In addition, at 350°C, illite samples show near-neutral to slightly velocity-weakening behaviour, as opposed to mainly velocity-weakening for the illite/quartz mixtures.
Notably, whereas the wet illite/quartz samples showed predominantly velocity-weakening behaviour in Regime 2, the wet illite samples were velocity-neutral to slightly velocity-weakening at 350°C.
Our conclusions are as follows: 1. Wet (near- pure illite gouge shows similar temperature-depenear- puree-regilliteip stability behaviour to that previously found for wet 65/35 illite/quartz gouge, but with near-neutral to showstly velocity-weakening behaviour at 350°C insimilarf velocitemperature-dependent
Wet (near- pure illite gouge shows similar temperature-depenear- puree-regilliteip stability behaviour to that previously found for wet 65/35 illite/quartz gouge, but with near-neutral to showstly velocity-weakening behaviour at 350°C insimilarf velocitemperature-dependent
Under high loading rates, the crack propagates with slightly decreasing velocity, though the maximum crack speed reached up to 20.6% of the Rayleigh wave speed of the tested HSC.
As each half-bubble resides a flow field of a slightly different velocity, the force acting on respective halves is calculated by integrating the defect in kinetic energy and convective potential-rate.
Again, the un-pruned, un-thinned 500 stems ha−1 treatment did not appear to adhere to this trend, yielding on average a slightly lower velocity even than for the 100 stems ha−1 treatment.
Kaneshima and Matsuzawa (2015) confirm the existence of a slightly low velocity region in the uppermost 300 km of the outer core by SmKS phases observed by seismic arrays around the world.
These characteristics are almost the same as those for MTr6 (Fig. 3(a)), with the exception of the slightly lower velocity in the lower crust in the southwestern part of MTr8.
An increase in radiation parameter (R) is found to slightly upturn velocity values close to the sheet because of the flow is accelerated therefore momentum boundary layer thickness is therefore increased strongly after some distance from the wall.
They travel a significantly shorter trajectory (accumulated distance; p = 0.002), and Euclidean distance (the shortest linear distance from the starting point to the end point; p = 0.0001) with a slightly reduced velocity (Fig. 2F).
