I would like to know if there are any works describing the variation of ionic strength for alkali silicate solutions at high solid concentration (i.e. >50%) i.e. when the suspension turns from liquid like to honey like consistence. If I have a suspension of colloidal particles in a diluted waterglass solution, the the zeta potential and Debye length can be calculated by the DLVO theory in diluted state, but what happens when the viscosity of the system increase from liquid to honey-like state? I suppose the mobility of ionic species drops due ionic crowding (electroviscous effects)? how can I quantify this phenomenon? how does the ionic double layer change?

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