Silica polymer bonding of stressed silica grains: An early growth of intergranular tensile strength
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.
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- 4019 Resources engineering and extractive metallurgy
- 3705 Geology
- 0905 Civil Engineering
- 0403 Geology
Citation
Published In
DOI
EISSN
Publication Date
Volume
Start / End Page
Related Subject Headings
- 4019 Resources engineering and extractive metallurgy
- 3705 Geology
- 0905 Civil Engineering
- 0403 Geology