Porosity = (bulk volume - grain volume)/bulk volume x 100
Range of Porosity in %
- 0-5 - negligible
- 5-10 - poor
- 10-15 - fair
- 15-20 - good
- 20+ - very good
Nature of Porosity
1. Primary
- rock possesses this at the end of its depositional phase
- void of unaltered, fractured or dissolved grains
- depends on:
* degree of uniformity
* shapes of grains
* packing
* effects of compaction, during and after deposition
2. Secondary
- additional void space due to post-depositional or diagenetic processes
Rock samples
1. Sandstones - compaction, contact-solution and redeposition and to cementation
2. Carbonates - modification by solution, recrystallization, fracturing and cementation
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