By Victoria M. Petrova
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Additional resources for Advances in Engineering Research
J. Atmos. Sci. 1974, 31, 1324-1333. Monin, A. S. The atmospheric boundary layer. Annu. Rev. Fluid Mech. 1970, 2, 225-250. Morton, B. R. The ascent of turbulent forced plumes in a calm atmosphere. Int. J. Air Poll. 1959, 1, 184-197. Nieuwstadt, F. T. M. The steady-state height and resistance laws of the nocturnal boundary layer: theory compared with Cabauw observations. -Lay. Meteorol. 1981, 20, 317. Nieuwstadt, F. T. M. Some aspects of the turbulent stable boundary layer. -Lay. Meteorol. 1984, 30, 31-55.
The bed thermal conductivity was increased 88 times that of granular packed bed and its cooling power was doubled. Fragmentation in the consolidated block was observed during strength test. W. et al. G. et al. G. et al. 2003. That adsorbent bed was produced based on the steps of; (1) mixing the adsorbent granules with pitch binder and water (2) compression moulding the mixture (3) heating up the adsorbent block to 120°C for three hours. 5 times of the granular packed bed. 9 times of granular packed bed respectively.
Clim. 2007, 46, 212-225. Stull, R. B. A heat-flux history length scale for the nocturnal boundary layer. Tellus. 1983, 35A, 219-230. Stull, R. B. 1988. An introduction to boundary layer meteorology. Kluwer Academic Publishers: Norwell, MA, 666 p. , Mahrt, L. A simple model of the atmospheric boundary layer: sensitivity to surface evaporation. -Lay. Meteorol. 1986, 37, 129–148. United States Environmental Protection Agency (EPA). 0-A Relief Value Discharge Screening Model, EPA-450/4-88-024, 1989, 62 pp.
Advances in Engineering Research by Victoria M. Petrova