Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Charakterystyka dojrzałości kerogenu w złożach łupkowych
Charakterystyka dojrzałości kerogenu w złożach łupkowych

Charakterystyka dojrzałości kerogenu w złożach łupkowych

Malleswara Yenugu

98,69 €
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Editorial:
KS OmniScriptum Publishing
Año de edición:
2025
Materia
Ciencias de la tierra/geociencias
ISBN:
9786208835545
98,69 €
IVA incluido
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Sobre IBD

Główną różnicą między złożem konwencjonalnym a niekonwencjonalnym jest obecność materii organicznej w złożach niekonwencjonalnych. Materia organiczna składa się z kerogenu (~90%) i bitumu (~10%). Po osiągnięciu dojrzałości kerogen najpierw wytwarza ropę naftową, a następnie gaz. Pozostaje jednak pewna ilość pozostałości w postaci czystego węgla (grafitu). Aby lepiej zrozumieć wydobycie węglowodorów z łupków, ważną rolę odgrywa multidyscyplinarne podejście łączące geologię, geomechanikę, geochemię, geofizykę, petrofizykę i fizykę skał.

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