Measurement report: Source apportionment of carbonaceous aerosol using dual-carbon isotopes (13C and 14C) and levoglucosan in three northern Chinese cities during 2018–2019

to related objects

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Measurement report: Source apportionment of carbonaceous aerosol using dual-carbon isotopes (¹³C and ¹⁴C) and levoglucosan in three northern Chinese cities during 2018–2019 ; day:17 ; month:12 ; year:2021 ; pages:1-55 ; extent:55
Atmospheric chemistry and physics / Discussions. Discussions ; (17.12.2021), 1-55 (gesamt 55)

Creator: Zhao, Huiyizhe
Niu, Zhenchuan
Zhou, Weijian
Wang, Sen
Feng, Xue
Wu, Shugang
Lu, Xuefeng
Du, Hua

DOI: 10.5194/acp-2021-916

URN: urn:nbn:de:101:1-2021122304321798546240

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

Last update: 15.08.2025, 7:36 AM CEST

Data provider

This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.

Show original at data provider

Associated

Zhao, Huiyizhe
Niu, Zhenchuan
Zhou, Weijian
Wang, Sen
Feng, Xue
Wu, Shugang
Lu, Xuefeng
Du, Hua

Other Objects (12)

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

Hochschulschrift

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

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 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 metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

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

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Insights into Protein Dynamics from 15N-1H HSQC

Insights into Protein Dynamics from 15N-1H HSQC

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Global simulation of dissolved 231Pa and 230Th in the ocean and the sedimentary 231Pa∕230Th ratios with the ocean general circulation model COCO ver4.0

Global simulation of dissolved 231Pa and 230Th in the ocean and the sedimentary 231Pa∕230Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (δ15N) and first quantification of oxygen isotope anomalies (Δ17O, δ18O) in atmospheric nitrogen dioxide

Measurement report: Nitrogen isotopes (<italic>δ</italic>15N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic>17O, <italic>δ</italic>18O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ13C and F14C)

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ13C and F14C)

Verzeichnung

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

Kapitel

s - sup

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Hochschulschrift

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

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 metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Insights into Protein Dynamics from 15N-1H HSQC

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Global simulation of dissolved 231Pa and 230Th in the ocean and the sedimentary 231Pa∕230Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic>15N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic>17O, <italic>δ</italic>18O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ13C and F14C)

Verzeichnung

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

Kapitel

s - sup

Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Hochschulschrift

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: FeII, CoII, NiII, CuII und CuII)

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 metastable state NH4+–Na+–Ca2+–K+–Mg2+–SO42––NO3––Cl– based on ISORROPIA II

Precise dating of deglacial Laptev Sea sediments via 14C and authigenic 10Be/9Be – assessing local 14C reservoir ages

Insights into Protein Dynamics from 15N-1H HSQC

Reaction dynamics of P (4S) + O2(X 3Σ-) → O (3P) + PO (X 2Π) on a global CHIPR potential energy surface of PO2(X 2A1): implication for atmospheric modelling

Global simulation of dissolved 231Pa and 230Th in the ocean and the sedimentary 231Pa∕230Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic>15N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic>17O, <italic>δ</italic>18O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ13C and F14C)

Verzeichnung

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

Kapitel

s - sup

Cultural heritage institutions wishing to register will find more information here.

Fields marked * need to be filled in.

Username*

Please enter your username

Email*

Please enter your email address

Please do not fill this field

First name

Last name

Password*

Please enter your password

Confirm password*

Please enter the same password

I have read the terms of use and the privacy policy for the collection of personal data and accept them. *

This field is required.

I would like to subscribe to the newsletter of the Deutsche Digitale Bibliothek. See newsletter subscription info.

Account created

Your "My DDB" account has been successfully created. Before you can log in to your account, you must click the confirmation link in the message we just sent to the email address you provided.

Germany's digital cultural heritage

Measurement report: Source apportionment of carbonaceous aerosol using dual-carbon isotopes (<sup>13</sup>C and <sup>14</sup>C) and levoglucosan in three northern Chinese cities during 2018–2019

Data provider

Associated

Other Objects (12)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

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

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic><sup>15</sup>N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic><sup>17</sup>O, <italic>δ</italic><sup>18</sup>O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ<sup>13</sup>C and F<sup>14</sup>C)

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

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

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic><sup>15</sup>N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic><sup>17</sup>O, <italic>δ</italic><sup>18</sup>O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ<sup>13</sup>C and F<sup>14</sup>C)

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

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

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic><sup>15</sup>N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic><sup>17</sup>O, <italic>δ</italic><sup>18</sup>O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ<sup>13</sup>C and F<sup>14</sup>C)

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Measurement report: Source apportionment of carbonaceous aerosol using dual-carbon isotopes (<sup>13</sup>C and <sup>14</sup>C) and levoglucosan in three northern Chinese cities during 2018&ndash;2019

Object Details

References and Relationships

Contributors, Places and Time

Further information

Data provider

Associated

Other Objects (12)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

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

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic><sup>15</sup>N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic><sup>17</sup>O, <italic>δ</italic><sup>18</sup>O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (&delta;<sup>13</sup>C and F<sup>14</sup>C)

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

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

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic><sup>15</sup>N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic><sup>17</sup>O, <italic>δ</italic><sup>18</sup>O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (&delta;<sup>13</sup>C and F<sup>14</sup>C)

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

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

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Measurement report: Nitrogen isotopes (<italic>δ</italic><sup>15</sup>N) and first quantification of oxygen isotope anomalies (<italic>Δ</italic><sup>17</sup>O, <italic>δ</italic><sup>18</sup>O) in atmospheric nitrogen dioxide

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (&delta;<sup>13</sup>C and F<sup>14</sup>C)

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Related objects

Reset password

Measurement report: Source apportionment of carbonaceous aerosol using dual-carbon isotopes (<sup>13</sup>C and <sup>14</sup>C) and levoglucosan in three northern Chinese cities during 2018–2019

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

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

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ<sup>13</sup>C and F<sup>14</sup>C)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

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

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ<sup>13</sup>C and F<sup>14</sup>C)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

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

Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ<sup>13</sup>C and F<sup>14</sup>C)