Silicates are among the most abundant minerals on the earth's crust and exist in a wide range of crystalline and amorphous forms. Porous silicate gels occur naturally as a consequence of interaction between silicate minerals, either crystalline or amorphous, and water. They can also be synthesized and find a variety of technological applications such as adsorption, catalysis, separation, environmental remediation, and biomedicine. 1-6 Of particular interest is the