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Measured field properties included topography, soil texture, pre-application soil nitrate levels, and plant available soil water content.
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Using backcalculation analysis, in situ material properties can be backcalculated by the measured field data for appropriate analysis techniques.
The electrostatic induction current of the measured field induces an electric charge on the measuring plate.
The measured field of view is 32°.
Overall, the simulation results are consistent with measured field data.
Using the measured field map, the initial reconstruction function was generated.
Now, a signal is detected if the measured field strength exceeds the threshold.
The wind field, computed by unsteady and large eddy simulation (LES), agreed well with the measured field wind variations.
A comparison between the reconstructed field and the measured field in the M1 magnet of the separator COMBAS is given.
The underlying questions of these studies are whether the measured seepage can at least qualitatively be predicted either using measured field permeabilities or data generated using analytical formula.
Morphology and receptive field properties of VG3-ACs.
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