Tetraruthenium Macrocycles with Laterally Extended Bis(alkenyl)quinoxaline Ligands and Their F4TCNQ•− Salts

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: In: Inorganics ; 10 (2022), 6. - 82. - MDPI. - eISSN 2304-6740

Event: Veröffentlichung

(where): Konstanz

(who): KOPS Universität Konstanz

(when): 2022

Creator: Das, Rajorshi
Linseis, Michael A.
Senft, Laura
Ivanović-Burmazović, Ivana
Winter, Rainer F.

URN: urn:nbn:de:bsz:352-2-scqv61bb2h2m7

Rights: Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:28 AM CEST

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Associated

Das, Rajorshi
Linseis, Michael A.
Senft, Laura
Ivanović-Burmazović, Ivana
Winter, Rainer F.
KOPS Universität Konstanz

Time of origin

2022

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Tetraruthenium Macrocycles with Laterally Extended Bis(alkenyl)quinoxaline Ligands and Their F<sub>4</sub>TCNQ<sup>•−</sup> Salts

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Time of origin

Other Objects (12)

Ferro-ferri-holmquistite, <italic>□</italic>Li<sub>2</sub>(Fe<sup>2+</sup><sub>3</sub>Fe<sup>3+</sup><sub>2</sub>) Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, Fe<sup>2+</sup>Fe<sup>3+</sup> analogue of holmquistite, from the Iwagi islet, Ehime, Japan

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X<sup>3</sup>Σ<sup>−</sup><sub>g</sub>)  →  O (<sup>3</sup>P) + PO (X<sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X<sup>2</sup>A<sub>1</sub>): implications for atmospheric modelling

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Igelströmite, Fe<sup>3+</sup>(Sb<sup>3+</sup>Pb<sup>2+</sup>) O<sub>4</sub>, and manganoschafarzikite, Mn<sup>2+</sup>Sb<sup>3+</sup><sub>2</sub>O<sub>4</sub>, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

Rotherkopfite, KNa<sub>2</sub>(Fe<sup>2+</sup><sub>2.5</sub>Ti<sup>4+</sup><sub>1.5</sub>) Fe<sup>2+</sup>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

Inter-comparison of online and offline methods for measuring ambient heavy and trace elements and water-soluble inorganic ions (NO<sub>3</sub><sup>−</sup>, SO<sub>4</sub><sup>2−</sup>, NH<sub>4</sub><sup>+</sup>, and Cl<sup>−</sup>) in PM<sub>2.5</sub> over a heavily polluted megacity, Delhi

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Igelströmite, Fe<sup>3+</sup>(Sb<sup>3+</sup>Pb<sup>2+</sup>) O<sub>4</sub>, and manganoschafarzikite, Mn<sup>2+</sup>Sb<sup>3+</sup><sub>2</sub>O<sub>4</sub>, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

Rotherkopfite, KNa<sub>2</sub>(Fe<sup>2+</sup><sub>2.5</sub>Ti<sup>4+</sup><sub>1.5</sub>) Fe<sup>2+</sup>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

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<sup>1</sup>H enhanced <sup>103</sup>Rh NMR spectroscopy and relaxometry of Rh (acac)<sub>3</sub> in solution

Ferro-ferri-holmquistite, <italic>□</italic>Li<sub>2</sub>(Fe<sup>2+</sup><sub>3</sub>Fe<sup>3+</sup><sub>2</sub>) Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, Fe<sup>2+</sup>Fe<sup>3+</sup> analogue of holmquistite, from the Iwagi islet, Ehime, Japan

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X<sup>3</sup>Σ<sup>−</sup><sub>g</sub>)  →  O (<sup>3</sup>P) + PO (X<sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X<sup>2</sup>A<sub>1</sub>): implications for atmospheric modelling

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Igelströmite, Fe<sup>3+</sup>(Sb<sup>3+</sup>Pb<sup>2+</sup>) O<sub>4</sub>, and manganoschafarzikite, Mn<sup>2+</sup>Sb<sup>3+</sup><sub>2</sub>O<sub>4</sub>, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

Rotherkopfite, KNa<sub>2</sub>(Fe<sup>2+</sup><sub>2.5</sub>Ti<sup>4+</sup><sub>1.5</sub>) Fe<sup>2+</sup>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

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Inter-comparison of online and offline methods for measuring ambient heavy and trace elements and water-soluble inorganic ions (NO<sub>3</sub><sup>−</sup>, SO<sub>4</sub><sup>2−</sup>, NH<sub>4</sub><sup>+</sup> and Cl<sup>−</sup>) in PM<sub>2.5</sub> over a heavily polluted megacity, Delhi

<sup>1</sup>H enhanced <sup>103</sup>Rh NMR spectroscopy and relaxometry of Rh (acac)<sub>3</sub> in solution

Tetraruthenium Macrocycles with Laterally Extended Bis(alkenyl)quinoxaline Ligands and Their F<sub>4</sub>TCNQ<sup>•−</sup> Salts

