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Modern Engineering Thermodynamics

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Summary 51<br />

change in the mass of X due to the reaction”: m GX = m PX = δm X . Then, for a chemical reaction in a closed system, the mass<br />

balance for each of the chemical species present can be written as<br />

m GA = m PA = δm A<br />

m GB = m PB = δm B<br />

m GC = m PC = δm C<br />

m GD = m PD = δm D<br />

If we add these equations together, we get<br />

δm A + δm B + δm C + δm D = m PA + m PB + m PC + m PD<br />

Now, since total mass must be conserved, it follows that<br />

∑m P = m PA + m PB + m PC + m PD = 0<br />

then the previous equation can be written as<br />

δm A + δm B = −δm C − δm D<br />

If we now convert this equation into a molar equation by dividing each mass term by its corresponding species molecular<br />

mass, then this equation becomes the stoichiometric chemical reaction equation n a A + n b B ! n c C + n d D, where<br />

n a = δm A<br />

;<br />

M A<br />

n c = − δm C<br />

M C<br />

n b = δm B<br />

; n d = − δm D<br />

M B M D<br />

and M A , M B , M C ,andM D are the molecular masses of chemical species A, B, C, andD. Consequently, all stoichiometric<br />

chemical reaction equations are just molar mass balances that utilize the conservation of mass law.<br />

SUMMARY 7<br />

In this chapter, we provide the definitions of many of the concepts necessary in the development of thermodynamics.<br />

First, we review the phases of matter and define thermodynamic equilibrium. Then we see that one of the fundamental<br />

elements underlying modern technology is the thermodynamic processes that systems undergo. Next we reexamine and<br />

expand the pressure and temperature scales information given in Chapter 1. The zeroth law of thermodynamics is found<br />

to provide an axiomatic way to develop temperature measurement technology, and the continuum hypothesis is found<br />

to be a useful and valid analysis tool so long as the system’s dimensions are very large compared to those of the<br />

molecules it contains. The balance and conservation concepts round out the chapter with an important discussion of<br />

the form of all the equations used to represent the basic thermodynamic laws in this book.<br />

Some of the more important equations introduced in this chapter are as follows.<br />

1. The equations for the conversion of temperature units, Eqs. (2.1)–(2.4):<br />

Tð°FÞ = 9 Tð°CÞ + 32 = TðRÞ − 459:67<br />

5<br />

Tð°CÞ = 5 ½Tð°FÞ − 32Š = TðKÞ − 273:15<br />

9<br />

TðRÞ = 9 TðKÞ = 1:8TðKÞ = Tð°FÞ + 459:67<br />

5<br />

TðKÞ = 5 TðRÞ<br />

TðRÞ = = Tð°CÞ + 273:15<br />

9 1:8<br />

2. The equation for absolute to gauge pressure conversion:<br />

Absolute pressure = Gauge pressure + Local atmospheric pressure<br />

3. The general balance equations, (2.11) and (2.12), are<br />

7 Well, what do you think of this course so far? Isn’t this a fascinating subject? I know, I know, it is a little vague right now, but it gets better.

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