INHIBITION OF CALCITE PRECIPITATION BY ORTHOPHOSPHATE: SPECIATION AND THERMODYNAMIC CONSIDERATIONS

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dc.contributor.author Lin Y.P.
dc.contributor.author Singer P.C.
dc.date.accessioned 2024-05-05T03:46:12Z
dc.date.available 2024-05-05T03:46:12Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=12091809
dc.identifier.citation Geochimica et Cosmochimica Acta, 2006, 70, 10, 2530-2539
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/43817
dc.description.abstract The inhibition of heterogeneous calcite precipitation by orthophosphate was investigated under four different solution compositions using a pH-stat system. The system composition was designed to maintain a constant degree of supersaturation with respect to calcite, but with different carbonate/calcium ratios and pH values during precipitation. Inhibition in the presence of orthophosphate was found to be more effective at lower carbonate/calcium ratios and lower pH values. With the assumption that the calcite precipitation rate is proportional to the surface concentration of active crystal-growth sites, the reduction in the rate of calcite precipitation by phosphate can be explained by a Langmuir adsorption model using a conditional equilibrium constant and total phosphate concentration. Through a detailed analysis of chemical speciation in the solution phase and calcite surface speciation using chemical equilibrium computer modeling, the "conditional" equilibrium constants obtained at different solution compositions were found to converge to a single "non-conditional" value if only multiscripts(CaHPO, 4 ( aq ), mml:none(), mml:none(), 0) was considered in the adsorption reaction. This suggests that multiscripts(CaHPO, 4 ( aq ), mml:none(), mml:none(), 0) is the responsible species for inhibition of calcite precipitation because it adsorbs to the surface and blocks the active crystal-growth sites. The standard enthalpy change (?H0) and standard entropy change (T?S0) of the adsorption reaction, determined by experiments performed from 15 to 45 °C, were 58.5 and 98.3 kJ/mol, respectively. The high positive values of the standard enthalpy change and the standard entropy change suggest that the adsorption reaction is an endothermic reaction, chemisorptive in nature, and driven by the entropy change, most likely resulting from the dehydration process that accompanies the adsorption of multiscripts(CaHPO, 4 ( aq ), mml:none(), mml:none(), 0) onto the calcite surface. ? 2006 Elsevier Inc. All rights reserved.
dc.subject CALCITE
dc.subject ORTHOPHOSPHATE
dc.subject PH
dc.subject PRECIPITATION (CHEMISTRY)
dc.subject SPECIATION (CHEMISTRY)
dc.title INHIBITION OF CALCITE PRECIPITATION BY ORTHOPHOSPHATE: SPECIATION AND THERMODYNAMIC CONSIDERATIONS
dc.type Статья
dc.identifier.doi 10.1016/j.gca.2006.03.002


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