Le Log de Potentiel Spontané (SP), un incontournable de la diagraphie depuis les années 1930, est un outil d'une simplicité trompeuse qui a le pouvoir de révéler des informations cruciales sur les formations souterraines. C'est l'une des techniques de diagraphie les plus anciennes et les plus simples, mesurant la différence de tension naturelle entre la formation et le fluide de forage dans le puits.
Fonctionnement :
Le log SP repose sur un principe fondamental : les différences de salinité. Lorsque le fluide de forage, souvent une solution saline, entre en contact avec les fluides de formation (qui peuvent être salés, d'eau douce, ou même des hydrocarbures), un potentiel électrochimique est créé. Cette différence de potentiel, mesurée par l'outil SP, est enregistrée le long du puits, produisant une courbe SP caractéristique.
Applications du Log SP :
Le log SP, malgré sa simplicité, offre une mine d'informations sur la formation. Il peut être utilisé pour :
Limitations :
Le log SP n'est pas sans limites :
Conclusion :
Malgré ses limites, le log SP reste un outil précieux pour les géologues et les géophysiciens. Sa capacité à fournir des estimations qualitatives de la perméabilité, des informations sur la qualité du réservoir et des informations sur la shalinité en fait un élément crucial de l'analyse des logs de puits. Le log SP, bien qu'une technique relativement simple, continue de jouer un rôle important dans la compréhension de la géologie complexe du sous-sol.
Instructions: Choose the best answer for each question.
1. What is the fundamental principle upon which the SP log operates?
a) Differences in pressure between the formation and the wellbore b) Differences in temperature between the formation and the wellbore c) Differences in salinity between the formation and the wellbore d) Differences in magnetic properties between the formation and the wellbore
c) Differences in salinity between the formation and the wellbore
2. Which of the following is NOT a common application of the SP log?
a) Estimating the permeability of a formation b) Identifying potential reservoir zones c) Determining the exact depth of a fault d) Evaluating the water resistivity of a formation
c) Determining the exact depth of a fault
3. What is a limitation of the SP log?
a) It can be used to identify hydrocarbon deposits with high accuracy. b) Its penetration is limited to the near-wellbore region. c) It is unaffected by the salinity of the drilling mud. d) It is highly effective in formations with very low permeability.
b) Its penetration is limited to the near-wellbore region.
4. How does the SP log differentiate between shaly and clean formations?
a) Shaly formations show stronger SP deflections. b) Clean formations show stronger SP deflections. c) Shaly formations show suppressed or distorted SP deflections. d) Clean formations show suppressed or distorted SP deflections.
c) Shaly formations show suppressed or distorted SP deflections.
5. What is the primary reason the SP log remains a valuable tool in well log analysis despite its limitations?
a) It is the cheapest and easiest logging technique. b) It can identify specific types of hydrocarbons. c) It provides valuable qualitative information about permeability, reservoir quality, and shaliness. d) It is highly accurate in estimating the depth of formations.
c) It provides valuable qualitative information about permeability, reservoir quality, and shaliness.
Scenario: You are a geologist working on a well log analysis. The SP log shows a strong negative deflection at a depth of 1000 meters. This deflection is followed by a gradual increase in the SP reading towards a more positive value. The formation is suspected to be a sandstone reservoir.
Task:
The strong negative SP deflection at 1000 meters indicates a high permeability zone. This is because the difference in salinity between the formation fluids and the drilling mud is significant, leading to a stronger electrochemical potential.
The gradual increase in SP reading after the deflection suggests a transition to a lower permeability zone. This could be due to a change in the lithology, porosity, or the type of formation fluids present.
Based on the SP log information and the suspected sandstone formation, the reservoir is likely a porous and permeable sandstone with good reservoir quality. The strong negative deflection at 1000 meters indicates a zone of high permeability, which is a desirable characteristic for a reservoir.
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