21 research outputs found

    The dominant Anopheles vectors of human malaria in the Asia-Pacific region: occurrence data, distribution maps and bionomic précis

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    <p>Abstract</p> <p>Background</p> <p>The final article in a series of three publications examining the global distribution of 41 dominant vector species (DVS) of malaria is presented here. The first publication examined the DVS from the Americas, with the second covering those species present in Africa, Europe and the Middle East. Here we discuss the 19 DVS of the Asian-Pacific region. This region experiences a high diversity of vector species, many occurring sympatrically, which, combined with the occurrence of a high number of species complexes and suspected species complexes, and behavioural plasticity of many of these major vectors, adds a level of entomological complexity not comparable elsewhere globally. To try and untangle the intricacy of the vectors of this region and to increase the effectiveness of vector control interventions, an understanding of the contemporary distribution of each species, combined with a synthesis of the current knowledge of their behaviour and ecology is needed.</p> <p>Results</p> <p>Expert opinion (EO) range maps, created with the most up-to-date expert knowledge of each DVS distribution, were combined with a contemporary database of occurrence data and a suite of open access, environmental and climatic variables. Using the Boosted Regression Tree (BRT) modelling method, distribution maps of each DVS were produced. The occurrence data were abstracted from the formal, published literature, plus other relevant sources, resulting in the collation of DVS occurrence at 10116 locations across 31 countries, of which 8853 were successfully geo-referenced and 7430 were resolved to spatial areas that could be included in the BRT model. A detailed summary of the information on the bionomics of each species and species complex is also presented.</p> <p>Conclusions</p> <p>This article concludes a project aimed to establish the contemporary global distribution of the DVS of malaria. The three articles produced are intended as a detailed reference for scientists continuing research into the aspects of taxonomy, biology and ecology relevant to species-specific vector control. This research is particularly relevant to help unravel the complicated taxonomic status, ecology and epidemiology of the vectors of the Asia-Pacific region. All the occurrence data, predictive maps and EO-shape files generated during the production of these publications will be made available in the public domain. We hope that this will encourage data sharing to improve future iterations of the distribution maps.</p

    Near-Infrared Photoluminescence from a Plutonyl Ion

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    Cerium(III) Carbonate Formation from {CeCp*<sub>2</sub>H}<sub>2</sub> and Carbon Dioxide: Structure and Mechanistic Insights

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    The reaction between {CeCp*<sub>2</sub>H}<sub>2</sub> with CO<sub>2</sub> in thf resulted in a new cerium­(III) carbonate species, {Ce­(Cp*)<sub>2</sub>(thf)}<sub>2</sub>(μ-η<sup>2</sup>:η<sup>1</sup>-CO<sub>3</sub>). Investigations into the mechanism suggest the intermediacy of a bridging oxo-complex, {CeCp*<sub>2</sub>(thf)<sub><i>x</i></sub>}<sub>2</sub>(μ-O), which could either be formed from the ring opening and oxygen abstraction from an oxygenated solvent such as thf or via insertion of CO<sub>2</sub> and elimination of formaldehyde from the resulting methylenediolate intermediate

    Unexpected Actinyl Cation-Directed Structural Variation in Neptunyl(VI) A‑Type Tri-lacunary Heteropolyoxotungstate Complexes

