Platinum nanoparticles "burrow" into a zeolite support and form new pores
Zeolites are crystalline, highly porous silicates. Because of their large surface area and their cage-like pores, which can take up "guest molecules", they are used as ion exchangers, molecular sieves, and catalysts. The researchers chose one of these zeolites as a support for their platinum particles and exposed them, at 800 °C, to an atmosphere equivalent to that in an average car exhaust. After one hundred hours, they looked at the little platinum-containing zeolite crystals under an electron microscope. Amazingly, there were no more platinum particles to be found on the surface of the zeolite. Where could they have gone? The surprising discovery: the tiny spheres of precious metal had burrowed into the surface of the zeolite. In the process, they left behind little channels with a diameter corresponding to the diameter of the particles. The researchers noted that there was a preferred direction for the channels within the zeolite crystals. The channels have a hexagonal cross-section, which is in agreement with the lattice structure of the zeolite, and the channel walls consist of facets of the crystal. Aside from a platinum sphere at the end of each pore, they are empty and the surrounding crystal structure is not disturbed in any way. Atoms have clearly just disappeared from the crystal lattice. At the points of contact between the platinum particles and the zeolite, the platinum presumably catalyzes a chemical reaction between the silicon and oxygen atoms of the zeolite and the components of the exhaust. The components of the zeolite can thus leave the crystal in the form of gaseous SiO or Si(OH)4. The platinum particles "sink" deeper and deeper into the holes formed by the reaction.
"The observed phenomenon could be used to produce tailored porous materials," hopes Kato. "The number of pores, as well as their shape and size could be controlled by the diameter of the platinum particles, the duration of heating, the type of zeolite selected, and the orientation of the crystals."
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