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Fig. 2

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(a) Segmentation des phases et du liant (matrice) ; (b) partitionnement d’une image grand champ segmentée d’une roche argileuse de surface Dmax × Dmax en (c) Ni domaines de surface Di × Di. Les domaines sont caractérisés par une propriété p, qui est ici la fraction d’aire de la matrice argileuse représentée en noir.

(a) Mineral segmentation; (b) division of a 2D image of clayrock’microstructure characterized by a Dmax × Dmax area; (c) Ni domains of Di × Di areas. The domains are characterized by the clay fraction p (black).

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