Coupling Langmuir with Michaelis-Menten-A practical alternative to estimate Se content in rice?

Authors:
Alexandra K Nothstein
Alexandra K Nothstein
Institute of Applied Geosciences (AGW)
Elisabeth Eiche
Elisabeth Eiche
Institute of Applied Geosciences
Michael Riemann
Michael Riemann
Karlsruhe Institute of Technology
Germany
Peter Nick
Peter Nick
Karlsruhe Institute of Technology
Germany
Philipp Maier
Philipp Maier
University of Freiburg
Germany
Thomas Neumann
Thomas Neumann
Justus-Liebig-University of Giessen
Germany

PLoS One 2019 19;14(4):e0214219. Epub 2019 Apr 19.

Technical University of Berlin (TUB), Institute of Applied Geosciences, Berlin, Germany.

Selenium plays an important, but vastly neglected role in human nutrition with a narrow gap between dietary deficiency and toxicity. For a potential biofortification of food with Se, as well as for toxicity-risk assessment in sites contaminated by Se, modelling of local and global Se cycling is essential. As bioavailability of Se for rice plants depends on the speciation of Se and the resulting interactions with mineral surfaces as well as the interaction with Se uptake mechanisms in plants, resulting plant Se content is complex to model. Unfortunately, simple experimental models to estimate Se uptake into plants from substrates have been lacking. Therefore, a mass balance of Se transfer between lithosphere (represented by kaolinite), hydrosphere (represented by a controlled nutrient solution), and biosphere (represented by rice plants) has been established. In a controlled, closed, lab-scale system, rice plants were grown hydroponically in nutrient solution supplemented with 0-10 000 μg L-1 Se of either selenate or selenite. Furthermore, in a series of batch experiments, adsorption and desorption were studied for selenate and selenite in competition with each of the major nutrient oxy-anions, nitrate, sulfate and phosphate. In a third step, the hydroponical plants experiments were coupled with sorption experiments to study synergy effects. These data were used to develop a mass balance fitting model of Se uptake and partitioning. Adsorption was well-described by Langmuir isotherms, despite competing anions, however, a certain percentage of Se always remained bio-unavailable to the plant. Uptake of selenate or selenite by transporters into the rice plant was fitted with the non-time differentiated Michaelis-Menten equation. Subsequent sequestration of Se to the shoot was better described using a substrate-inhibited variation of the Michaelis-Menten equation. These fitted parameters were then integrated into a mass balance model of Se transfer.

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http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0214219PLOS
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC6474650PMC
April 2019
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