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

zu Verbundenen Objekten

Standort: Deutsche Nationalbibliothek Frankfurt am Main

Umfang: Online-Ressource

Sprache: Englisch

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

Ereignis: Veröffentlichung

(wo): Konstanz

(wer): KOPS Universität Konstanz

(wann): 2022

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

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

Rechteinformation: Der Zugriff auf das Objekt ist unbeschränkt möglich.

Letzte Aktualisierung: 15.08.2025, 07:28 MESZ

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Beteiligte

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

Entstanden

2022

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

Datenpartner

Beteiligte

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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

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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

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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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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