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The use of geologically realistic networks to predict the flow properties for a variety of porous media Predictive Pore-Scale Modelling of Multiphase Flow.

Автор:   Per V.
мягкая обложка
144 страниц
2009 год
Издательство:   Книга по Требованию
Цена:
2400 руб
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Описание:A state of the art pore-scale network model is developed for this purpose. Furthermore, the variation of these properties in the field, due to wettability trends and different pore structures, can now be predicted reliably. Flow properties for a variety of porous media can be predicted using pore-scale modelling with geologically realistic networks. More complex experimental data are subsequently investigated. By developing a methodology combining realistic network topology with network properties tuned to easily obtainable experimental data such as mercury injection capillary pressures, the flow properties for several porous media can successfully be predicted. The aim of this work is not simply to match experiments, but to use easily acquired data to predict difficult-to-measure properties. It combines topologically disordered networks that represent real systems with detailed displacement mechanisms for any sequence of water and oil flooding, and any wettability. The model is verified by successfully predicting experimental relative permeability from a well described water-wet Berea sandstone. This is initially applied to a water-wet sand pack.


Orthomol Immun Junior Сила иммунитета на страже Вашего ребенка Orthomol Immun Junior Сила иммунитета на страже Вашего ребенка

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A short history of nearly everything

We will travel great distances and pay small fortunes to see it in sunshine. And even though we know it is dangerous and drowns tens of thousands of people every year, we canБЂ™t wait to frolic in it. Because water is so ubiquitous we tend to overlook what an extraordinary substance it is. Almost nothing about it can be used to make reliable predictions about the properties of other liquids and vice versa. If you knew nothing of water and based your assumptions on the behavior of compounds most chemically akin to it-hydrogen selenide or hydrogen sulphide notably-you would expect it to boil at minus 135 degrees Fahrenheit and to be a gas at room temperature. Most liquids when chilled contract by about 10 percent. Water does too, but only down to a point. Once it is within whispering distance of freezing, it begins-perversely, beguilingly, extremely improbably-to expand. By the time it is solid, it is almost a tenth more voluminous than it was before. Because it expands, ice floats on water-БЂњan utterly bizarre property,БЂ« according to John Gribbin ...»

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