RATES OF FELDSPAR DISSOLUTION AT PH 3-7 WITH 0-8 MM OXALIC-ACID

Citation
Ll. Stillings et al., RATES OF FELDSPAR DISSOLUTION AT PH 3-7 WITH 0-8 MM OXALIC-ACID, Chemical geology, 132(1-4), 1996, pp. 79-89
Citations number
40
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
00092541
Volume
132
Issue
1-4
Year of publication
1996
Pages
79 - 89
Database
ISI
SICI code
0009-2541(1996)132:1-4<79:ROFDAP>2.0.ZU;2-V
Abstract
Feldspar dissolution rates were measured in flow-through reactors, ove r a pH range of 3-7, oxalic acid concentration of 0-8 mM, and feldspar compositional range of An(0)-An(76). Dissolution rates in 0 and 1 mM concentrations of oxalic acid increased linearly with increasing mole percent anorthite in the solid. Dissolution was nonstoichiometric in o xalic acid, due to a preferential release of Al at steady state. 1 mM concentrations of oxalic acid increased dissolution rates by a factor of 2-5 at pH 3 and 2-15 at pH 5-6. At pH 5-6 the rate enhancement due to oxalic acid may increase with increasing anorthite content of the f eldspar. The ligand-promoted rate; R(L), defined as the observed total rate in oxalic acid minus the proton-promoted rate, R(t)-R(H), was es timated as 10(-12.8)(a(HOx-)+a(Ox2-))(0.75), suggesting that both HC2O 4- (bioxalate) and C2O42- (oxalate) play a role in the dissolution mec hanism.