Kg. Knauss et Sa. Copenhaver, THE EFFECT OF MALONATE ON THE DISSOLUTION KINETICS OF ALBITE, QUARTZ,AND MICROCLINE AS A FUNCTION OF PH AT 70-DEGREES-C, Applied geochemistry, 10(1), 1995, pp. 17-33
The effect of malonate on the dissolution rate of the reservoir minera
ls: albite, quartz, and microcline has been examined. The effect of pH
on rate has been decoupled from the effect of the ligand by controlli
ng pH using dilute buffer solutions at values of pH 4 through pH 10 at
70 degrees C. Any effect of the buffer ligands (acetate and berate) o
r alkali cation (Na) on rate was accounted for by comparing the measur
ed dissolution rates in buffer solutions with and without malonate. Fl
owing reactors were used and malonate concentration was varied from 1
to 100 mmolal. As malonate anion concentration is increased, the disso
lution rate of these minerals also increases. At moderately acidic to
near neutral pH in the solutions containing the highest malonate conce
ntration, malonate most significantly increases the dissolution rate o
f the silicates over that expected due to simple hydrolysis. At alkali
ne pH the effect of malonate on the dissolution rate of these silicate
s is not significant, compared to the dissolution rate due to simple h
ydrolysis alone.