Abstract
The pyrolysis of the organic material of Timahdit oil shale under an inert atmosphere has been realised to point out the role of both sedimented plan and profile concentration of organic material according to parallel and perpendicular orientation in relation to the sedimented plan. These concentration profiles have been determined by means of microthermobalance. The diffusional coefficient, which varies with concentration has been calculated by the resolution of Pick's Second Law at 345 °C.
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