The isothermal compression
and isobaric expansion of crystalline o-xylene (1,2-dimethylbenzene)
are inconsistent with the
rule of reverse relationship between effects of pressure and temperature
attributed to most crystals in general. On isobaric cooling at ambient
pressure, the o-xylene crystal shrinks, with the
strongest contraction of the unit-cell dimensions a and c, while during isothermal compression at ambient
temperature these are the least compressed directions. This direct
relationship (as opposed to the “inverse relationship”
rule) between the compression and expansion of o-xylene
has been associated with weak directional CH···π
interactions arranging the molecules into a two-dimensional framework
and with its distinct mechanisms of distortions occurring at high
pressure and low temperature. Single crystals of o-xylene were grown in situ in isochoric and isothermal conditions
in a diamond-anvil cell and their structure determined by X-ray diffraction.