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Residual phase difference.
We use the residual phase changes as the crustal deformation data associated with the inland earthquakes.
The residual phase compensation is implemented after a fast Fourier transform (FFT) in range.
This residual phase can be removed by increasing the calcination temperature.
The residual phase, containing less fringes, is more easily unwrapped than the original interferogram.
The residual phase contamination generates the glitches around the Bragg peaks for the inaccurate estimation of the contamination frequency.
Concentrations of the analyzed trace elements in the extractions, residual phase, and total sediment samples are given in Table II.
An interwell field test to determine residual phase and dissolution trapping of CO2 is being designed at Heletz, Israel.
Besides, the effect of changing the capillary and viscous forces and interfacial tension on the residual phase saturations were characterized.
Trace elements in the residual phase are strongly bound, or held, within mineral crystal structure, and thus are almost impossible to be mobilized under the natural conditions.
N T is also used to correlate changes in the residual phase saturations during immiscible displacement and is graphically represented as capillary desaturation curve (CDC).
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