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    A-type tri-lacunary heteropolyoxotungstate anions (e.g., [PW<sub>9</sub>O<sub>34</sub>]<sup>9–</sup>, [AsW<sub>9</sub>O<sub>34</sub>]<sup>9–</sup>, [SiW<sub>9</sub>O<sub>34</sub>]<sup>10–</sup>, and [GeW<sub>9</sub>O<sub>34</sub>]<sup>10–</sup>) are multidentate oxygen donor ligands that readily form sandwich complexes with actinyl cations ({UO<sub>2</sub>}<sup>2+</sup>, {NpO<sub>2</sub>}<sup>+</sup>, {NpO<sub>2</sub>}<sup>2+</sup>, and {PuO<sub>2</sub>}<sup>2+</sup>) in near-neutral/slightly alkaline aqueous solutions. Two or three actinyl cations are sandwiched between two tri-lacunary anions, with additional cations (Na<sup>+</sup>, K<sup>+</sup>, or NH<sub>4</sub><sup>+</sup>) also often held within the cluster. Studies thus far have indicated that it is these additional +1 cations, rather than the specific actinyl cation, that direct the structural variation in the complexes formed. We now report the structural characterization of the neptunyl­(VI) cluster complex (NH<sub>4</sub>)<sub>13</sub>[Na­(NpO<sub>2</sub>)<sub>2</sub>(A-α-PW<sub>9</sub>O<sub>34</sub>)<sub>2</sub>]·12H<sub>2</sub>O. The anion in this complex, [Na­(NpO<sub>2</sub>)<sub>2</sub>(PW<sub>9</sub>O<sub>34</sub>)<sub>2</sub>]<sup>13–</sup>, contains one Na<sup>+</sup> cation and two {NpO<sub>2</sub>}<sup>2+</sup> cations held between two [PW<sub>9</sub>O<sub>34</sub>]<sup>9–</sup> anions, with an additional partial occupancy NH<sub>4</sub><sup>+</sup> or {NpO<sub>2</sub>}<sup>2+</sup> cation also present. In the analogous uranium­(VI) system, under similar reaction conditions that include an excess of NH<sub>4</sub>Cl in the parent solution, it was previously shown that [(NH<sub>4</sub>)<sub>2</sub>(U<sup>VI</sup>O<sub>2</sub>)<sub>2</sub>(A-PW<sub>9</sub>O<sub>34</sub>)<sub>2</sub>]<sup>12–</sup> is the dominant species in both solution and the crystallized salt. Spectroscopic studies provide further proof of differences in the observed chemistry for the {NpO<sub>2</sub>}<sup>2+</sup>/[PW<sub>9</sub>O<sub>34</sub>]<sup>9–</sup> and {UO<sub>2</sub>}<sup>2+</sup>/[PW<sub>9</sub>O<sub>34</sub>]<sup>9–</sup> systems, both in solution and in solid state complexes crystallized from comparable salt solutions. This work reveals that varying the actinide element (Np vs U) can indeed measurably impact structure and complex stability in the cluster chemistry of actinyl­(VI) cations with A-type tri-lacunary heteropolyoxotungstate anions

    Tetrahalide Complexes of the [U(NR)<sub>2</sub>]<sup>2+</sup> Ion: Synthesis, Theory, and Chlorine K‑Edge X‑ray Absorption Spectroscopy

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    Synthetic routes to salts containing uranium bis-imido tetrahalide anions [U­(NR)<sub>2</sub>X<sub>4</sub>]<sup>2–</sup> (X = Cl<sup>–</sup>, Br<sup>–</sup>) and non-coordinating NEt<sub>4</sub><sup>+</sup> and PPh<sub>4</sub><sup>+</sup> countercations are reported. In general, these compounds can be prepared from U(NR)<sub>2</sub>I<sub>2</sub>(THF)<sub><i>x</i></sub> (<i>x</i> = 2 and R = <sup><i>t</i></sup>Bu, Ph; <i>x</i> = 3 and R = Me) upon addition of excess halide. In addition to providing stable coordination complexes with Cl<sup>–</sup>, the [U­(NMe)<sub>2</sub>]<sup>2+</sup> cation also reacts with Br<sup>–</sup> to form stable [NEt<sub>4</sub>]<sub>2</sub>[U­(NMe)<sub>2</sub>Br<sub>4</sub>] complexes. These materials were used as a platform to compare electronic structure and bonding in [U­(NR)<sub>2</sub>]<sup>2+</sup> with [UO<sub>2</sub>]<sup>2+</sup>. Specifically, Cl K-edge X-ray absorption spectroscopy (XAS) and both ground-state and time-dependent hybrid density functional theory (DFT and TDDFT) were used to probe U–Cl bonding interactions in [PPh<sub>4</sub>]<sub>2</sub>[U­(N<sup><i>t</i></sup>Bu)<sub>2</sub>Cl<sub>4</sub>] and [PPh<sub>4</sub>]<sub>2</sub>[UO<sub>2</sub>Cl<sub>4</sub>]. The DFT and XAS results show the total amount of Cl 3p character mixed with the U 5f orbitals was roughly 7–10% per U–Cl bond for both compounds, which shows that moving from oxo to imido has little effect on orbital mixing between the U 5f and equatorial Cl 3p orbitals. The results are presented in the context of recent Cl K-edge XAS and DFT studies on other hexavalent uranium chloride systems with fewer oxo or imido ligands

    Tetrahalide Complexes of the [U(NR)<sub>2</sub>]<sup>2+</sup> Ion: Synthesis, Theory, and Chlorine K‑Edge X‑ray Absorption Spectroscopy

