A peek into the origin of creep in sand
Artikel i vetenskaplig tidskrift, 2019

This paper presents the results of an experimental study of the particle scale mechanisms that underpin creep, on-going deformations under constant external load, in dry non-cemented sand under 1D oedometric compression loading at 2500kPa. Traditional observations on the boundary of the sample are complemented with simultaneous measurements of the 3D kinematics of both the entire grain assembly and details of grain-scale mechanisms using synchrotron based X-ray tomography at two different spatial resolutions. Both the continuum response and the local grain scale response are captured using two spatial resolutions, i.e.6.and 0.65m respectively. The results, for the first time, illustrate that small displacements measured at the boundary can be the result of rather pronounced fracturing at the individual grain scale.

X-ray tomography

Sand

Micro-mechanics

Creep

Författare

Edward Ando

Université Grenoble Alpes

Jelke Dijkstra

Chalmers, Arkitektur och samhällsbyggnadsteknik, Geologi och geoteknik

Emmanuel Roubin

Université Grenoble Alpes

Christophe Dano

Université Grenoble Alpes

Elodie Boller

European Synchrotron Radiation Facility (ESRF)

Granular Matter

1434-5021 (ISSN) 1434-7636 (eISSN)

Vol. 21 1 11

Ämneskategorier

Teknisk mekanik

Keramteknik

Annan materialteknik

DOI

10.1007/s10035-018-0863-5

Mer information

Senast uppdaterat

2019-02-07