In situ X-ray diffraction (XRD) and environmental scanning
electron
microscope (ESEM) crystallization experiments show oriented growth
of magnesium sulfate crystals on a diethylenetriamine-penta-methylene
phosphonic acid (DTPMP) template adsorbed onto Iceland spar (calcite,
CaCO3) cleavage surfaces. Epsomite (MgSO4·7H2O) and hexahydrite (MgSO4·6H2O)
crystallize (depending on the ambient conditions) in the presence
of DTPMP with (010)epsomite//(101̅4)calcite and (1̅11)hexahydrite//(101̅4)calcite, whereas in the absence of DTPMP they show no preferred orientation.
On the other hand, sodium sulfate (mirabilite, Na2SO4·10H2O) nucleates onto a Ca-DTPMP precipitate
with (001)mirabilite//(101̅4)calcite.
In contrast, different sodium sulfate phases crystallize and grow
with no preferred crystallographic orientation in the absence of an
organic additive. These results allow us to propose a model for the
interaction calcite-DTPMP-Na and Mg sulfates based on the template-assisted
nucleation and oriented heterogeneous crystallization, mediated by
a Ca-precipitate, of inorganic salts on calcitic substrates. This
effect results in a (measured) reduction in the critical supersaturation
reached by these salts when crystallizing in confined geometries,
i.e., a pore, thus resulting in a reduction in crystallization pressure
and damage to porous substrates such as building stones. These results
have implications in fields where in-pore crystallization of salts
results in damage or plugging of the porous network, e.g., cultural
heritage conservation and in the oil industry, where phosphonates
are used as crystallization inhibitors.