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This paper identifies distinctive regimes for the combustion of particles in a packed bed.
The oxidation of carbon monoxide occurred in two distinctive regimes, a high-activity regime and a low-activity regime, which have high and low rates of reaction respectively.
Regardless of the particle size, the CO oxidation occurred in two distinctive regimes, a high-activity regime and a low-activity regime, which have high and low rates of reaction respectively, as observed in previous studies.
Depending on the control of deposition amount ranging between 0.5 and 100 nm at various annealing temperatures, four distinctive regimes of Pd nanostructures are demonstrated: (i) small pits and grain formation, (ii) nucleation and growth of NPs, (iii) lateral evolution of NPs, and (iv) merged nanostructures.
In general, the local stress keeps increasing before creep relaxation overwhelms the consequences of growth strains, and there are two distinctive regimes separated by an extreme point corresponding to the maximum stress value and transition time in the stress variation curve.
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For such a distinctive regime to exist, stresses associated with mantle convection have to exceed the strength of the rigid lithosphere, which may happen with weakening of the lithosphere.
Yet while much has been promised, Europe, America, Switzerland and other financial centers are today regrettably agreeing to their own separate and distinctive financial regimes.
Six distinctive impact regimes were identified and classified for binary and single component droplets' cases.
The plasma nitrided AISI 1045 steel exhibited three distinctive wear regimes, with an intermediate stage characterised by a low cavitation erosion rate (2.0 mg h− 1) between the incubation period (first regime) and accelerated stage (third regime); this intermediate regime could be associated with the wear of the nitrided layer.
Based on the control of initial film thickness between 2 and 200 nm at 500 °C of annealing, three distinctive growth regimes of Ag nanostructures were observed: Specifically, the tiny to the enlarged dome-shaped Ag NPs between 2 and 20 nm, the merged and irregular nanoclusters between 30 and 60 nm, and the Ag nanoclusters network between 80 and 200 nm.
The associated disturbances along these faults have given rise to a distinctive fluvial regime and geomorphology in the region.
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