Consider a similar case but liquid depth in tank (C) is twice that of tank (A) previously shown For the same fluid in bo

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Consider a similar case but liquid depth in tank (C) is twice that of tank (A) previously shown For the same fluid in bo

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Consider A Similar Case But Liquid Depth In Tank C Is Twice That Of Tank A Previously Shown For The Same Fluid In Bo 1
Consider A Similar Case But Liquid Depth In Tank C Is Twice That Of Tank A Previously Shown For The Same Fluid In Bo 1 (37.11 KiB) Viewed 43 times
Consider a similar case but liquid depth in tank (C) is twice that of tank (A) previously shown For the same fluid in both cases and the fluid height ratio ( hc/ha) - 2. Given: Pa = pc and An Ac 1.14) The solution for the ratio (Vove/Wave) { 2 }*. With R= 2 D2) The solution for the ratio (nis et, damit deta) = (2), with S - 2 P=pgh P=2P ✓ 2 V zū + г. Р Р V, 2 m-PAU 912, 2) Flow Area, Ac = A 2+2=U² he ſ4=2 EXTRA CREDIT Consider changes in absolute pressure and density in the lower part of Earth's stratosphere. At elevations above sea level from z = 10,000 m to z = 20,000 m the absolute temperature remains constant. The air acts like a perfect gas under these conditions so pressure and density are related by Pane = PRT. Note: For a perfect gas with constant temperature the ratio (ppi) + (palp:) Set up a relationship for the variation of pressure with elevation (x) based on the hydrostatic equation dp = - Pgdz Letz: = 10000 mand 2. - 20000 m so the ratio (zzz:) = 2. 4) Set up and solve for the ratio (pulpa) = some function of the ratio ( zszx) = With (za/zı) = 2.0, then the numerical value for (pap) Show you work P=PgAz P9 Write out basic equations in symbolic form to receive full or partial credit for your solution.
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