Nine organic sorbates of different scattering power were adsorbed into
the mesopores of calcined, high quality B-MCM-41. The intensity of th
e observed X-ray diffraction peaks of the loaded samples results from
the difference in the scattering power (or 'scattering contrast') betw
een the two building blocks (amorphous silicate wall and amorphous sor
bate) of the MCM-41 structure. In general, the intensity of the X-ray
peaks decreases with decreasing 'scattering contrast' and is zero when
the scattering power of the silicate wall and the pore filling materi
al are similar (bromoform loaded B-MCM-41). After the recalcination of
the loaded B-MCM-41 materials all X-ray diffraction intensities are r
ecovered to about the same level as observed for the calcined sample w
hich was never used for an adsorption experiment. It is concluded that
the general structure of the MCM-41 material with its regular arrange
ment of the channels is maintained during all the calcination and adso
rption processes. This is confirmed by transmission electron micrograp
hs of B-MCM-41 which had been calcined, loaded with bromoform and calc
ined again.