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Consequently, the stress fluctuation did not propagate.
The k-ω model is used to simulate the bed stress fluctuation under random waves.
Therefore, most microseismic events in Mqs2 appear to be triggered by stress fluctuation.
However, we should note that the stress fluctuation was ~ 1 MPa at most.
The saturated water in the fracture zone could be a mediator for the stress fluctuation.
However, the mechanism for the transfer of the stress fluctuation from the Test Well to Mqs2 is still unclear.
Similar(45)
Mqs2 may have been triggered by the water flow and the stress fluctuations resulting from changes in the injection rate.
These modeling results suggest that the stress fluctuations found in this study may be associated with active faults.
The critical stress fluctuations associated with the Portevin-Le Chaˆtelier effect (serrated yielding) are discussed.
Both types of internal stress fluctuations acted to enhance cyclic creep.
Local heterogeneity in the amorphous phase (stress fluctuations and states) is analyzed.
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