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However, this transverse flux circulation has uncommon features for an electrotechnical system due to flux paths which are not enclosed in radial planes.
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The energy flux and circulation of materials in the dark deep-sea biosphere have become a research frontier and the focus of attention.
The total RHC change above 14°C declines by −0.5 × 10 J throughout 2010 and 2011, of which RHCT = −0.3 × 10 J is due to changes in the average temperature and RHCV = −0.2 × 10 J due to changes in the volume: a 60 40 split in heat content changes due to air-sea fluxes and circulation changes, respectively.
Meanwhile, the operational control behavior of different parameters is quantified by estimating both the solids circulation flux (SCF) and the gas bypassing flux (GBF).
By varying RC distributor elevation while keeping HEC constant, the circulation flux is also changing and the highest flux is observed at an elevation level of 90 mm.
The final reaction temperature is kept at 240 °C, and circulation flux is kept for 1 h.
The fluidizing air velocity and solid circulation flux were varied in the range of 4 8 m/s and 13 80 kg/m2/s, respectively.
Within the given ranges of gaseous superficial velocity ( U 0 ) and solid circulation flux ((G_{text{s}})), a core-annulus flow mode was observed.
The elevated RC distributor is found to have a little impact on the solid circulation flux as a function of Uf.
In the fully developed region of the downer, the volumetric solids fraction increases with increasing solids circulation flux or decreasing superficial gas velocity U1.
At a given location, increasing the fluidizing velocity resulted in reduced heat transfer coefficient while increasing the solid circulation flux enhanced it.
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