# Download Analyse numérique: exercises et problèmes corrigés by Héron Bernard, Issard-Roch Françoise, Picard Colette PDF

By Héron Bernard, Issard-Roch Françoise, Picard Colette

Heron, Issard-Roch, Picard. examine numerique (fr)(Dunod, 1999)(ISBN 2100043722)(C)(302s)

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Additional info for Analyse numérique: exercises et problèmes corrigés

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10460 ~ ~ I, rr... : ~IIf liT Results of Dipmeter Computation with High Depth Resolution. Reprinted by permission of the SPWLA from Kerzner (1983). 8 scribed earlier: matched elements should be of the same type and, if possible, of the same size. If there are no matches of the same size, then the next closest size is tried, but with a smaller coefficient of importance or confidence. The rule of noncrossing correlations is also present, but in this algorithm it takes a more complicated form, since all four curves (or more) are considered simultaneously.

In image processing, functions similar to activity are called differentiators or edge detectors. In many applications, edge detection is the first stage in the analysis. 5 can also be viewed as corresponding to edges - in this case, to boundaries between different depositional layers. As is known in log analysis, bed boundaries occur at or close to the inflection points on the logs. For smooth curves, these are also the points at which activity reaches a maximum. Because activity maximums correspond to points of the most rapid change in the log values, it is natural that they should occur where one layer meets another and the physical properties of the formation change most abruptly.

Errors of this type result in depth discrepancies between logs recorded with different tools. 1 Effect of the Formation Dip on Depth Errors. Reprinted by permission of the SPWLA from Zangwill (1982). different runs - for example, measuring updip in the formation on one run and downdip on another. The effect of the depth error depends on how the logs are going to be used. Fine investigation utilizing level-by-Ievel computation is certainly very sensitive to depth errors, and such modern techniques as crossplots are even more sensitive.