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

Diopside dissolution kinetics as a function of pH, CO[sub 2], temperature, and time

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
; ;  [1]
  1. Lawrence Livermore National Lab., CA (United States)
The authors have measured the dissolution rate of diopside in dilute solutions (far from equilibrium) at 25, 50, and 70[degrees]C from pH 2 through pH 12 using a flow-through reactor. Reducing the CO[sub 2] concentration tenfold produced little, if any, effect on dissolution rate at alkaline pH (pH 8 through pH 12) at 25 and 70[degrees]C. Linear dissolution kinetics (i.e., time-invariant rates) were eventually observed in all runs. The overall trend with increasing pH is decreasing diopside dissolution rate based on the release rate of all constituents. The authors fit these rates by regression to a general rate law of the form r = Ak[[alpha][sub H[sup +]]][sup n], where A is the surface area, k is the rate constant, and n is the order with respect to hydrogen ion activity. At 70[degrees]C over the range pH 2 through pH 10 in solutions equilibrated with atmospheric CO[sub 2], the rate of diopside dissolution based on Si release is rate (mol/cm[sup 2]-s) = 2.45 ([plus minus]0.96)[times]10[sup [minus]13] [alpha][sub H[sup +]][sup 0.18[plus minus]0.03]. At 50[degrees]C the rate based on Si release is rate (mol/cm[sup 2]-s) = 1.10([plus minus]0.61)[times]10[sup [minus]13] [alpha][sub H[sup +]][sup 0.21[plus minus]]0.04. At 25[degrees]C the rate based on Si release is rate (mol/cm[sup 2]-s) = 2.88([plus minus]1.33)[times]10[sup [minus]14] [alpha][sub H[sup +]][sup 0.18[plus minus]0.03]. Based on a regression of the rate constants, over the temperature interval 25 to 70[degrees]C, the activation energy for the dissolution of diopside is 9.7 [plus minus] 0.4 kcal/mol. This energy is indicative of a surface-reaction controlled dissolution process, as is the observation of crystallographically controlled etch pits. 31 refs., 5 figs., 5 tabs.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
6951094
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Journal Name: Geochimica et Cosmochimica Acta; (United States) Vol. 57:2; ISSN GCACAK; ISSN 0016-7037
Country of Publication:
United States
Language:
English

Similar Records

Dissolution rates of prehnite, epidote, and albite
Journal Article · Thu Oct 31 23:00:00 EST 1991 · Geochimica et Cosmochimica Acta; (United States) · OSTI ID:5201175

Dissolution kinetics of heulandite at pH 2--12 and 25{degrees}C
Journal Article · Tue Jun 01 00:00:00 EDT 1993 · Geochimica et Cosmochimica Acta · OSTI ID:139166

Groundwater chemical evolution in a sandy silicate aquifer in northern Wisconsin 2. Reaction modeling
Journal Article · Fri Jan 31 23:00:00 EST 1992 · Water Resources Research; (United States) · OSTI ID:5178395