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

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Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: Rhizodeposition efficiency of pearl millet genotypes assessed on short growing period by carbon isotopes (δ¹³C and F¹⁴C) ; day:28 ; month:09 ; year:2021 ; pages:1-15 ; extent:15
Soil discussions ; (28.09.2021), 1-15 (gesamt 15)

Creator: Ndour, Papa Mamadou Sitor
Hatté, Christine
Achouak, Wafa
Heulin, Thierry
Cournac, Laurent

DOI: 10.5194/soil-2021-108

URN: urn:nbn:de:101:1-2021093005165784999328

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

Last update: 15.08.2025, 7:24 AM CEST

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Ndour, Papa Mamadou Sitor
Hatté, Christine
Achouak, Wafa
Heulin, Thierry
Cournac, Laurent

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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)

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s - sup

Rhenus sup.

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)

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Other Objects (12)

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s - sup

Rhenus sup.

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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

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

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

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