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)

zu Verbundenen Objekten

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
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)

Urheber
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
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
14.08.2025, 10:48 MESZ

Datenpartner

Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Original beim Datenpartner anzeigen

Beteiligte

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

Ähnliche Objekte (12)

How do Cl concentrations matter for simulating CH4, &delta;13C (CH4) and estimating CH4 budget through atmospheric inversions?

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

How do Cl concentrations matter for the simulation of CH4 and δ13C (CH4) and estimation of the CH4 budget through atmospheric inversions?

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, □Li2(Fe2+3Fe3+2) Si8O22(OH)2, Fe2+Fe3+ analogue of holmquistite, from the Iwagi islet, Ehime, Japan

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

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH4+–Na+–Ca2+–K+–Mg2+–SO42−–NO3−–Cl−–H2O system based on ISORROPIA II

HETerogeneous vectorized or Parallel (HETPv1.0): an updated inorganic heterogeneous chemistry solver for the metastable-state NH<sub>4</sub><sup>+</sup>–Na<sup>+</sup>–Ca<sup>2+</sup>–K<sup>+</sup>–Mg<sup>2+</sup>–SO<sub>4</sub><sup>2−</sup>–NO<sub>3</sub><sup>−</sup>–Cl<sup>−</sup>–H<sub>2</sub>O system based on ISORROPIA II

Rotherkopfite, KNa2(Fe2+2.5Ti4+1.5) Fe2+(Si4O12)2, a new neptunite-group mineral without essential lithium, from Rother Kopf, Eifel volcanic fields, Germany

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 CH4 and &delta;13CH4 measurements in London demonstrate under-reported natural gas leakage

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 CO2 from combined CO, &delta;13CO2 and &Delta;14CO2 observations

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

Reaction dynamics of P (4S)&thinsp;+&thinsp;O2(X3Σ−g)&thinsp; → &thinsp;O (3P)&thinsp;+&thinsp;PO (X2Π) on a global CHIPR potential energy surface of PO2(X2A1): implications for atmospheric modelling

Reaction dynamics of P (<sup>4</sup>S)&thinsp;+&thinsp;O<sub>2</sub>(X<sup>3</sup>Σ<sup>−</sup><sub>g</sub>)&thinsp; → &thinsp;O (<sup>3</sup>P)&thinsp;+&thinsp;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

Manganrockbridgeite, Mn2+2Fe3+3(PO4)3(OH)4(H2O), a new member of the rockbridgeite group, from the Hagendorf-Süd pegmatite, Oberpfalz, Bavaria

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 (NO3−, SO42−, NH4+, and Cl−) in PM2.5 over a heavily polluted megacity, Delhi

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 (4S) + O2(X 3&Sigma;-) &rarr; O (3P) + PO (X 2&Pi;) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

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, Fe3+(Sb3+Pb2+) O4, and manganoschafarzikite, Mn2+Sb3+2O4, two new members of the newly established minium group, from the Långban Mn–Fe deposit, Värmland, Sweden

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

Verbundene Objekte