Iron and zinc isotope fractionation during uptake and translocation in rice (Oryza sativa) grown in oxic and anoxic soils.

This study investigated zinc and iron isotope fractionation in rice grown to maturity in anaerobic and aerobic soils under greenhouse conditions

Abstract

Stable isotope fractionation is emerging quickly as a powerful novel technique to study metal uptake and translocation in plants. Fundamental to this development is a thorough understanding of the processes that lead to isotope fractionation under differing environmental conditions. In this study, we investigated Zn and Fe isotope fractionation in rice grown to maturity in anaerobic and aerobic soils under greenhouse conditions.

This is a publication arising from the Sustainable Crop production for International Development (SCPRID) programme.

Citation

Arnold T, Markovic T, Kirk G, Schönbächler M, Rehkämper M, Zhao F, Weiss D (2015). Iron and zinc isotope fractionation during uptake and translocation in rice (Oryza sativa) grown in oxic and anoxic soils. C R Geosci. 347:397-404.

Iron and zinc isotope fractionation during uptake and translocation in rice (Oryza sativa) grown in oxic and anoxic soils

Published 2 July 2015