R. Shiraki et Sl. Brantley, KINETICS OF NEAR-EQUILIBRIUM CALCITE PRECIPITATION AT 100-DEGREES-C -AN EVALUATION OF ELEMENTARY REACTION-BASED AND AFFINITY-BASED RATE LAWS, Geochimica et cosmochimica acta, 59(8), 1995, pp. 1457-1471
Three affinity-based rate models based upon physical growth mechanisms
were used to fit surface-controlled precipitation rate data for calci
te using a continuously stirred tank reactor in NaOH-CaCl2-CO2-H2O sol
utions at 100 degrees C and 100 bars total pressure between pH 6.38 an
d 6.98. At higher stirring speeds, when alpha(H2CO3) was smaller than
2.33 x 10(-3), rate showed a parabolic dependence upon exp(Delta/RT)
for exp(Delta G/RT) < 1.72. However, the rate increased exponentially
for exp(Delta G/RT) > 1.72 and followed a rate law based upon the assu
mption that surface nucleation is rate-limiting. When alpha(H2CO3) wa
s greater than 5.07 x 10(-3), the rate showed a linear dependence upon
exp(Delta G/RT), suggesting growth by a simple surface adsorption mec
hanism. The rate of these three mechanisms at 100 degrees C can be exp
ressed by the following equations: [GRAPHICS] The mechanistic model of
Plummer et al. (1978) given by R(net) = k(1)a(H+) + k(2)a(H2CO3) + k
(3)a(H2O) - k(4)a(Ca2+)a(HCO3-) also describes the precipitation rate
when growth followed the spiral growth equation. The rate constant for
precipitation, k(4), ranges between 7.08 X 10(-4) to 1.01 X 10(-3) mo
les cm(-2) s(-1) in the a(H2CO3) range studied. This work shows that
precipitation at 100 degrees C in the spiral growth regime is well fit
by both the mechanistic model of Plummer et al. (1978), based on mult
iple elementary reactions, and by a model derived for growth at screw
dislocations. Outside of the regime of spiral growth, however, the mod
el of Plummer et al. (1978) fails, suggesting that different elementar
y reactions control growth in the adsorption or two-dimensional nuclea
tion regimes. However, the model of Plummer et al. (1978), based upon
individual elementary reactions, accurately predicts both dissolution
and precipitation of calcite under certain conditions; tests of the af
finity based models reveal that none of these models accurately predic
t dissolution. Therefore, although affinity-based models may yield ins
ights concerning the physical mechanism of growth, they may not be as
useful in modelling dissolution and growth over the full range of Delt
a G.