Building a fundamental
understanding of the reactions between scale
inhibitor (SI) and formation minerals is essential for effectively
designing SI “squeeze” treatments. Results of bulk “apparent
adsorption” (Γapp) experiments are presented
for a widely used phosphonate SI, DETPMP, on calcite and dolomite
mineral substrates. The apparent adsorption results are supported
by (i) measuring the corresponding solution [Ca2+] and
pH values in solution, (ii) studying the surface chemistry of the
resulting SI/Ca precipitates using environmental scanning electron
microscopy–energy-dispersive X-ray (ESEM-EDX) analysis to identify
the morphology/composition of the SI/Ca precipitates, and (iii) a
detailed mass balance analysis, indicating the fate of the Ca2+ and the SI. Results revealed that DETPMP was dominantly
retained by both calcite and dolomite via a precipitation mechanism
(actually coupled adsorption/precipitation) for all initial pH values
(pH0 2, 4, and 6) and T = 95 °C,
although a small region of pure adsorption (Γ) was observed
at [DETPMP] < 100 ppm. Moreover, higher Γapp occurred
on dolomite than on calcite for all initial pH0. This result
is counterintuitive, because it is well-known that calcite is much
more reactive than dolomite. However, final equilibrium pH values
are higher for dolomite, compared to calcite. Thus, a higher pHfinal led to a more dissociated DETPMP and this effect had
a greater effect on SI/Ca precipitation than the higher [Ca2+] by rock dissolution. EDX analysis confirmed scale-inhibitor phosphorus
in the deposited solids, indicating coupled adsorption/precipitation.
Supporting mass balance calculations correlated very well with our
experimental observations, showing higher generated calcium in calcite
than dolomite and less calcium generation at higher initial pH0 (lower rock dissolution). Finally, an equilibrium mechanistic
model describing the inhibitor dissociation, Ca-binding to the dissociated
SI species, and precipitation of the SI_Ca
n
complex, coupled to the carbonate system, is proposed to qualitatively
explain these experimental findings.