. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography 278 Donald J. P. Swift, John C. Ludwick, and W. Richard Boehmer PHI UNITS Figure 90. Grain-size distribution at a station. For simplicity a local admittance vector and retention vector are linear and complementary. Local input distribution 1 is uniform; the shape of the corresponding retained distribution, 1, is solely dependent on the action of local admittance vector and retention vector. Local input distribution 2 is an arbitrary positivel
. Collected reprints / Atlantic Oceanographic and Meteorological Laboratories [and] Pacific Oceanographic Laboratories. Oceanography 278 Donald J. P. Swift, John C. Ludwick, and W. Richard Boehmer PHI UNITS Figure 90. Grain-size distribution at a station. For simplicity a local admittance vector and retention vector are linear and complementary. Local input distribution 1 is uniform; the shape of the corresponding retained distribution, 1, is solely dependent on the action of local admittance vector and retention vector. Local input distribution 2 is an arbitrary positively skewed, bell-shaped distribution; the corresponding retained distribution, 2, is altered in skewness by the action of the local admittance vector and retention vector. The array of probabilities, pjn (1 — pjn), n = 1, 2, . . , 10, for a station does not necessarily indicate the form of a retained distribution, because what is retained is dependent also on shape of the local input distribution. If the local input is uniform, the array of probabilities referred to above gives the shape of the retained distribution. In general, the local input distribution is not uniform, and this causes a skewing of the form of the retained distribution. If I]n is the frequency of occurrence of grains of size n in the local input to station j, then R. = tjnlinOLZPjnl , n=l2 10 Y, tjnPjnV-Pjn) n = 1 is the frequency of grains of size n-in the retained distribution at station j. The local output from station j would usually be different than the local input to station j, because of the unequal partial removal of various grain-size classes. The retained grain-size frequency distribution is, in this context, comprised of two significant parts: a coarser-grained part; and a finer-grained part. The extreme of the coarser-grained part is comprised of those available grains whose 892. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readab
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