Four mesophase powders, A, B, C, and D, are studied. A is petroleum de
rived, B, C, and D are commercialized powders and are coal-tar derived
. No additives are recognized in A, which is almost devoid of cross-li
nking oxygen. In B, a thin deposit (approximately 100 nm) of a phase,
which appears isotropic in transmission electron microscope (TEM), sur
rounds the spheres and the primary quinoline insoluble (QI). C and D a
re increasingly altered. The altered areas of C surround a core of res
idual mesophase sphere with a thickness up to 1 mum. D, the powder ric
her in oxygen, is entirely altered. By aging, B becomes similar to C,
whereas C is transformed in a matrix of alteration, including relics o
f spheres. After carbonization and heat treatment (HT) at 2800-degrees
-C, A is entirely lamellar and strongly graphitized. B, C, and D conta
in a decreasing amount of lamellae and an increasing amount of pores o
f decreasing size. They have a decreasing ability to graphitize. The i
ncreasing alteration is assumed to be due to the occurrence of adsorbe
d heavy solvents. They act as dispersing agents on the basic structura
l units (BSU). Correspondingly, mesophase spheres regress down to loca
l molecular orientations (LMO), which decrease in size as solvent alte
ration progresses.