Permeability is the ability of that water to be transmitted from one place to another. For example clays have a huge porosity, but very bad permeability. Secondary permeability is the measure of other physical structures in a rock or admixture that allows for storage of water in spaces not primary to the fabric of the formation.
Yes, an aquifer is a permeable rock layer that can hold and transmit water underground. It typically consists of materials such as sand, gravel, or rock that can store and allow the flow of water through them.
That would be an aquifer, which is a layer of permeable rock that can hold water and allow it to flow. Impermeable rock layers above and below the aquifer restrict the movement of water, causing it to accumulate within the aquifer.
Clay can form a barrier to water flow and prevent the formation of a good aquifer. However, if the clay layer is thick and overlain by a permeable layer, it can act as a confining layer for an underlying aquifer, enhancing its ability to hold water. Ultimately, the presence of other factors like the porosity and connectivity of the rock material will determine if a good aquifer can form in a layer of clay.
Aquifers are typically both porous and permeable. Porosity refers to the ability of a material to hold water within its spaces, while permeability is the ability of that material to allow water to flow through it. For an aquifer to effectively store and transmit water, it must possess both characteristics. Therefore, an aquifer cannot be porous but not permeable; it needs to have both properties to function as a reliable water source.
Aquifers are layers of rock (primarily limestone) that gather water in thier porous holes. People have made machines to extract this water, and they are very useful. Aquifers are used primarily in the coastal plains region of the USA.
The layer's low temperature allows it to hold more water vapor. Additionally, the layer's relatively still air prevents the water vapor from being quickly dispersed.
The two characteristics of the atmosphere that allow it to retain water vapor on Earth are temperature and pressure. Warmer air can hold more water vapor than cooler air, and higher pressure air can hold more water vapor than lower-pressure air. This combination allows for the retention of significant amounts of water vapor in the Earth's atmosphere.
The two key characteristics that allow a layer of the atmosphere, such as the troposphere, to retain significant amounts of water vapor are its temperature and pressure. Warmer air can hold more moisture due to increased kinetic energy, allowing for greater evaporation and retention of water vapor. Additionally, lower pressure in this layer facilitates the accumulation of water vapor, as it allows for a greater volume of air to contain moisture without condensing.
The two characteristics that help this layer retain water vapor are low temperature and high humidity. The low temperature allows the air to hold more water vapor, while the high humidity indicates that the air is already saturated with moisture, making it easier for the layer to retain additional water vapor.
Aquifers are layers of rock that hold a lot of water and allow it to circulate.
Yes, an aquifer is a permeable rock layer that can hold and transmit water underground. It typically consists of materials such as sand, gravel, or rock that can store and allow the flow of water through them.
The layer's temperature and pressure both play a crucial role in its ability to retain water vapor. Lower temperatures decrease the air's capacity to hold moisture, contributing to condensation and water retention. Additionally, higher pressure exerts more force, preventing water vapor molecules from escaping into the atmosphere.
That would be an aquifer, which is a layer of permeable rock that can hold water and allow it to flow. Impermeable rock layers above and below the aquifer restrict the movement of water, causing it to accumulate within the aquifer.
The two characteristics of the troposphere that help retain water vapor on Earth are the relatively low temperatures and high pressure at lower altitudes. The low temperatures allow the air to hold more water vapor, while the high pressure helps keep the water vapor from escaping into space.
Soil characteristics that allow for greater water retention include high organic matter content, finer texture (such as clay or silt), crumbly structure, and good porosity. These features help the soil hold onto water for longer periods of time and provide plants with better access to moisture.
A single layer DVD can hold 4.7gb and a double layer can hold 9.4gb
it would have to get colder for the water molucules to shrink and more to come in and it woluld allow more space