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Porosity is the ratio of empty space (void volume) to the total bulk volume of a solid material. This empty space can be in the form of pores between grains or crystals, or cracks within the material.12

In rocks, porosity is influenced by factors such as the compaction of sediment, the arrangement and shape of grains, and the presence of cementing minerals. For example, well-sorted sediments, which have grains of similar sizes, can have significant porosity, while poorly sorted sediments have decreased porosity.2

Porosity is also a key property in materials like coal, affecting the rate of chemical reactions due to the increased internal surface area it provides. The accessibility of this internal surface area depends on the size and shape of the pores.3

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