipėda sand is typical Baltic see-shore sand consisting of grains the average diameter of which varies from 1.18 mm to 0.3 mm. Variation of the porosity during oedometric compression of the whole mixture of the sand and of three separate fractions were investigated experimentally. Porosity was characterised by the maximal (initial) and minimal (after compression) values of the void ratio. It was proved experimentally that porosity of the sand mixture is practically predicted by the coarse-grained fraction with grain diameters ranging between 1.18 mm and 0.6 mm. The role of microstucture in the densification mechanism is explained by employing the discrete element method simulations. The spherical particles and commercial EDEM code were used for modelling purposes. Discrete element method simulations confirmed generally the macroscopic experimental results and yielded additional data on microscopic behaviour. The non-smooth deformation behaviour was observed during detailed numerical time-history analysis. The detected instabilities are explained by rearrangement of the sand grains.https://bjrbe-journals.rtu.lv/article/view/3788sandoedometer testvoid ratiodiscrete element method (dem)spherical particles
collection DOAJ
language English
format Article
sources DOAJ
author Jonas Amšiejus
Rimantas Kačianauskas
Arnoldas Norkus
Liudas Tumonis
spellingShingle Jonas Amšiejus
Rimantas Kačianauskas
Arnoldas Norkus
Liudas Tumonis
Investigation of the Sand Porosity via Oedometric Testing
The Baltic Journal of Road and Bridge Engineering
sand
oedometer test
void ratio
discrete element method (dem)
spherical particles
author_facet Jonas Amšiejus
Rimantas Kačianauskas
Arnoldas Norkus
Liudas Tumonis
author_sort Jonas Amšiejus
title Investigation of the Sand Porosity via Oedometric Testing
title_short Investigation of the Sand Porosity via Oedometric Testing
title_full Investigation of the Sand Porosity via Oedometric Testing
title_fullStr Investigation of the Sand Porosity via Oedometric Testing
title_full_unstemmed Investigation of the Sand Porosity via Oedometric Testing
title_sort investigation of the sand porosity via oedometric testing
publisher RTU Press
series The Baltic Journal of Road and Bridge Engineering
issn 1822-427X
1822-4288
publishDate 2010-09-01
description Investigation of the porosity of Klaipėda sand by oedometric test is presented. The Klaipėda sand is typical Baltic see-shore sand consisting of grains the average diameter of which varies from 1.18 mm to 0.3 mm. Variation of the porosity during oedometric compression of the whole mixture of the sand and of three separate fractions were investigated experimentally. Porosity was characterised by the maximal (initial) and minimal (after compression) values of the void ratio. It was proved experimentally that porosity of the sand mixture is practically predicted by the coarse-grained fraction with grain diameters ranging between 1.18 mm and 0.6 mm. The role of microstucture in the densification mechanism is explained by employing the discrete element method simulations. The spherical particles and commercial EDEM code were used for modelling purposes. Discrete element method simulations confirmed generally the macroscopic experimental results and yielded additional data on microscopic behaviour. The non-smooth deformation behaviour was observed during detailed numerical time-history analysis. The detected instabilities are explained by rearrangement of the sand grains.
topic sand
oedometer test
void ratio
discrete element method (dem)
spherical particles
url https://bjrbe-journals.rtu.lv/article/view/3788
work_keys_str_mv AT jonasamsiejus investigationofthesandporosityviaoedometrictesting
AT rimantaskacianauskas investigationofthesandporosityviaoedometrictesting
AT arnoldasnorkus investigationofthesandporosityviaoedometrictesting
AT liudastumonis investigationofthesandporosityviaoedometrictesting
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