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The obtained age data were calibrated using the OxCal 4.2 program (Ramsey 2009) and the calibration curve IntCal13 (Reimer et al. 2013).
Hyperspectral data were calibrated using a white and a black reference image.
To further confirm the elemental compositions and the electronic state, the porous- and hollow-structured LiNb3O8 powders are analyzed by XPS, as shown in Fig. 4. The XPS data were calibrated using C 1s as a reference with the binding energy at 284.6 eV.
Raw image data were calibrated using the sensitivity factor (eq 3) to give 2-D planar spatial arrays of tracer concentration data at 30 s intervals for up to 3 h during and after transit of the main mass of 99mTc through the flow cell.
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Heat flux data was calibrated using calibration curves provided by the manufacturer.
The data was calibrated using C0, C1, C2 parameters before processing.
The fluorescence data was calibrated using Γ̂ P λ m / P λ x, where P λ x and P λ m were the measured powers at λ x and λ m, respectively.
If virtual sensors were calibrated using laboratory data, the amount of the calibration data could be minimized using design of experiment techniques.
Models were calibrated using data for grass and native prairie conditions, and future scenarios were simulated to guide design and management actions.
In both techniques, samples were calibrated using data collected in a well-characterized methane/air diffusion flame supported on a Wolfhard-Parker slot burner.
The direct reading photometric instruments were calibrated using data from co-located gravimetric samplers [ 8].
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