Calibration of Hydroxyacetonitrile (HOCH2CN) and Methyl isocyanate (CH3NCO) Isomers using I- Chemical Ionization Mass Spectrometry (CIMS)

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Calibration of Hydroxyacetonitrile (HOCH₂CN) and Methyl isocyanate (CH₃NCO) Isomers using I^- Chemical Ionization Mass Spectrometry (CIMS) ; day:21 ; month:06 ; year:2024 ; pages:1-13 ; extent:13
Atmospheric measurement techniques discussions ; (21.06.2024), 1-13 (gesamt 13)

Creator: Finewax, Zachary
Chattopadhyay, Aparajeo
Neuman, J. Andrew
Roberts, James
Burkholder, James

DOI: 10.5194/amt-2024-94

URN: urn:nbn:de:101:1-2408051559016.472520630057

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 14.08.2025, 10:48 AM CEST

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Finewax, Zachary
Chattopadhyay, Aparajeo
Neuman, J. Andrew
Roberts, James
Burkholder, James

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Calibration of Hydroxyacetonitrile (HOCH<sub>2</sub>CN) and Methyl isocyanate (CH<sub>3</sub>NCO) Isomers using I<sup>-</sup> Chemical Ionization Mass Spectrometry (CIMS)

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Calibration of Hydroxyacetonitrile (HOCH<sub>2</sub>CN) and Methyl isocyanate (CH<sub>3</sub>NCO) Isomers using I<sup>-</sup> Chemical Ionization Mass Spectrometry (CIMS)

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How do Cl concentrations matter for the simulation of CH<sub>4</sub> and <italic>δ</italic><sup>13</sup>C (CH<sub>4</sub>) and estimation of the CH<sub>4</sub> budget through atmospheric inversions?

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

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

Continuous CH<sub>4</sub> and <em>&delta;</em><sup>13</sup>CH<sub>4</sub> measurements in London demonstrate under-reported natural gas leakage

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

Manganrockbridgeite, Mn<sup>2+</sup><sub>2</sub>Fe<sup>3+</sup><sub>3</sub>(PO<sub>4</sub>)<sub>3</sub>(OH)<sub>4</sub>(H<sub>2</sub>O), a new member of the rockbridgeite group, from the Hagendorf-Süd pegmatite, Oberpfalz, Bavaria

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

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

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How do Cl concentrations matter for simulating CH<sub>4</sub>, <em>δ</em><sup>13</sup>C (CH<sub>4</sub>) and estimating CH<sub>4</sub> budget through atmospheric inversions?

Continuous CH<sub>4</sub> and <em>δ</em><sup>13</sup>CH<sub>4</sub> measurements in London demonstrate under-reported natural gas leakage

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

How do Cl concentrations matter for simulating CH<sub>4</sub>, <em>δ</em><sup>13</sup>C (CH<sub>4</sub>) and estimating CH<sub>4</sub> budget through atmospheric inversions?

Continuous CH<sub>4</sub> and <em>δ</em><sup>13</sup>CH<sub>4</sub> measurements in London demonstrate under-reported natural gas leakage

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

How do Cl concentrations matter for simulating CH<sub>4</sub>, <em>δ</em><sup>13</sup>C (CH<sub>4</sub>) and estimating CH<sub>4</sub> budget through atmospheric inversions?

Continuous CH<sub>4</sub> and <em>δ</em><sup>13</sup>CH<sub>4</sub> measurements in London demonstrate under-reported natural gas leakage

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