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Silicate Chemistry

Sodium silicates (Na2O • XSiO2) are metal oxides of silica. All soluble silicates can be differentiated by their ratio, defined as the weight proportion of silica to alkali (SiO2 / Na2O). Ratio determines the physical and chemical properties of the product.

Four major chemical processes account for the usefulness of silicates in industry, construction and other fields. Each of the hundreds of applications for silicates takes advantage of one or more of these phenomena: 
  • Hydration and Dehydration 
  • Metal Ion Reaction 
  • Surface Charge Modification 
  • Gelation and Precipitation Reactions
  • Hydration and Dehydration
    Hydration is the pick-up of moisture by a solid material from the air or from a water source (dissolving). Dehydration is the loss of moisture from a material to the air or to another substrate.

    Soluble silicates are unique in the way they dissolve from their solid forms (powders and glasses) and the way they dry from liquid solutions. The more water a solid product contains, the faster it will dissolve. Also, the lower the ratio of silica to alkali in the solid product, the faster it will dissolve.

    Dehydration of silicate liquids at equivalent solids depends greatly on ratio. The higher the ratio, the faster the drying rate, because high ratio products have low alkali levels. Alkalis tend to hold moisture more readily.

    The glassy nature of silicates imparts strong and rigid physical properties to dried films or coatings. Silicates air dry to a specific moisture level, according to ambient temperature and relative humidity. Heating is necessary to take these films to complete dryness—a condition in which silicates become nearly insoluble. Reaction with other materials, such as aluminum or calcium compounds, will make the film or coating completely insoluble.

    Metal Ion Reactions
    Using silicates to tie up metal ions is an inexpensive way to enhance the performance of many processes.

    Soluble silica reacts with all multivalent cationic metal ions to form the corresponding insoluble metal silicate. These multivalent cationic metal ions include:
     
  • Calcium
  • Manganese
  • Magnesium
  •  
  • Cadmium
  • Iron
  • Lead
  •  
  • Zinc
  • Nickel
  • Chromium
  •  
  • Copper
  • Silicates will precipitate these metals out of solution and render them insoluble and non-reactive. The reactant byproduct normally displays long-term stability. The bond formed can be broken only by extremely aggressive chemical action.

    Detergency, pulp and paper, waste treatment, and water treatment applications all benefit from the silicate reaction that eliminates or ties up undesirable metals. Left in the process to react with other more expensive chemicals, these metals degrade the functionality of those chemicals or render the application less effective.

    Surface Charge Modification
    All dissolved silica has an anionic charge of -2. In solution, silica can donate this charge to other materials dispersed in water and cause them to be negatively charged. If all solids become negatively charged, they will repel one another. This phenomenon is the basis for the dispersive and deflocculating effects of silicates.

    These effects are important in applications such as detergency and clay manufacture. In detergency, the silica prevents the redeposition of soils on clothing. In clay processing, the silica helps keep the clay dispersed using substantially less water.

    Precipitation and Gelation Reactions
    In essence, these reactions involve the destabilization of liquid silicate solutions. When the pH value of a liquid silicate is modified to a point below 10.7, the silica is destabilized and the system polymerizes or gels.

    Individual silica monomers link up to form long chains of repeating SiO2 units. The result is a precipitation of silica, a colloidal solution or a continuous gel, depending on the silica concentration. This method is one way of making a solution insoluble. In these reactions, the silicate solution becomes the feedstock for the production of silica solutions, gels or precipitates.


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