Silica Break Through of Demineralizers
Silica Breakthrough of Demineralizers
SILICA | |
| A large percentage of the earth's solid crust is silicon. Silicon is found to a certain degree in all natural water supplies, usually as dissolved silica (Si02) or as small suspended silicate particles (colloidal silica). In applications calling for demineralized water / ultrapure water, demineralization of ion exchangers are an effective and common means of removing silica. But basic anion exchange resins must be strongly charged to remove silica effectively because dissolved silica has a very low ionic strength. When exchangers approach their end point, silica usually is the first impurity to "break through" into the effluent. For this reason, silica is a critical quality control parameter in demineralized / ultrapure water treatment. Conductivity measurements, long used as a measure of water purity, are unreliable in detecting resin bed exhaustion because silica breakthrough does not increase conductance appreciably. For high pressure boiler operators, semiconductor manufacturers and chemical processors, continuous silica analyzers provide dependable monitoring of demineralizer performance and guard against introduction of silica into pure water reservoirs and systems downstream. [Figure] Two stages of a strongly basic exchange column show anion layering as column nears exhaustion. Silica is the first impurity to break through the exhausted resin. Research data indicate slug concentrations of silicates slipping off the exhausted column can be four or more times higher than that of incoming raw water. | Source: Water analysis handbook - Hach |
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