1971
DOI: 10.1039/tf9716702258
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Thermodynamics of polystyrene solutions. Part 1.—Polystyrene and methyl ethyl ketone

Abstract: The excess volumes V E of mixtures of polystyrene with methyl ethyl ketone determined at 25°C we negative. At a segment fraction & = 0.5 of polymer, VE is ca. 0.9 % of the total volume.Osmotic pressures have been measured from = 0.10 to 0.35 at 10" and at 50°C. The temperature coefficient of the reduced residual chemical potential x indicates a very small positive heat of mixing in accord with vapour pressure measurements of Bawn, Freeman and Kamaliddin at higher concentrations. The recent statistical thermody… Show more

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Cited by 113 publications
(25 citation statements)
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“…(9) and (10) in the homogeneous region at a series of temperatures and pressures is seen in Table 4. A similar increase of 2~ with polymer concentration has been observed experimentally for several polymer solution systems [14][15][16][17][18][19]. In the hole theory of S-S this dependence origi- nates in the free volume contribution to the partition function [20].…”
Section: The Z-functionsupporting
confidence: 52%
“…(9) and (10) in the homogeneous region at a series of temperatures and pressures is seen in Table 4. A similar increase of 2~ with polymer concentration has been observed experimentally for several polymer solution systems [14][15][16][17][18][19]. In the hole theory of S-S this dependence origi- nates in the free volume contribution to the partition function [20].…”
Section: The Z-functionsupporting
confidence: 52%
“…As a result, the residual chemical potential, µ 1 R , is able to provide the information of the sorption enthalpic energy for various organic compounds in soils. Flory (1971) …”
Section: Interaction Between Organic Contaminants and Soilmentioning
confidence: 99%
“…To evaluate the interaction between the organic contaminant and the soil, the SOC has been regarded as a solvent and its sorption characteristics are similar to that of a polymer (Weber et al, 1992). Flory and Hocker (1971) proposed an equation to compute the activity "a" of small solute molecules in a polymer: [3.14] where subscript 1 represents the solute phase, subscript 2 represents the polymer, φ i is volume fraction concentration, V i is molar volume, and χ is called the Flory interaction parameter. Flory-Huggins theory has been used to describe the thermodynamics of organic contaminants in a soil-water system (Chiou, 1983;Chin, 1989;Spurlock,1994) and it was always simplified as:…”
Section: Interaction Between Organic Contaminants and Soilmentioning
confidence: 99%
“…(12) M. B. Ewing and K. M. Marsh, J. Chem. (14) J. M. Bardin and D. Patterson, Polymer, 10, 247 (1969). (13) Phuong Nguyen Hong and G. Patterson, to be published.…”
mentioning
confidence: 99%