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Studies with pearl millet have shown that application of P increased the concentrations of PA in the grain between 25 and 29%, increased the PA:Zn molar ratio and decreased Zn concentrations between 6 and 11% due to greater P uptake and a dilution of Zn by the large yield increases after P application (Buerkert et al. 1998).
Because the sample is mainly composed of LiFePO4 phase, as we know, the reason for the decrease and increase of grain area and height are due to phase transformation of the grain between LiFePO4 and FePO4 during the charge and discharge processes.
Among these genes, we found one differentially regulated potassium transporter and two sulfate transporters, which are potentially related to the differences identified in K and S concentrations in the grain between genotypes (Additional file 1: Table S1).
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Grain sizes ranged between 0.125 and 1.00 mm with the majority of the grains between 0.250 and 0.500 mm.
In this study, we employed PETIS in our two objectives: to realize direct observation of Cd uptake by the roots in the culture solution, and to characterize clearly the differences in Cd dynamics from the culture to the grains between the high- and low-Cd accumulating cultivars.
Using the PETIS, we made the first direct observation of Cd uptake by the roots in the culture solution, characterized the successive transport processes in the root tissues, and described the differences in real-time Cd dynamics from the roots to the grains between the high- and low-Cd accumulating rice cultivars.
Initial analysis suggests that the failure probably occurred at the "step" in the fuel grain, between the star-shaped main body and the round tail end.
The errors of the grain size between the experiment and simulation are less than 20%.
The largest pore size, 37.1 nm, is at the grain boundary between silica nanoparticles.
(c) MNBs that captured fine particles were also located on the grain boundary between ice crystallites.
Significantly smaller mafic minerals exist in the grain boundaries between igneous plagioclase grains with albite twinning textures.
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