Pseudochannel

The best exposures of pseudochannels are at the Wilson Creek, Walnut Creek, Canyoun Creek, and Gerald Wash section localities. The features are restricted to the gray unit of the upper member and nearly all of the well-developed pseudochannels are in the gray facies and the gray sandstone.

The large pseudochannel seen in cross section in the center of the photograph is surrounded by a multitude of smaller pseudochannels.

This method requires that pseudochannel boundaries be located in the flow reach upstream from each of the openings to simulate the actual upstream boundaries of the single-opening constriction.

To determine the discharge, establish in the approach channel pseudochannel boundaries which divide the flow between openings. This procedure defines a separate approach channel for each individual opening.

As a result, multispectral orthorectified images were created, each containing the respective DEM as a separate pseudochannel.

For such potentials the imaginary part of the potential causes a loss of flux from the incident channel and plays a comparable role to the pseudochannel of the MEP.

In the first run, we assume unit incident flux in the pseudochannel ф₁, while in the second unit incident flux is assumed in ф₂.

Thus it is not necessary to use complex potentials to mimic the loss of flux from the first electronic channel. Since the pseudochannel is supposed to mimic the total effect of all excited electronic states, the flux associated with it should be compared to the whole electronically inelastic cross section.