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The calcium and iron distribution maps show a fifteenth-century page from a calender (Fig. 5).
After the experiment, the iron distribution within a natural wetland ecosystem was quantitatively observed.
The increase of the activation temperature up to 800 °C favors a more homogeneous iron distribution through the carbon particles.
When comparing the painting with the iron distribution map, we can see that the foreground is continuous behind the shapes of the easel legs.
What the iron distribution does show is a cursive script from the sixteenth century that does not follow the shape of two columns.
In the iron distribution map only the upper text is visible, again difficult to decipher because of the overlap of the recto and verso of the manuscript.
Fig. 7 Iron distribution on the surface of the cement mortar containing different ratios of nano-Fe3O4 - 1 wt%(a); 2 wt%(b); 3 wt%(c); 4 wt%(d) and 5 wt%(e).
The iron distribution map in Fig. 6 clearly shows the handwritten text and even though the text overlaps slightly with text from the backside of the fragment it can still be easily read: "Mijn mond sal voertkundigen dijn lof.
More than 10 years back, I talked to a US scientist just back from an iron fertilisation experiment who explained that personally, he wasn't interested in geoengineering; really, he wanted to answer more academic questions about iron distribution in the water and derive answers about what the oceans used to look like in the past.
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The iron (Fe) distribution map shows that Magritte used iron rich pigments to establish the initial general form of the cave.
Cellular iron homeostasis is controlled by iron uptake at the plasma membrane, eliciting balanced iron distributions among cellular compartments and iron export (Valerio, 2007; Zhang, 2014).
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