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Primary migration may be initiated during compaction as a result of the pressure of overlying sediments.
The cells may be either empty or filled with mineral matter, and the cell walls may have been crushed during compaction (bogen texture).
Damage occurred during compaction was quantified using image analysis.
This pattern is modified during compaction and diagenesis (Khan et al. 2011).
Hence, physical and compaction data interval was established that evaluated powder deformation behavior during compaction.
This has been fitted with force and strain transducers to measure the stress state during compaction.
Finally, FA was used to further characterize deformation behavior during compaction.
This resulted in a better understanding of the behavior and local organization of foils during compaction.
It increased relatively slowly during compaction, and often not before high loading steps.
This can be attributed to interparticle resistance developed during compaction and mechanical loading.
Tensile stresses are generated during compaction that may lead to fracture.
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