Porosity

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Porosity is the measure of the void (i.e., "empty") spaces in a material, and can be used to quantify the porous nature of many substances such as rocks, soil, ceramics, foam, and biological tissue. It is defined as the ratio of the volume of voids to the total volume of the material. It is a fraction between 0–1, often expressed as a percentage.

Types of Porosity[edit | edit source]

There are several types of porosity:

  • Primary porosity: This is the original porosity of a material. It is often found in sedimentary rocks and is created during the deposition of the sediment.
  • Secondary porosity: This is porosity that is created after the rock has been formed. It can be caused by factors such as dissolution or fracturing.
  • Effective porosity: This refers to the porosity that contributes to fluid flow or permeability in a rock. This is the porosity that is interconnected and allows fluid to flow from one pore to another.
  • Ineffective porosity: This refers to the porosity that does not contribute to fluid flow in a rock. This is the porosity that is not interconnected and does not allow fluid to flow from one pore to another.

Measurement of Porosity[edit | edit source]

Porosity can be measured through several methods, including:

Applications of Porosity[edit | edit source]

Porosity is used in multiple fields, including:

  • Petroleum geology: Porosity is a key factor in the reservoir capacity of a rock.
  • Civil engineering: Porosity affects the strength of materials and the ease with which water can flow through soils and rocks.
  • Hydrology: Porosity is an important factor in groundwater flow and aquifer recharge.
  • Soil science: Porosity affects the movement of air and water through soil, and the ability of plants to extract water.

See Also[edit | edit source]

Porosity Resources
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