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Hr. Johann Arnd Weil. Gen. Sup. des Fürstenh. Lüneb.

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Digitalisierung: Dresden SLUB, ZB

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Bibliographic citation: Arndt, Johann. - Johann Arnds, Weil. Gen. Sup. des Hertzogth. Lüneb. Paradieß-Gärtlein, Voller Christlichen Tugenden, Wie solche durch geistreiche Gebete in die Seele zu pflantzen : Worzu itzo kommen 1. Eilf Wunder-Geschichte ... 2. Bernhardi völlig verteutschtes Jubel- und Jesus-Lied. 3. Ein dreyfaches Register ... 4. Morgen- und Abend-Gebete auf alle Tage in der Wochen

Sponsorship: Deutsche Forschungsgemeinschaft

Last update: 09.10.2025, 2:20 PM CEST

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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)

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)

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

Verzeichnung

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Karte

Rhenus sup.

Hochschulschrift

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

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

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

Verzeichnung

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Karte

Rhenus sup.

Hochschulschrift

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

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

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

Verzeichnung

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Karte

Rhenus sup.

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Hr. Johann Arnd Weil. Gen. Sup. des Fürstenh. Lüneb.

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Other Objects (12)

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>)

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)

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

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Rhenus sup.

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>)

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)

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

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Rhenus sup.

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>)

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)

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

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Rhenus sup.

Hr. Johann Arnd Weil. Gen. Sup. des Fürstenh. Lüneb.

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Other Objects (12)

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>)

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)

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

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Rhenus sup.

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>)

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)

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

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Rhenus sup.

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>)

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)

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

Hr. Christoph Weil, Brinksitzer zu Engelnstedt ./. Hr. Andreas Weil, den Kotsasse zu Bleckenstedt wegen Abfindung

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

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

Rhenus sup.

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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

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