Estimates for the density of periodic three-dimensional nets in Euclid
ean three-dimensional space (R3) are derived. The analysis assumes tha
t the nets tile triply periodic hyperbolic surfaces that are free of s
elf-intersections (embedded in R3). Upper and lower bounds of the net
density as a function of the average ring size on the surfaces are giv
en. These geometrical relations are compared with framework densities
of a range of silicon-rich zeolites, silica clathrasils and dense four
-connected silicates in order to separate the roles of geometry and ch
emistry in setting silicate densities. The data suggest that silica fr
ameworks are constrained by an approximate requirement of constant are
a per framework vertex in addition to the impositions of Euclidean thr
ee-space and are thus hyperbolic two-dimensional (layer) structures.