The operation of natural gas transmission systems, today as in the past, has everything to do with line pack management. Professor Weymouth gives a good account of this subject in his paper.
By the way, the 2/3 factor was not derived by professor Weymouth. It is the result of constants of integration in deriving the average pressure equation used today. It is important to note that the assumed pipeline conditions were pressures below 1000 psia and temperatures of 60° F or higher.
Below is the derivation of the average pressure equation per Uhl, A. E., et al., Steady Flow in Gas Pipelines, Technical Report No. 10, Institute of Gas Technology, Chicago, 1965, pages 85 and 86.
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For the operating ranges usually encountered in transmission practice; i. e., pressures below 1000 psia and temperatures of 60° F or higher, the variation of z with P is nearly linear, so that the compressibility factor may be represented by a function of the form
Z=1/(1+aP)
where a is a Constant dependent on T. The mean pressure (Pm) which must be used can be determined as follows:
[tt]
P2 P2
(1/Zavg)[∫] PdP = [∫] (P/Z)dP
P1 P1
or
P2 P2
(1+aPm)[∫]PdP = [∫]P(1+aP)dP
P1 P1
[/tt]
Upon integration
(1+aPm)(P12 - P22)/2 = (P12 - P22)/2 + a(P13 - P23)/3
or
Pm = 2/3(P13- P23)/( P12 - P22)
If full integration of the general energy balance is desired, however, for the sake of extreme accuracy or where a computer program is involved, the variation of P and T and the consequent variation of z along the line can be accounted for by graphical or numerical techniques. Graphical integration could be effected by plotting P/ZT against P, and subsequently determining the area under the curve between the initial and terminal values of P. An additional possibility would involve the use of an analytical or virial equation of state.
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