RATES OF FELDSPAR DISSOLUTION AT PH 3-7 WITH 0-8 M M OXALIC ACID
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dc.contributor.author | Stillings L.L. | |
dc.contributor.author | Drever J.I. | |
dc.contributor.author | Brantley S.L. | |
dc.contributor.author | Yanting S. | |
dc.contributor.author | Oxburgh R. | |
dc.date.accessioned | 2020-11-20T10:52:40Z | |
dc.date.available | 2020-11-20T10:52:40Z | |
dc.date.issued | 1996 | |
dc.identifier | https://elibrary.ru/item.asp?id=485243 | |
dc.identifier.citation | Chemical Geology, 1996, , 1, 79-89 | |
dc.identifier.issn | 0009-2541 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/19138 | |
dc.description.abstract | Feldspar dissolution rates were measured in flow-through reactors, over a pH range of 3-7, oxalic acid concentration of 0-8 m M, and feldspar compositional range of An0-An76. Dissolution rates in 0 and 1 m M concentrations of oxalic acid increased linearly with increasing mole percent anorthite in the solid. Dissolution was nonstoichiometric in oxalic acid, due to a preferential release of Al at steady state. 1 m M 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 feldspar. The ligand-promoted rate, RL, defined as the observed total rate in oxalic acid minus the proton-promoted rate, Rt - RH, was estimated as 10-12.8(aHOx- + aOx2-)0.75, suggesting that both HC2O-4 (bioxalate) and C2O2-4 (oxalate) play a role in the dissolution mechanism. | |
dc.title | RATES OF FELDSPAR DISSOLUTION AT PH 3-7 WITH 0-8 M M OXALIC ACID | |
dc.type | Статья |
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