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The evaluation results show that porosity decreases as the intensity of cementation increases (Fig. 5 left).
Relative intensity of cementation and dissolution is characterized by the content of cement/apparent dissolution surface porosity ratio.
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On the whole, the development intensity of the cementation is moderate to strong.
Open image in new window Fig. 7 Evaluation map of relative intensity of compaction and cementation of the semi-weathered rock layer.
Open image in new window Fig. 8 Evaluation map of relative intensity of dissolution and cementation of the semi-weathered rock layer.
The reservoirs develop medium intensity of compaction, moderate to strong cementation, relatively strong dissolution, suggesting that it is in stage B of the middle diagenetic evolution.
Bioclastic content, algal and microbial content, sorting and roundness of skeletal grains and porosity in depositional successions change with sediment source, sediment accumulation rate, grain characteristics and textures of sediments, hydrodynamic intensity and cementation features.
In our study, no such forces acted on the cemented coping from time of cementation to time of testing.
The proportion of cementation in similar material increases linearly with the strength of similar material specimen.
However, coring revealed varying degrees of cementation.
The model can be applied for any structured material regardless of the origin of cementation.
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