Yes for example Clay has high porosity and low permeability
Metamorphic rocks like marble and quartzite are typically low in porosity and permeability due to their dense and compact nature. These rocks have undergone intense pressure and heat, which has resulted in their tight interlocking mineral grains that limit the movement of fluids through them.
Permeability/ hydraulic conductivity.
The permeability and porosity of an aquifer is very high, air and pretty much any liquid can pass trough it with ease. Where as shale has very little porosity making it virtually impossible for air or liquid to pass through.
Some soils may have high porosity due to a large number of interconnected pore spaces, but low permeability because the pores are small and not well connected. This restricts the movement of water through the soil, despite the high porosity.
Porosity refers to the amount of pore space within a material, while permeability refers to the ability of fluids to flow through that material. Materials can have high porosity but low permeability if the pore spaces are not interconnected or are blocked, which would inhibit fluid flow. Conversely, materials with high permeability typically have interconnected pore spaces that allow fluids to flow easily.
Metamorphic rocks like marble and quartzite are typically low in porosity and permeability due to their dense and compact nature. These rocks have undergone intense pressure and heat, which has resulted in their tight interlocking mineral grains that limit the movement of fluids through them.
Permeability/ hydraulic conductivity.
Porosity refers to the amount of empty space that is between particles of material. When something has a low porosity, it does not have much of this space between its particles.
poorly sorted = low porosity well sorted = high porosity
The permeability and porosity of an aquifer is very high, air and pretty much any liquid can pass trough it with ease. Where as shale has very little porosity making it virtually impossible for air or liquid to pass through.
Some soils may have high porosity due to a large number of interconnected pore spaces, but low permeability because the pores are small and not well connected. This restricts the movement of water through the soil, despite the high porosity.
Porosity refers to the amount of pore space within a material, while permeability refers to the ability of fluids to flow through that material. Materials can have high porosity but low permeability if the pore spaces are not interconnected or are blocked, which would inhibit fluid flow. Conversely, materials with high permeability typically have interconnected pore spaces that allow fluids to flow easily.
big particles=low porosity small particles=high porosity
Rocks that typically exhibit high permeability and low porosity include certain types of fractured or well-sorted sandstones and some volcanic rocks, such as basalt. In these cases, the presence of fractures or intergranular spaces allows fluids to flow easily through the rock, despite the overall volume of void spaces being relatively low. Additionally, some limestone formations can also have high permeability if they are highly fractured. These characteristics make such rocks important in fields like hydrogeology and petroleum engineering.
Earth materials vary in their capacity to hold water due to differences in their porosity and permeability. Porosity refers to the amount of pore space within a material, while permeability describes how easily water can flow through it. Materials with high porosity and permeability, such as sand and gravel, can hold more water compared to materials with low porosity and permeability, such as clay and bedrock.
moderate porosity, low permeability.
High porosity and permeability are typically found in sedimentary rocks such as sandstone and limestone, which have interconnected pore spaces that allow fluids to flow easily. Conversely, igneous rocks like granite and metamorphic rocks such as schist generally have low porosity and permeability due to their dense, crystalline structures that lack significant pore spaces. The properties of rocks can significantly affect their ability to store and transmit fluids, making these characteristics important in fields like geology and petroleum engineering.