Kaolinite intercalates ortho- and para-nitroanilines (oNA and pNA) between
the layers whereas meta-nitroaniline (mNA) is not intercalated. para-Nitroa
niline takes a monolayer arrangement with the long axis inclined to the lay
ers of kaolinite. oNA molecules also take a monolayer arrangement though th
e orientation is not well ordered. Kaolinite-pNA and -oNA intercalation com
pounds exhibit second harmonic generation, which is evaluated quantitativel
y by the second-harmonic wave generated with evanescent wave (SHEW) method.
This indicates noncentrosymmetric arrangements of pNA and oNA, and such or
ientations are induced by the asymmetric environment of the interlayer regi
on of kaolinite.