Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Dissolution kinetics of heulandite at pH 2--12 and 25{degrees}C

Journal Article · · Geochimica et Cosmochimica Acta
Because of their favourable cation exchange reactions, heulandite and clinoptilolite have been suggested as being capable of immobilizing radionuclides and therefore could possibly act as an important barrier for nuclear waste. Recent studies of laboratory-reacted minerals indicate, however, that hydrated surface layers tend to accumulate highly hydrolyzable heavy elements. These hydrated layers may therefore be the most important retardants for radionuclides. The dissolution rate of heulandite depends strongly on pH. Based on silica release, the logarithm of the steady-state dissolution rate at pH 2 is {minus}13.1 mol cm{sup {minus}2} s{sup {minus}1}. The logarithm of the rate decreases to {minus}15.8 mol cm{sup {minus}2} s{sup {minus}1} at pH 7.2 and increases again to {minus}14.6 mol cm{sup {minus}2} s{sup {minus}1} at pH 12.2. At low pH, Al is released preferentially to silica; but at intermediate and high pH, the release of silica appears to be congruent relative to Al. The change in dissolution rate with pH indicates that at low pH, the dissolution mechanism is controlled by the detachment of a positively charged Al species, >Al-OH{sub 2}{sup +}. Below pH 5, however, a silica-rich surface layer is formed requiring diffusion through the layer. At intermediate and high pH, it is likely that the dissolution rate is controlled by the detachment of a negatively charged silica species, >Si{sup {minus}}O{sup {minus}}. The reaction order of the hydrogen ion under low pH conditions is 0.7, and the reaction order of the OH{sup {minus}} ion is 0.3 at high pH. The measured dissolution rates indicate that a 1 mm heulandite crystal would dissolve in 300,000 yrs if the solution composition is maintained undersaturated. 75 refs., 11 figs., 3 tabs.
OSTI ID:
139166
Journal Information:
Geochimica et Cosmochimica Acta, Journal Name: Geochimica et Cosmochimica Acta Journal Issue: 11 Vol. 57; ISSN GCACAK; ISSN 0016-7037
Country of Publication:
United States
Language:
English

Similar Records

Micro FT-IR study of the hydration-layer during dissolution of silica glass
Journal Article · Fri Feb 28 23:00:00 EST 1997 · Geochimica et Cosmochimica Acta · OSTI ID:554909

Clinoptilolite and heulandite structural differences as revealed by multinuclear nuclear magnetic resonance spectroscopy
Journal Article · Wed Jan 26 23:00:00 EST 1994 · Journal of Physical Chemistry; (United States) · OSTI ID:5146432

Diopside dissolution kinetics as a function of pH, CO[sub 2], temperature, and time
Journal Article · Thu Dec 31 23:00:00 EST 1992 · Geochimica et Cosmochimica Acta; (United States) · OSTI ID:6951094