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    Synthetic routes to salts containing uranium bis-imido tetrahalide anions [U­(NR)<sub>2</sub>X<sub>4</sub>]<sup>2–</sup> (X = Cl<sup>–</sup>, Br<sup>–</sup>) and non-coordinating NEt<sub>4</sub><sup>+</sup> and PPh<sub>4</sub><sup>+</sup> countercations are reported. In general, these compounds can be prepared from U(NR)<sub>2</sub>I<sub>2</sub>(THF)<sub><i>x</i></sub> (<i>x</i> = 2 and R = <sup><i>t</i></sup>Bu, Ph; <i>x</i> = 3 and R = Me) upon addition of excess halide. In addition to providing stable coordination complexes with Cl<sup>–</sup>, the [U­(NMe)<sub>2</sub>]<sup>2+</sup> cation also reacts with Br<sup>–</sup> to form stable [NEt<sub>4</sub>]<sub>2</sub>[U­(NMe)<sub>2</sub>Br<sub>4</sub>] complexes. These materials were used as a platform to compare electronic structure and bonding in [U­(NR)<sub>2</sub>]<sup>2+</sup> with [UO<sub>2</sub>]<sup>2+</sup>. Specifically, Cl K-edge X-ray absorption spectroscopy (XAS) and both ground-state and time-dependent hybrid density functional theory (DFT and TDDFT) were used to probe U–Cl bonding interactions in [PPh<sub>4</sub>]<sub>2</sub>[U­(N<sup><i>t</i></sup>Bu)<sub>2</sub>Cl<sub>4</sub>] and [PPh<sub>4</sub>]<sub>2</sub>[UO<sub>2</sub>Cl<sub>4</sub>]. The DFT and XAS results show the total amount of Cl 3p character mixed with the U 5f orbitals was roughly 7–10% per U–Cl bond for both compounds, which shows that moving from oxo to imido has little effect on orbital mixing between the U 5f and equatorial Cl 3p orbitals. The results are presented in the context of recent Cl K-edge XAS and DFT studies on other hexavalent uranium chloride systems with fewer oxo or imido ligands

    Determining Relative f and d Orbital Contributions to M–Cl Covalency in MCl<sub>6</sub><sup>2–</sup> (M = Ti, Zr, Hf, U) and UOCl<sub>5</sub><sup>–</sup> Using Cl K-Edge X‑ray Absorption Spectroscopy and Time-Dependent Density Functional Theory

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    Chlorine K-edge X-ray absorption spectroscopy (XAS) and ground-state and time-dependent hybrid density functional theory (DFT) were used to probe the electronic structures of <i>O</i><sub><i>h</i></sub>-MCl<sub>6</sub><sup>2–</sup> (M = Ti, Zr, Hf, U) and <i>C</i><sub>4<i>v</i></sub>-UOCl<sub>5</sub><sup>–</sup>, and to determine the relative contributions of valence 3d, 4d, 5d, 6d, and 5f orbitals in M–Cl bonding. Spectral interpretations were guided by time-dependent DFT calculated transition energies and oscillator strengths, which agree well with the experimental XAS spectra. The data provide new spectroscopic evidence for the involvement of both 5f and 6d orbitals in actinide–ligand bonding in UCl<sub>6</sub><sup>2–</sup>. For the MCl<sub>6</sub><sup>2–</sup>, where transitions into d orbitals of <i>t</i><sub>2<i>g</i></sub> symmetry are spectroscopically resolved for all four complexes, the experimentally determined Cl 3p character per M–Cl bond increases from 8.3(4)% (TiCl<sub>6</sub><sup>2–</sup>) to 10.3(5)% (ZrCl<sub>6</sub><sup>2–</sup>), 12(1)% (HfCl<sub>6</sub><sup>2–</sup>), and 18(1)% (UCl<sub>6</sub><sup>2–</sup>). Chlorine K-edge XAS spectra of UOCl<sub>5</sub><sup>–</sup> provide additional insights into the transition assignments by lowering the symmetry to <i>C</i><sub>4<i>v</i></sub>, where five pre-edge transitions into both 5f and 6d orbitals are observed. For UCl<sub>6</sub><sup>2–</sup>, the XAS data suggest that orbital mixing associated with the U 5f orbitals is considerably lower than that of the U 6d orbitals. For both UCl<sub>6</sub><sup>2–</sup> and UOCl<sub>5</sub><sup>–</sup>, the ground-state DFT calculations predict a larger 5f contribution to bonding than is determined experimentally. These findings are discussed in the context of conventional theories of covalent bonding for d- and f-block metal complexes
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