Abstract
The compressibility factor (z-factor) of gases is a thermodynamic property used to account for the deviation of real gas behavior from that of an ideal gas. Correlations based on the equation of state are often implicit, because they require iteration and are computationally expensive. A number of explicit correlations have been derived to enhance simplicity; however, no single explicit correlation has been developed for the full range of pseudo-reduced temperatures $$\left( {1.05 \le T_{pr} \le 3} \right)$$ and pseudo-reduced pressures $$\left( {0.2 \le P_{pr} \le 15} \right)$$ , which represents a significant research gap. This work presents a new z-factor correlation that can be expressed in linear form. On the basis of Hall and Yarborough’s implicit correlation, we developed the new correlation from 5346 experimental data points extracted from 5940 data points published in the SPE natural gas reservoir engineering textbook and created a linear z-factor chart for a full range of pseudo-reduced temperatures $$(1.15 \le T_{pr} \le 3)$$ and pseudo-reduced pressures $$(0.2 \le P_{pr} \le 15)$$ .
Highlights
The compressibility factor (z-factor) of gases is used to correct the volume of gas estimated from the ideal gas equation to the actual value
On the basis of Hall and Yarborough’s implicit correlation, we developed the new correlation from 5346 experimental data points extracted from 5940 data points published in the SPE natural gas reservoir engineering textbook and created a linear z-factor chart for a full range of pseudo-reduced temperatures ð1:15 Tpr 3Þ and pseudo-reduced pressures ð0:2 Ppr 15Þ
The cross plots show that the plotted points fall on the unit slope line through the origin, which implies that the new correlation reproduces the measured values to a considerable degree of accuracy
Summary
The compressibility factor (z-factor) of gases is used to correct the volume of gas estimated from the ideal gas equation to the actual value It is required in all calculations involving natural gases. Z 1⁄4 0:27Ppr ; ð8Þ yTpr where y is the root of the following equation:
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