Publication

Uranium Isotopes Fingerprint Biotic Reduction

À propos
Confidentialité
Mentions légales

Graph Chatbot

Chattez avec Graph Search

Posez n’importe quelle question sur les cours, conférences, exercices, recherches, actualités, etc. de l’EPFL ou essayez les exemples de questions ci-dessous.

AVERTISSEMENT : Le chatbot Graph n'est pas programmé pour fournir des réponses explicites ou catégoriques à vos questions. Il transforme plutôt vos questions en demandes API qui sont distribuées aux différents services informatiques officiellement administrés par l'EPFL. Son but est uniquement de collecter et de recommander des références pertinentes à des contenus que vous pouvez explorer pour vous aider à répondre à vos questions.

Connectez-vous pour utiliser Chat avec Graph Search

Uranium Isotopes Fingerprint Biotic Reduction

Graph Chatbot

Chattez avec Graph Search

The isotopic signature of U(V) during bacterial reduction

Diagenetic isotope exchange in biocalcites for paleoclimate reconstruction

Mercury Isotope Fractionation during Dark Abiotic Reduction of Hg(II) by Dissolved, Surface-Bound, and Structural Fe(II)

Isotope Ratio - Discharge Relationships of Solutes Derived From Weathering Reactions

Rapid grain boundary diffusion in foraminifera tests biases paleotemperature records

Persistence of the isotopic signature of pentavalent uranium in magnetite

Phloem water isotopically different to xylem water: Potential causes and implications for ecohydrological tracing

Persistence of the isotopic signature of pentavalent uranium in magnetite

Active anaerobic methane oxidation and sulfur disproportionation in the deep terrestrial subsurface

Design of the 590 MeV proton beamline for the proposed TATTOOS isotope production target at PSI

Diagenetic isotope exchange in biocalcites for paleoclimate reconstruction

The isotopic signature of U(V) during bacterial reduction

Isotope Ratio - Discharge Relationships of Solutes Derived From Weathering Reactions

Rapid grain boundary diffusion in foraminifera tests biases paleotemperature records

Persistence of the isotopic signature of pentavalent uranium in magnetite

Phloem water isotopically different to xylem water: Potential causes and implications for ecohydrological tracing

Active anaerobic methane oxidation and sulfur disproportionation in the deep terrestrial subsurface

Design of the 590 MeV proton beamline for the proposed TATTOOS isotope production target at PSI

Mercury Isotope Fractionation during Dark Abiotic Reduction of Hg(II) by Dissolved, Surface-Bound, and Structural Fe(II)

Persistence of the isotopic signature of pentavalent uranium in magnetite