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So just how to look at this is the fact that after we are under twenty% to the X-axis (under twenty% water in the oil), There may be zero within the y-axis (the h2o is not going to stream through the rock in the least). As we get previously mentioned twenty% water saturation, the circulation of h2o increases speedily, until previously mentioned eighty% h2o, there is absolutely no flow of oil in the slightest degree.
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In a set of interconnected pores by which oil and drinking water are now being compelled at force, the circulation is too turbulent for big areas of the two fluids to different out from one another. And nonetheless, oil and drinking water do not love to mix, and can have a tendency to bead up during the presence of another. When there is only a bit drinking water and loads of oil, then the oil will type an interconnected community of fluid through the rock pores, whereas the drinking water will usually make little beads in the oil.
Very well, I've managed to search out in One more SPE paper some real details from which I was able to infer the fractional stream curve for 3 locations of Southern and Central Ghawar. In a distinct references, I found a carbonate fractional circulation curve through the United Arab Emirates.
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