Water flows through a 30 mm i.d. pipe at atmospheric pressure. The velocity of water at the center of the pipe is measured by a pitot tube as shown in Figure. The pressure difference between the impact tube and the static tube is 20 cm of Carbon tetra chloride (density 1600 kg/m³). Calculate the volumetric flow rate through the pipe in cubic meter per hour. Viscosity of water is 1 cP. Water Reading = h X- X' CCI4

Introduction to Chemical Engineering Thermodynamics
8th Edition
ISBN:9781259696527
Author:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Publisher:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Chapter1: Introduction
Section: Chapter Questions
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Water flows through a 30 mm i.d. pipe at atmospheric
pressure. The velocity of water at the center of the pipe is
measured by a pitot tube as shown in Figure. The pressure
difference between the impact tube and the static tube is 20
cm of Carbon tetra chloride (density 1600 kg/m³). Calculate
the volumetric flow rate through the pipe in cubic meter per
hour. Viscosity of water is 1 cP.
Water
Reading = h
X-
X'
CCl4
Transcribed Image Text:Water flows through a 30 mm i.d. pipe at atmospheric pressure. The velocity of water at the center of the pipe is measured by a pitot tube as shown in Figure. The pressure difference between the impact tube and the static tube is 20 cm of Carbon tetra chloride (density 1600 kg/m³). Calculate the volumetric flow rate through the pipe in cubic meter per hour. Viscosity of water is 1 cP. Water Reading = h X- X' CCl4
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