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In upper layer, the demand clutch torque can be calculated by a robust H∞controller considering the clutch engaging time and the vehicle jerk.
These two waveguides in upper layer do not cross each other but instead each twice cross over the waveguide in the lower layer.
However, comprehensive heat transfer performance of structure P2 (i.e., parallel flow with rectangular channels in upper layer and complex channels in bottom layer) shows the best from the viewpoint of thermodynamics.
Formulations were initially developed for theophylline and the release was optimized by using two different soluble forms of theophylline with varying amount of hydrophilic polymer mixture in upper layer and polyethylene oxide (expandable hydrogel) in lower layer.
Furthermore, heat dissipation and pressure drop of structure 2 are both better and lower than that of structure 1. Form the viewpoint of temperature distribution, structure C2 (i.e., counter flow with rectangular channels in upper layer and complex channels in bottom layer) presents the most uniform bottom temperature for microelectronic cooling.
It is found that, no matter whether a background parabolic current is considered or not, the maximum force lies at the depth of turning point (where the horizontal current in upper layer begins to turn to zero and flow against that in lower layer), a negative extremum torque appears at the depth of turning point, and the maximum torque appears at the bottom of tendon leg.
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Water mass movements and entrainment of deep waters in upper layers can occur over steep or highly variable topography.
Activation of pyramidal neurons in upper layers has been proposed to underlie the emergence of network oscillations in beta gamma frequency range in the neonatal PL8.
Alternatively, the continuing development of other deep layers in skin (for instance, subcutaneous tissues) that expands their volume may also provide stress in upper layers, such as the dermis.
We analysed pollen, plant macrofossils (more abundant in bottom layers), testate amoebae (more abundant in upper layers), peat stratigraphy and chemistry.
The drought caused by the downward transport of soil moisture in upper layers altered the allocation of plant belowground biomass at various soil depths.
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