4 research outputs found
Solid-State Crystal-to-Crystal Phase Transitions and Reversible Structure–Temperature Behavior of Phosphovanadomolybdic Acid, H<sub>5</sub>PV<sub>2</sub>Mo<sub>10</sub>O<sub>40</sub>
The crystal packing and secondary
structure of H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> was followed by careful X-ray
diffraction studies that revealed four unique structures and three
solid phase transitions at temperatures between 25 and 55 °C,
with loss of solvated water and concomitant contraction of the volume
and increase of the packing density. Above 60 °C H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> becomes amorphous and
then anhydrous although the polyoxometalate cluster is stable indefinitely
up to 300 °C. Above this temperature, combined IR, Raman, XRD,
and XPS measurements show the decomposition of H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> to crystalline MoO<sub>3</sub> and probably amorphous vanadium oxide and vanadylphosphate, the
latter appearing to cover the surface of MoO<sub>3</sub>. Importantly,
H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> can be easily
recovered by dissolution in water at 80 °C
Solid-State Crystal-to-Crystal Phase Transitions and Reversible Structure–Temperature Behavior of Phosphovanadomolybdic Acid, H<sub>5</sub>PV<sub>2</sub>Mo<sub>10</sub>O<sub>40</sub>
The crystal packing and secondary
structure of H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> was followed by careful X-ray
diffraction studies that revealed four unique structures and three
solid phase transitions at temperatures between 25 and 55 °C,
with loss of solvated water and concomitant contraction of the volume
and increase of the packing density. Above 60 °C H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> becomes amorphous and
then anhydrous although the polyoxometalate cluster is stable indefinitely
up to 300 °C. Above this temperature, combined IR, Raman, XRD,
and XPS measurements show the decomposition of H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> to crystalline MoO<sub>3</sub> and probably amorphous vanadium oxide and vanadylphosphate, the
latter appearing to cover the surface of MoO<sub>3</sub>. Importantly,
H<sub>5</sub>PV<sub>2</sub>Mo<sub>12</sub>O<sub>40</sub> can be easily
recovered by dissolution in water at 80 °C
Dicobalt-μ-oxo Polyoxometalate Compound, [(α<sub>2</sub>‑P<sub>2</sub>W<sub>17</sub>O<sub>61</sub>Co)<sub>2</sub>O]<sup>14–</sup>: A Potent Species for Water Oxidation, C–H Bond Activation, and Oxygen Transfer
High-valent oxo compounds of transition
metals are often implicated
as active species in oxygenation of hydrocarbons through carbon–hydrogen
bond activation or oxygen transfer and also in water oxidation. Recently,
several examples of cobalt-catalyzed water oxidation have been reported,
and cobalt(IV) species have been suggested as active intermediates.
A reactive species, formally a dicobalt(IV)-μ-oxo polyoxometalate
compound [(α2-P2W17O61Co)2O]14–, [(POMCo)2O], has
now been isolated and characterized by the oxidation of a monomeric
[α2-P2W17O61CoII(H2O)]8–, [POMCoIIH2O], with ozone in water. The crystal structure shows
a nearly linear Co–O–Co moiety with a Co–O bond
length of ∼1.77 Å. In aqueous solution [(POMCo)2O] was identified by 31P NMR, Raman, and UV–vis
spectroscopy. Reactivity studies showed that [(POMCo)2O]2O] is an active compound for the oxidation of H2O to O2, direct oxygen transfer to water-soluble sulfoxides
and phosphines, indirect epoxidation of alkenes via a Mn porphyrin,
and the selective oxidation of alcohols by carbon–hydrogen
bond activation. The latter appears to occur via a hydrogen atom transfer
mechanism. Density functional and CASSCF calculations strongly indicate
that the electronic structure of [(POMCo)2O]2O] is best defined as a compound having two cobalt(III) atoms with
two oxidized oxygen atoms
Dicobalt-μ-oxo Polyoxometalate Compound, [(α<sub>2</sub>‑P<sub>2</sub>W<sub>17</sub>O<sub>61</sub>Co)<sub>2</sub>O]<sup>14–</sup>: A Potent Species for Water Oxidation, C–H Bond Activation, and Oxygen Transfer
High-valent oxo compounds of transition
metals are often implicated
as active species in oxygenation of hydrocarbons through carbon–hydrogen
bond activation or oxygen transfer and also in water oxidation. Recently,
several examples of cobalt-catalyzed water oxidation have been reported,
and cobalt(IV) species have been suggested as active intermediates.
A reactive species, formally a dicobalt(IV)-μ-oxo polyoxometalate
compound [(α<sub>2</sub>-P<sub>2</sub>W<sub>17</sub>O<sub>61</sub>Co)<sub>2</sub>O]<sup>14–</sup>, [(POMCo)<sub>2</sub>O], has
now been isolated and characterized by the oxidation of a monomeric
[α<sub>2</sub>-P<sub>2</sub>W<sub>17</sub>O<sub>61</sub>Co<sup>II</sup>(H<sub>2</sub>O)]<sup>8–</sup>, [POMCo<sup>II</sup>H<sub>2</sub>O], with ozone in water. The crystal structure shows
a nearly linear Co–O–Co moiety with a Co–O bond
length of ∼1.77 Å. In aqueous solution [(POMCo)<sub>2</sub>O] was identified by <sup>31</sup>P NMR, Raman, and UV–vis
spectroscopy. Reactivity studies showed that [(POMCo)<sub>2</sub>O]<sub>2</sub>O] is an active compound for the oxidation of H<sub>2</sub>O to O<sub>2</sub>, direct oxygen transfer to water-soluble sulfoxides
and phosphines, indirect epoxidation of alkenes via a Mn porphyrin,
and the selective oxidation of alcohols by carbon–hydrogen
bond activation. The latter appears to occur via a hydrogen atom transfer
mechanism. Density functional and CASSCF calculations strongly indicate
that the electronic structure of [(POMCo)<sub>2</sub>O]<sub>2</sub>O] is best defined as a compound having two cobalt(III) atoms with
two oxidized oxygen atoms
