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Density atmospheric distillation unit

The first step in the building the atmospheric distillation unit is entering the composition of the crude in order to generate the necessary hypothetical components for model. For the purposes of this simulation, we will consider the crude assays given in Table 2.5 to Table 2.8. It is important to remember that that we may have to remove extraneous details from the distillation curve to avoid unusual column behavior. We use the TB P distillation, density distribution and overall bulk density to define this system in Figure 2.14. [Pg.75]

Pahr and tbo barometer at 30 inches. In the United States, the Winchester bushel of 2150.42 inches has been generally odo ted. which holds 77.627413 pounds of distilled water at 39.83 Fahr., the temperature of its maximum density, and 30 inches barometric pressure. In New York the bushel is declared to contain 80 pounds distilled water at its maximum density, under the mean pressure of the atmosphere at the level of the sea. This would make the New York bushel contain 2216.128 cubic inches, somewhat less than the Imperial bushel, owing to the different standard of temperature of the water. The small measure" used in the morketa should contain 2 quarts, or i peck. [Pg.340]


See other pages where Density atmospheric distillation unit is mentioned: [Pg.371]    [Pg.629]    [Pg.243]    [Pg.481]    [Pg.673]    [Pg.665]    [Pg.716]    [Pg.481]    [Pg.652]    [Pg.722]    [Pg.665]   
See also in sourсe #XX -- [ Pg.66 , Pg.71 , Pg.75 , Pg.91 , Pg.92 , Pg.93 , Pg.94 ]




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