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Other Objects (12)

Ferro-ferri-holmquistite, <italic>□</italic>Li<sub>2</sub>(Fe<sup>2+</sup><sub>3</sub>Fe<sup>3+</sup><sub>2</sub>) Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, Fe<sup>2+</sup>Fe<sup>3+</sup> analogue of holmquistite, from the Iwagi islet, Ehime, Japan

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Igelströmite, Fe<sup>3+</sup>(Sb<sup>3+</sup>Pb<sup>2+</sup>) O<sub>4</sub>, and manganoschafarzikite, Mn<sup>2+</sup>Sb<sup>3+</sup><sub>2</sub>O<sub>4</sub>, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

Rotherkopfite, KNa<sub>2</sub>(Fe<sup>2+</sup><sub>2.5</sub>Ti<sup>4+</sup><sub>1.5</sub>) Fe<sup>2+</sup>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

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<sup>1</sup>H enhanced <sup>103</sup>Rh NMR spectroscopy and relaxometry of Rh (acac)<sub>3</sub> in solution

Ferro-ferri-holmquistite, <italic>□</italic>Li<sub>2</sub>(Fe<sup>2+</sup><sub>3</sub>Fe<sup>3+</sup><sub>2</sub>) Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, Fe<sup>2+</sup>Fe<sup>3+</sup> analogue of holmquistite, from the Iwagi islet, Ehime, Japan

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Igelströmite, Fe<sup>3+</sup>(Sb<sup>3+</sup>Pb<sup>2+</sup>) O<sub>4</sub>, and manganoschafarzikite, Mn<sup>2+</sup>Sb<sup>3+</sup><sub>2</sub>O<sub>4</sub>, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

Rotherkopfite, KNa<sub>2</sub>(Fe<sup>2+</sup><sub>2.5</sub>Ti<sup>4+</sup><sub>1.5</sub>) Fe<sup>2+</sup>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

Inter-comparison of online and offline methods for measuring ambient heavy and trace elements and water-soluble inorganic ions (NO<sub>3</sub><sup>−</sup>, SO<sub>4</sub><sup>2−</sup>, NH<sub>4</sub><sup>+</sup>, and Cl<sup>−</sup>) in PM<sub>2.5</sub> over a heavily polluted megacity, Delhi

Quantification of fossil fuel CO<sub>2</sub> from combined CO, &delta;<sup>13</sup>CO<sub>2</sub> and &Delta;<sup>14</sup>CO<sub>2</sub> observations

Solid-state <sup>1</sup>H spin polarimetry by <sup>13</sup>CH<sub>3</sub> nuclear magnetic resonance

<sup>1</sup>H enhanced <sup>103</sup>Rh NMR spectroscopy and relaxometry of Rh (acac)<sub>3</sub> in solution

Ferro-ferri-holmquistite, <italic>□</italic>Li<sub>2</sub>(Fe<sup>2+</sup><sub>3</sub>Fe<sup>3+</sup><sub>2</sub>) Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, Fe<sup>2+</sup>Fe<sup>3+</sup> analogue of holmquistite, from the Iwagi islet, Ehime, Japan

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Igelströmite, Fe<sup>3+</sup>(Sb<sup>3+</sup>Pb<sup>2+</sup>) O<sub>4</sub>, and manganoschafarzikite, Mn<sup>2+</sup>Sb<sup>3+</sup><sub>2</sub>O<sub>4</sub>, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

Rotherkopfite, KNa<sub>2</sub>(Fe<sup>2+</sup><sub>2.5</sub>Ti<sup>4+</sup><sub>1.5</sub>) Fe<sup>2+</sup>(Si<sub>4</sub>O<sub>12</sub>)<sub>2</sub>, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

Inter-comparison of online and offline methods for measuring ambient heavy and trace elements and water-soluble inorganic ions (NO<sub>3</sub><sup>−</sup>, SO<sub>4</sub><sup>2−</sup>, NH<sub>4</sub><sup>+</sup>, and Cl<sup>−</sup>) in PM<sub>2.5</sub> over a heavily polluted megacity, Delhi

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<sup>1</sup>H enhanced <sup>103</sup>Rh NMR spectroscopy and relaxometry of Rh (acac)<sub>3</sub> in solution

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Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Quantification of fossil fuel CO<sub>2</sub> from combined CO, δ<sup>13</sup>CO<sub>2</sub> and Δ<sup>14</sup>CO<sub>2</sub> observations

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Quantification of fossil fuel CO<sub>2</sub> from combined CO, δ<sup>13</sup>CO<sub>2</sub> and Δ<sup>14</sup>CO<sub>2</sub> observations

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Quantification of fossil fuel CO<sub>2</sub> from combined CO, δ<sup>13</sup>CO<sub>2</sub> and Δ<sup>14</sup>CO<sub>2</sub> observations