After a historical description of the different families of porous com
pounds and their synthesis pathways, the paper describes a particular
system, the ULM series, and the correlation between the evolution of t
he pertinent chemical parameters and the structure of the resulting ma
terials. The hypothesis for a possible mechanism of formation of these
porous solids is rested both by in situ experiments (NMR and synchrot
ron radiation) in hydrothermal conditions and from the examination of
its possible consequences, principally in the domain of magnet ic poro
us compounds. The analysis of its limits leads to a new family of comp
osite inorganic organic porous solids in which organic and inorganic p
arts participate in the framework.