1974
DOI: 10.1016/0021-9797(74)90379-8
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The interpretation of electrokinetic potentials and the inaccuracy of the DLVO theory for anatase sols

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Cited by 18 publications
(8 citation statements)
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“…where 0 and 4~ are spherical polar coordinates with gravity acting in the 0 = 7r direction, A(R, )`), B(R, )`), and G(R, )`) the hydrodynamic correction functions (10), and t the time. By integrating [24], the limiting trajectory for particle capture can be located and used to compute the capture efficiency (10). This limiting trajectory corresponds to those trajectories furthest from the reference sphere which still lead to particle capture and are charac-terized by the upstream coordinates R = oo and 0 = 01ira.…”
Section: Gravity-enhanced Flocculation Experimentsmentioning
confidence: 99%
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“…where 0 and 4~ are spherical polar coordinates with gravity acting in the 0 = 7r direction, A(R, )`), B(R, )`), and G(R, )`) the hydrodynamic correction functions (10), and t the time. By integrating [24], the limiting trajectory for particle capture can be located and used to compute the capture efficiency (10). This limiting trajectory corresponds to those trajectories furthest from the reference sphere which still lead to particle capture and are charac-terized by the upstream coordinates R = oo and 0 = 01ira.…”
Section: Gravity-enhanced Flocculation Experimentsmentioning
confidence: 99%
“…electrophoretically determined ~" potential is commonly used as the characteristic potential in the calculation of the electrostatic repulsive force, although the relationship between the ~" potential and the surface potential remains unclear (24). Brownian tlocculation experiments with monodisperse systems have verified several of the qualitative features of the DLVO theory (25)(26)(27), and have yielded estimates of both the Hamaker constant (18,28,29) and an effective surface potential (25,27).…”
Section: Introductionmentioning
confidence: 99%
“…For the case of water, however, the most ubiquitous and important polar liquid, measurement of its viscosity in the presence of a strong, uniform field presents a strong challenge (as discussed later in this section), and to our knowledge no such direct measurements have been reported. Over the past six decades, therefore, the magnitude of the viscoelectric effect in water has been only indirectly estimated by extrapolation from its values for organic liquids ( 8 ), from estimates of its effect on electrokinetic phenomena ( 11 , 14 19 ), or by other approaches ( 7 , 12 , 20 , 21 ). These estimated values, as expressed in the viscoelectric coefficient f , vary over more than three orders of magnitude, ranging from f ∼10 −17 –2.5 × 10 −14 (V/m) 2 ( SI Appendix , Section 7 ).…”
mentioning
confidence: 99%
“…For completeness, we note that results contradictory to the viscoelectric model have also been reported ( 22 ) (i.e., suggesting a decreased water viscosity in an electric field). The reasons for the large span of these estimated f values were attributed to various factors such as solid/liquid coupling, varying ionic sizes, and varying water permittivity ( 12 , 19 ); however, while these factors may play some role, there is no evidence that they could lead to such large discrepancies.…”
mentioning
confidence: 99%
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