Research
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In fact, even a field such as evolutionary biology relies in part on the understanding of mineral at the interface with water. After all, cluster-containing enzymes may have their origin in small mineral fragments that have been taken up by cells, and that have subsequently been stabilised by the evolution of an organic scaffold. |
Activation of a metal-oxide mineral proceeds at the surface. It can be very difficult to study this type of reactions, since extended surfaces can contain different surface features which differ enormously in reactivity. Bulk analysis will thus be misleading and will only provide overall reactivities, which will not give any meaningful mechanistic information. |
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A particularly interesting class of discrete metal oxide clusters are the polyoxometalates. A few different areas that we focus on are described below.
Polyoxoniobates
The polyoxoniobates are different from the polyoxovanadates, -molybdates and -tungstates in that they typically are unstable at low pH, while showing good stability under more alkaline conditions. In addition, they are often more tolerant towards reducing conditions, suggesting their use as electron sinks, since they will seek to stay in or return to their higher oxidation states. Few homoleptic polyoxoniobates were until recently known, and their use as ligands is almost completely unexplored.
Figure: the ‘super’-Lindqvist ion [Ti12Nb6O44]10-.
NMR
Figure: Saturation transfer between two species separated by only a few ppm – the pulse sequence consists of pi/2, precession, pi/2, mixing, pi/2, observation
Mass spectrometry
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Figure: Stacked spectra obtained as a function of cone voltage.
Simulation and data decomposition
In addition to this, we also use computational chemistry — chiefly density functional theory-based methods — to improve our understanding of the chemistry of metal oxides in solution.
Figure: Concentration profiles derived from OPA treatment of stopped flow data of an oxidation reaction