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Isopiestic Determination of the Osmotic and Activity Coefficients of the {yNaH2PO4 + (1 − y)KH2PO4}(aq) System at T = 298.15 K
dc.contributor.author | Ivanović, Tijana | |
dc.contributor.author | Popović, Daniela | |
dc.contributor.author | Miladinović, Jelena | |
dc.contributor.author | Rard, Joseph | |
dc.contributor.author | Miladinović, Zoran | |
dc.contributor.author | Belošević, Svetlana | |
dc.contributor.author | Trivunac, Katarina | |
dc.date.accessioned | 2022-09-23T09:16:45Z | |
dc.date.available | 2022-09-23T09:16:45Z | |
dc.date.issued | 2019-03 | |
dc.identifier.uri | https://platon.pr.ac.rs/handle/123456789/640 | |
dc.description.abstract | Isopiestic measurements have been made for aqueous mixtures of NaH2PO4 and KH2PO4 at T = (298.15 ± 0.01) K, at NaH2PO4 ionic strength fractions y = (0, 0.19108, 0.38306, 0.58192, and 1), assuming that both electrolytes dissociate as 1:1 electrolytes, using KCl(aq) as the reference standard solution. Model parameters for an extended form of Pitzer’s ion-interaction model and also for the Clegg–Pitzer–Brimblecombe equa-tions based on the mole-fraction-composition scale were evaluated at T = 298.15 K for NaH2PO4(aq) using the present isopiestic results (13 values), as were those for KH2PO4(aq) using the present isopiestic results (12 values), together with numerous critically-assessed osmotic coefficients for both electrolytes taken from the published literature. The thermo-dynamic models for KH2PO4(aq) extend to m = 2.187 mol·kg−1, which is slightly above saturation, while those for NaH2PO4(aq) extend to m = 7.5 mol·kg−1, which is below satu-ration. The 39 osmotic coefficients for the ternary mixtures from the present study along with 42 values from a published study were likewise represented with these models, with both the usual Pitzer mixing terms and also Scatchard’s neutral-electrolyte model mix-ing terms being used for the extended ion-interaction model. Two mixing parameters were needed for each of the models, and all three models gave similar quality represen-tations of the experimental results. Maximum differences in calculated values of mean molality-based activity coefficients for these three models are ∆γ±(NaH2PO4) ≤ 0.0080 and ∆γ±(KH2PO4) ≤ 0.0043. The experimental results were also found to nearly conform to Zdanovskii’s rule. | en_US |
dc.language.iso | en_US | en_US |
dc.publisher | Journal of Solution Chemistry | en_US |
dc.rights | Ауторство-Некомерцијално-Без прерада 3.0 САД | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/us/ | * |
dc.title | Isopiestic Determination of the Osmotic and Activity Coefficients of the {yNaH2PO4 + (1 − y)KH2PO4}(aq) System at T = 298.15 K | en_US |
dc.title.alternative | Journal of Solution Chemistry | en_US |
dc.type | clanak-u-casopisu | en_US |
dc.description.version | publishedVersion | en_US |
dc.identifier.doi | 10.1007/s10953-018-0839-4 Authors: | |
dc.citation.volume | 48 | |
dc.citation.issue | 3 | |
dc.subject.keywords | Aqueous solutions | en_US |
dc.subject.keywords | Isopiestic measurements | en_US |
dc.subject.keywords | Osmotic coefficients | en_US |
dc.type.mCategory | M23 | en_US |
dc.type.mCategory | openAccess | en_US |
dc.type.mCategory | M23 | en_US |
dc.type.mCategory | openAccess | en_US |