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Caractérisation de la maturité du kérogène dans les réservoirs de schiste

Caractérisation de la maturité du kérogène dans les réservoirs de schiste

Malleswara Yenugu

98,68 €
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Editorial:
KS OmniScriptum Publishing
Año de edición:
2025
Materia
Ciencias de la tierra/geociencias
ISBN:
9786208835514
98,68 €
IVA incluido
Disponible

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Sobre IBD

La principale différence entre un réservoir conventionnel et un réservoir non conventionnel réside dans la présence de matière organique dans ce dernier. La matière organique est composée de kérogène (~90 %) et de bitume (~10 %). Lorsque le kérogène arrive à maturité, il produit d’abord du pétrole, puis du gaz. Il reste ensuite des résidus sous forme de carbone pur (graphite). Pour mieux comprendre la production d’hydrocarbures à partir des schistes, une approche multidisciplinaire associant la géologie, la géomécanique, la géochimie, la géophysique, la pétrophysique et la physique des roches joue un rôle important.

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