Porosity is the percentage of void space in a rock. It is defined as the ratio of the volume of the voids or pore space divided by the total volume. It is written as either a decimal fraction between 0 and 1 or as a percentage. For most rocks, porosity varies from less than 1% to 40%.
Porosity refers to the measure of how much of a rock is open space. The two factors concerning particles in a rock that have the greatest effect on the rock's porosity are shape and distribution.
The porosity of the rock is the most important factor in determining how much groundwater can be stored in underground rock. Porosity refers to the amount of empty space within the rock that can be filled with water. Rocks with high porosity can store more groundwater.
shape and sorting
The ability of a subsurface rock to hold water is called porosity. Porosity refers to the volume of open space within a rock that can hold water, allowing it to flow and be stored within the rock matrix.
It is called its porosity.
Porosity refers to the measure of how much of a rock is open space. The two factors concerning particles in a rock that have the greatest effect on the rock's porosity are shape and distribution.
porosity of the rock.
poorly sorted = low porosity well sorted = high porosity
total porosity of the rock weather their individual grains are connected or not.
The porosity of the rock is the most important factor in determining how much groundwater can be stored in underground rock. Porosity refers to the amount of empty space within the rock that can be filled with water. Rocks with high porosity can store more groundwater.
Porosity refers to the percentage of open space between individual rock particles in a rock layer. This space can be between grains or within the cracks or cavities of the rock.
The volume of open pore spaces in a rock is known as its porosity. It represents the percentage of void space in the rock that can potentially hold fluids like water or oil. Porosity is an important characteristic in determining the suitability of a rock for storing or transmitting fluids.
Clay has higher porosity than solid rock. Porosity is a measure of the amount of pore space within a material, and clay typically has more interconnected pore spaces compared to solid rock, allowing for greater water and gas storage. Solid rock, being less porous, has fewer interconnected pore spaces, limiting its ability to store fluids.
The relationship between density and porosity is an indirect proportionality.That is, the higher the density of a rock, the lower will be the porosity of that rock.In a more explicit way, the weight of over-lying rocks increase the density of the rock beneath, which in turn decreases the amount of pore spaces (porosity) of the rock through processes such as compaction, cementation, etc. Posted by Nwigwudu Ikechukwu.
shape and sorting
Shape and Distribution
The ability of a subsurface rock to hold water is called porosity. Porosity refers to the volume of open space within a rock that can hold water, allowing it to flow and be stored within the rock matrix.