Phosphonate-scale inhibitors are commonly used to prevent scale format
ion in many industrial processes involving high-salinity brine solutio
ns. To effectively prevent scale formation in these industrial process
es, one must have a fundamental understanding of how phosphonates are
released into high-salinity brines. Because phosphonates can precipita
te with divalent cations such as calcium, their release into aqueous m
edia is often governed by many dissolution mechanisms. This study focu
ses on the release of calcium;phosphonate precipitates from porous med
ia (as related to oil-field applications) and a mathematical model des
cribing these release mechanisms based on mechanistic studies of pore-
level phenomena. The phosphonate used was 1-hydroxyethylidene-1,1-diph
osphonic acid (HEDP). The release of two distinct calcium-HEDP precipi
tates from porous media was studied: soluble, fibrous 1:1; insoluble,
spherical 2:1. Visual studies using etched-glass micromodels showed th
at five distinct regimes govern the release of 1:1 calcium-HEDP precip
itate from porous media. Conversely, the release of 2:1 calcium-HEDP p
recipitate was dominated by two distinct regimes. A continuum model de
veloped describes the release of both precipitates from porous media b
y mathematically describing each of the distinct release regimes and d
efining conditions raider which the transition between release regimes
occurred. Experimental data agreed excellently with model simulations
for both precipitates.