Pulsed field gradient (PFG) nuclear magnetic resonance (NMR) is applie
d to study convective and diffusional transport in chromatographic col
umns packed with totally porous support particles, Here stagnant zones
exist in the particle pores;, and diffusional mass-transfer limitatio
ns between fluid molecules diffusing in the intraparticle pore network
and flowing in the interparticle void space are detected quantitative
ly, Axial displacement probability distributions were measured for wat
er over a range of Peclet numbers and observation times, with diffusio
n lengths between 0.15 and 0.91 times the average support particle dia
meter. The transition towards complete diffusional exchange is demonst
rated, thereby also revealing the development of the classical convect
ive dispersion process in a packed bed of (porous) particles. (C) 1998
Elsevier Science Inc.