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Amaefule's units; S. sub-flow units *Capillary pressure samples.
Furthermore, the coupling term ξ k ( m ) means that pressure samples at subregion boundaries are exchanged between neighboring clusters in order to compute the finite differences.
Furthermore, Figs. 13 and 14 present plots of irreducible water saturation versus corresponding FZI values from ten (10) mercury injection capillary pressure samples obtained from the study area.
The off-diagonals of Φ12 are extremely sparsely populated; in fact, (26) contains only few non-zero terms corresponding to adjacent pressure samples and the change of sources from one to another cluster.
In order to compute the latter, only elements of x k [ l, m ′ ] that correspond to pressure samples from the boundaries of adjacent subregions are exchanged, and in the event of source hopping from one to another cluster, a message is sent.
where x k = x 1 k x 2 k ⋯ x L k T denotes an observation vector composed of the pressure samples at each sensor at a frequency corresponding to the wavenumber k. v k = v 1 k v 2 k ⋯ v L k T is a noise vector, and s F k = s 1 k s 2 k ⋯ s D 1 k T and s N k = s D 1 + 1 k s D 1 + 2 k ⋯ s D k T are far-field and near-field source signals, respectively.
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A multi-channel pressure sampling system and a high-resolution digital CCD camera were employed for experimental investigations.
The influence of the applied pressure, sample volume, mechanical work, and density of the carbons was investigated.
With the availability of a high pressure sample gas at the hydrogen refueling stations, the device uses only a pressure sequence to enrich the impurities without need of a temperature cycle.
First, shear modulus of the reinforced soil was assumed to be a nonlinear function of multiple variables such as contents of short fiber and lime powder, confining pressure, sample-aging period as well as shear strain.
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