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2. The New York Waterway boat to Hoboken can be modeled as a rectangular box of length, L, width, W, and height, H: 9f = 2*t MY Waterway L H It begins to rain at noon, and the volume of rain flow increases linearly with time, qr=2*t. There is no effluent flow, qe = 0. The constant density is given by p.

2. The New York Waterway boat to Hoboken can be modeled as a rectangular box of length, L, width, W, and height, H: 9f = 2*t MY Waterway L H It begins to rain at noon, and the volume of rain flow increases linearly with time, qr=2*t. There is no effluent flow, qe = 0. The constant density is given by p.

Introduction to Chemical Engineering Thermodynamics
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
Problem 1.1P
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a) show the mass balance for the boat. d(mass)/dt

b)what are the dimensions of Ω?

c)Derive the height as a function of time (h(t)=?) assuming that the initial height is h=0.

sketch the height as a function of time.

2. The New York Waterway boat to Hoboken can be modeled as a rectangular box of length, L, width, W, and height, H: 9f=22*t ph.h It begins to rain at noon, and the volume of rain flow increases linearly with time, qr=22*t. There is no effluent flow, qe = 0. The constant density is given by p. MY Waterway H L W
Transcribed Image Text:2. The New York Waterway boat to Hoboken can be modeled as a rectangular box of length, L, width, W, and height, H: 9f=22*t ph.h It begins to rain at noon, and the volume of rain flow increases linearly with time, qr=22*t. There is no effluent flow, qe = 0. The constant density is given by p. MY Waterway H L W
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