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Solubilization-emulsification mechanisms of detergency

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184 C.A. Miller and K.H. Raney/Colloids Surfaces A: Physicochem. Eng. Aspects 74 (1993) 169-215<br />

triolein. The D phase is seen, however, for<br />

surfactant concentrations well above that <strong>of</strong> Fig.<br />

16. Note that the amounts <strong>of</strong> oleyl alcohol<br />

needed to depress the temperatures <strong>of</strong> the<br />

various phase boundaries are much greater than<br />

are shown in Fig. 15 for hydrocarbon systems.<br />

A likely explanation is that much <strong>of</strong> the oleyl<br />

alcohol is dissolved in the bulk triglyceride<br />

phase, leaving relatively little alcohol in the<br />

surfactant films which, to a large extent,<br />

determine the basic phase behavior by<br />

controlling the aggregate shape.<br />

4. Diffusion path analysis<br />

Being <strong>of</strong> rather short duration and typically<br />

involving small quantities <strong>of</strong> soils, <strong>detergency</strong><br />

processes are strongly influenced by dynamic,<br />

diffusional phenomena which occur on a<br />

microscopic scale. Oily soil removal, in<br />

particular, depends on phase transitions which<br />

occur at the oil-washing solution interface. The<br />

preceding section described equilibrium phase<br />

behavior in both water-surfactant systems,<br />

representing the washing solution, and<br />

oil-water-surfactant systems, As demonstrated<br />

below, such equilibrium phase behavior can be<br />

combined with the theory <strong>of</strong> diffusion processes<br />

to interpret certain dynamic behavior such as<br />

intermediate phase formation and spontaneous<br />

<strong>emulsification</strong> that occurs during detergent<br />

processes.<br />

A mathematical technique called diffusion<br />

path analysis has been used with success in<br />

predicting certain dynamic phenomena in<br />

multicomponent solid and liquid systems when<br />

two phases not in equilibrium are brought into<br />

contact with one another [62-64]. Essentially, a<br />

time-invariant path <strong>of</strong> compositions can be<br />

plotted across an equilibrium phase diagram<br />

by-solving component transport equations with<br />

certain assumptions and boundary conditions.<br />

First, convection in the system from any source<br />

is assumed to be negligible. Second, the two<br />

phases are assumed to be semiinfinite in extent.<br />

This assumption simplifies the mathematical<br />

analysis and is probably reasonable at least for<br />

short times after contacting. Third, diffusion <strong>of</strong><br />

each species is assumed to be dependent only on<br />

its own concentration gradient with a uniform<br />

diffusion coefficient in each phase. Also, local<br />

equilibrium is assumed at all interfaces which<br />

form; this means that the compositions at the<br />

interfaces are defined by equilibrium tie lines.<br />

Diffusion path analysis is most conveniently<br />

applied to three-component, i.e. ternary,<br />

systems. In this situation, the phase diagram can<br />

be represented in the form <strong>of</strong> a two-dimensional<br />

triangle as, for instance, in Fig. 8, with<br />

two-phase regions shown as regions <strong>of</strong> varying<br />

shape containing equilibrium tie lines and<br />

three-phase regions represented as triangles in<br />

which the compositions <strong>of</strong> the equilibrium<br />

phases are shown as the vertices. The analysis in<br />

this case consists <strong>of</strong> solving in each phase the<br />

following transport equations for two <strong>of</strong> the<br />

species<br />

(∂wi/∂t) = Di(∂ 2 wi/∂x 2 ) i = 1,2 (3)<br />

where x is the distance from the initial surface<br />

<strong>of</strong> contact, t is time and wi and D i are the mass<br />

fraction and diffusivity <strong>of</strong> species i,<br />

respectively. The value <strong>of</strong> W3 for the third<br />

species is found by invoking Σw i = 1. The<br />

semi-infinite phase assumption allows transformation<br />

<strong>of</strong> the above equations to ordinary<br />

differential equations in the similarity variable<br />

η i = [x/(4D it) 1/2 ]. Integration yields the following<br />

error function solutions for the diffusion path<br />

segment in each phase<br />

w i = A i + B i erf η I i = 1,2 (4)<br />

where A i and B i are constants which are<br />

evaluated from the boundary conditions. Since<br />

η i varies from - ∞ to + ∞ at each value <strong>of</strong> time,<br />

the set <strong>of</strong> compositions given by Eq. (4) is<br />

independent <strong>of</strong> time although the position x <strong>of</strong> a<br />

specific composition does vary with time. It is<br />

<strong>of</strong>ten convenient to plot the compositions or<br />

"diffusion path" directly on the equilibrium<br />

phase diagram.<br />

In evaluating A i and B i for phases in contact.<br />

iteration on a tie line is performed until the<br />

individual species mass balances at the interface<br />

are satisfied. In addition to obtaining the path <strong>of</strong><br />

compositions that forms between the initial

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