Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Caratterizzazione della maturità del cherogene per giacimenti di scisto
Caratterizzazione della maturità del cherogene per giacimenti di scisto

Caratterizzazione della maturità del cherogene per giacimenti di scisto

Malleswara Yenugu

98,69 €
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Editorial:
KS OmniScriptum Publishing
Año de edición:
2025
Materia
Ciencias de la tierra/geociencias
ISBN:
9786208835521
98,69 €
IVA incluido
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La differenza principale tra un giacimento convenzionale e uno non convenzionale è la presenza di materia organica in quest’ultimo. La materia organica è costituita da cherogene (~90%) e bitume (~10%). Quando il cherogene matura, inizialmente produce petrolio e poi gas. Rimane ancora qualche residuo sotto forma di carbonio puro (grafite). Per comprendere meglio la produzione di idrocarburi dagli scisti, è importante adottare un approccio multidisciplinare che coinvolga geologia, geomeccanica, geochimica, geofisica, petrofisica e fisica delle rocce.

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