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Very well, I have managed to discover in An additional SPE paper some true details from which I used to be in the position to infer the fractional movement curve for 3 locations of Southern and Central Ghawar. In another references, I discovered a carbonate fractional move curve within the United Arab Emirates.
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So my layer counting claims that over 14 yrs we went from 10 levels of red/pink inside the crest to two levels of red during the crest. And when we do precisely the same to the (b) cross portion over the japanese flank, we get this:
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So that implies that the distinction between the red regions (twenty% h2o saturation) in the simulation picture previously mentioned plus website the inexperienced areas (sixty% drinking water saturation) could possibly be quite substantial.
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