The variation of fluid pressure with height is described by the differential equation: dP =-pg dz Here, p is specific density and g is the local acceleration of gravity. For an ideal gas, p = MP/RT, where M is molar mass and R is the universal gas constant. Modeling the atmosphere as an isothermal column of ideal gas at 283.15 K (10°C), estimate the ambient pressure in Denver, where z = 1(mile) relative to sea level. For air, take M = 29 g mol; values of R are given in App. A.

Introduction to Chemical Engineering Thermodynamics
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ISBN:9781259696527
Author:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
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Chapter1: Introduction
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The variation of fluid pressure with height is described by the differential equation:
dP
=-pg
dz
Here, p is specific density and g is the local acceleration of gravity. For an ideal gas,
p = MP/RT, where M is molar mass and R is the universal gas constant. Modeling
the atmosphere as an isothermal column of ideal gas at 283.15 K (10°C), estimate
the ambient pressure in Denver, where z = 1(mile) relative to sea level. For air, take
M = 29 g mol; values of R are given in App. A.
Transcribed Image Text:The variation of fluid pressure with height is described by the differential equation: dP =-pg dz Here, p is specific density and g is the local acceleration of gravity. For an ideal gas, p = MP/RT, where M is molar mass and R is the universal gas constant. Modeling the atmosphere as an isothermal column of ideal gas at 283.15 K (10°C), estimate the ambient pressure in Denver, where z = 1(mile) relative to sea level. For air, take M = 29 g mol; values of R are given in App. A.
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