Kiliwani 1 gas contact was 30 mt lower than Songo Songo
Songo Songo and Kiliwani are both from the same reserviour.
The original source of the gas therefore must have been from Kiliwani
It is lower than Songo Songo(30 mt) and we know gas rises until it meets a cap.
Concluding the gas accumulation source is from Kiliwani 1 and therefore my view is that it should hold the bulk of the gas. Hence larger gas pool.
The remainder escaped - spilled over into Songo Songo.
and thoughts.
regards
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