Porosity and Permeability Flashcards

1
Q

ratio of pore space in a sediment or sedimentary rock to the total volume of the rock, often expressed as a percentage.

A

Porosity

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2
Q

Total or absolute porosity is calculated as the ratio of pore volume (Vp) to bulk volume (Vb).

A

Total Porosity

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3
Q
  • pore spaces that are interconnected
  • important for groundwater and petroleum analysis
A

Effective Porosity

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4
Q

Originating from deposition, it can be intergranular (between framework grains), intragranular (within particles), or intercrystalline (between chemically formed crystals).

A

Primary Porosity:

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5
Q

Caused by the dissolution of cements or metastable framework grains in siliciclastic sedimentary rocks, or dissolution of cements, fossils, framework crystals, etc., in chemically formed rocks.

A

Solution Porosity

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6
Q

Arises from pore space in cement or among other authigenic minerals.

A

Intercrystalline Porosity:

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7
Q

Occurs due to rock fracturing by tectonic forces, compaction, or desiccation.

A

Fracture Porosity

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8
Q

The porosity of sedimentary rocks is influenced by various factors:

A

Depositional
Post Depositional
Initial Porosity
Diagenesis
Porosity Evolution

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9
Q

This process can rearrange grain packing and reduce porosity.

A

Compaction

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10
Q

can lead to a reduction in porosity.

A

Chemical dissolution

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11
Q

fill pore spaces and decrease porosity.

A

Cementation

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12
Q

capacity of a medium to allow the transmission of a fluid. In the case of rocks, it refers to the property that enables a fluid to flow through the interconnected pores within the rock

A

Permeability

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13
Q

the rate of fluid flow through a porous rock is directly proportional to the rock’s permeability and inversely proportional to the fluid’s viscosity.

A

Darcy’s law,

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14
Q

defined as the permeability unit equivalent to the passage of one cubic centimeter of fluid with a viscosity of one centipoise, flowing in one second, under a pressure differential of one atmosphere, through a porous medium with a cross-sectional area of one square centimeter and a length of one centimeter.

A

darcy

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15
Q

Permeability tends to ???? with decreasing particle size. Smaller particles lead to ???? Pore diameters and ????? capillary pressures, impeding fluid flow.

A

decrease; smaller; increased

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16
Q

Permeability may ???? with decreasing sorting, as variations in grain size distribution can affect the connectivity of pore spaces.

A

decrease

17
Q

Permeability may decrease with ?????? particle sphericity, possibly due to tighter packing of spherical particles, which reduces pore size.

A

increasing