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Beáta Babka

Researcher at University of Debrecen

Publications -  9
Citations -  263

Beáta Babka is an academic researcher from University of Debrecen. The author has contributed to research in topics: Floodplain & Selenium. The author has an hindex of 6, co-authored 9 publications receiving 199 citations. Previous affiliations of Beáta Babka include Hungarian Academy of Sciences.

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Elemental, Nano-Sized (100-500 nm) Selenium Production by Probiotic Lactic Acid Bacteria

TL;DR: In these experiments, nano-size (100-500nm) elemental selenium is produced by using probiotic yogurt bacteria in a fermentation procedure and the laboratory technology of product purification and recovery from bacteria is developed.
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Accumulation of Red Elemental Selenium Nanoparticles and Their Biological Effects in Nicotinia Tabacum

TL;DR: The data clearly indicated that red nanoSe was taken up by tobacco callus cultures and rooted tobacco plantlets, and inhibited both callus growth and root regeneration totally in 265–530 μM concentrations.
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Changes in soil organic matter quality during sea-influenced marsh soil development at the North Sea coast

Marie Spohn, +2 more
- 01 Aug 2013 - 
TL;DR: In this article, the authors investigated how organic matter quality changes during initial soil development in salt marshes and found that organic carbon (OC) and nitrogen (N) contents increased significantly with decreasing inundation frequency at all sites, while inorganic carbon contents decreased.
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Dietary selenium augments sarcoplasmic calcium release and mechanical performance in mice.

TL;DR: Selenium supplementation augments calcium release from the sarcoplasmic reticulum thus improves skeletal muscle performance and is accompanied by the increased selenoprotein N expression in the muscles which could result in increased oxidative stress tolerance in case of long lasting contraction.
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Clustering oxbow lakes in the Upper-Tisza Region on the basis of stable isotope measurements

TL;DR: In this paper, the water addition in the oxbow lakes does not only take place through flooding; it is also likely that water can seep under the surface through the gravelled layers of the old riverbeds, and furthermore, precipitation also plays a role.