Water Saturation (Sw)- Dewan (1983) - Dispersed Clay Model
Water Saturation (Sw)- Dewan (1983) - Dispersed Clay Model
- Where:
- Sw= water saturation of the uninvaded zone
- Rt= true formation resistivity (i.e., deep induction or deep laterolog corrected for invasion)
- Rw= resistivity of formation water at formation temperature
- ɸs= sonic porosity
- q= intergranular space filled with clay
Calculate Water Saturation (Sw) | |||||||
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Results
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Water Saturation (Sw) - Results | ||||||
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Rw (ohm-m) | ɸs (dec) | Rt (dec) | q | Sw (dec) | Sw (%) | |
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Constant q (intergranular space filled with clay)
- Where:
- ɸD= density porosity
- ɸs= sonic porosity
- q= intergranular space filled with clay
Calculate Constant q | |||||||
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Results
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Constant q - Results | |||
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ɸs (dec) | ɸd (dec) | q | |
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