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For the analysis of the differential cell migration capacity of SCC38, SCC40, and SCC42B cells, the rate of front migration of cell monolayers was analyzed in an AxioObserver.Z1 microscope (Zeiss), equipped with an incubation module, by taking pictures at 0 h and 8 h using an EC Plan-Neofluor 10x/0.30 Ph1 objective.
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The analytical reaction diffusion model presented here allows to predict the propagation rate of fronts spreading through Peano-like basins, and comparison with the Optimal Channels Network model is also reported.
To determine whether the rate of front-head binding at the binding gate depends upon NL length, we performed run-length measurements as a function of load for constructs with extended NLs.
From these numbers, it follows that the 26-pN inter-head tension in WT kinesin can enhance the rate of front-head release at the unbinding gate by a factor of ∼50.
To quantify the rate of front-head detachment, we examined the unbinding of DmK-WT from the MT under load in the presence of saturating levels of ATP (2 mM).
Having determined values for the inter-head tension and the force-dependent rate of rear-head release (Table 2), it is also necessary to quantify the force-dependent rate of front-head release in order to model how inter-head tension affects the unbinding gate.
The heating range, the temperature increment and the movement rate of thermal front will all decline with the increase of hydrate saturation.
As a result of the time-lag, it was possible to determine the rate of movement of the wetting/drying front for the unconsolidated relatively sorted coarse sediments recorded on the site at 7.8 cm/day.
We give approximate asymptotic solutions for the reactant profiles, and the propagation rate of the front.
Also, density increase elevates monotonically the upper-limit temperature of heat waves, broadens the gradient of temperature profiles, as well as changes the rate of the front propagation non-monotonically.
Besides, the shut-off pressure of the saturated silty clay, at which no water flow into or out of the soil sample, is obtained based on the relationship between the critical advance rate of freezing front and the applied pressure.
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