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Briefly, it followed from examination of the class prediction scores by the OPLS-DA classifier (Fig. 3b) that the 10 samples measured in both batch measurements (or batch 1&2 samples) are spread over class 2 and 3 (the word batch here referring to a sample collection set).
Surface charge for nZnO and the nZnO – FBSdried NP samples, measured in nanopure water using electrophoretic measurements, was found to be 43.8 ± 0.55 mV and −11.8 ± 0.39 mV, respectively.
Given that the majority of the samples measured in the current study did not have measurable levels of uranium radionuclides, it is of value to estimate the upper limits for their presence in these STPs based on the current analytical capabilities.
These results confirm that it is possible to reliably compute the geometrical characteristic w k,xy of each channel using a single known sample, thus allowing extracting the absolute diffusion coefficients for unknown samples measured in different experiments, independently of the channel used for the measurement.
Samples measured in EDTA plasma.
Blood dosimetry may be derived from samples measured in a well counter.
Figure 6 Directional consistency of the sequoia samples measured in Pruhonice Paleomagnetic Laboratory.
Specimens of selected samples measured in the DSC were metallized in a thermal evaporator.
The models can be used for predictions when we introduce new data (new samples measured in the same way).
In order to obtain the systematic offsets, the signal differences were calculated for all samples measured in this work.
RMR, Q, RMi and GSI were determined by using field data and mechanical properties of intact rock samples, measured in the laboratory.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com