dc.contributor.author |
Guo, R |
|
dc.contributor.author |
Hueckel, T |
|
dc.date.accessioned |
2015-10-20T17:20:22Z |
|
dc.date.issued |
2015-01-01 |
|
dc.identifier.uri |
https://hdl.handle.net/10161/10760 |
|
dc.description.abstract |
© 2015 Elsevier Ltd. All rights reserved.Laboratory tests on microscale are reported
in which millimeter-sized amorphous silica cubes were kept highly compressed in a
liquid environment of de-ionized water solutions with different silica ion concentrations
for up to four weeks. Such an arrangement simulates an early evolution of bonds between
two sand grains stressed in situ. In-house designed Grain Indenter-Puller apparatus
allowed measuring strength of such contacts after 3-4 weeks. Observations reported
for the first time confirm a long-existing hypothesis that a stressed contact with
microcracks generates silica polymers, forming a bonding structure between the grains
on a timescale in the order of a few weeks. Such structure exhibits intergranular
tensile force at failure of 1-1.5 mN when aged in solutions containing silica ion
concentrations of 200-to 500-ppm. The magnitude of such intergranular force is 2-3
times greater than that of water capillary force between the same grains.
|
|
dc.publisher |
Elsevier BV |
|
dc.relation.ispartof |
Geomechanics for Energy and the Environment |
|
dc.relation.isversionof |
10.1016/j.gete.2015.02.002 |
|
dc.title |
Silica polymer bonding of stressed silica grains: An early growth of intergranular
tensile strength
|
|
dc.type |
Journal article |
|
duke.contributor.id |
Hueckel, T|0111038 |
|
pubs.begin-page |
48 |
|
pubs.end-page |
59 |
|
pubs.organisational-group |
Civil and Environmental Engineering |
|
pubs.organisational-group |
Duke |
|
pubs.organisational-group |
Pratt School of Engineering |
|
pubs.publication-status |
Published |
|
pubs.volume |
1 |
|
dc.identifier.eissn |
2352-3808 |
|