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data, the peculiar behavior of data points would be regarded
merely as an extensive scatter. However, comparison with the lar-
ger database of Figs. 6 and 7 allows attributing peaks of specific
gravity to the same asphaltene phase boundaries (boundary 3b is
not reproduced due to the lack of data points in the respective con-
centration range).
Fig. 7. Complex variations of specific gravity with asphaltene content for world’s
(dead) crudes. Apparent extrema are numbered in accordance with asphaltene
phase boundaries in Fig. 5.
Fig. 8. Complex variations of specific gravity with asphaltene content
in the limited collection of world’s (dead) crudes.
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