plants prevents soil eroison
Clay soils.
Plants absrb water through their roots which are in soil; so there must be water under the soil for the plants to survive.
Silt has neither high or low permeability. It has moderate permeability. :) !
Because depends on how the soil is
Soil permeability refers to the ability of soil to allow water to pass through it. It is influenced by the soil texture, structure, and organic matter content. Soils with high permeability allow water to infiltrate quickly, while soils with low permeability may lead to waterlogging or runoff issues.
Antarctic soil typically has low porosity due to the presence of permafrost, which limits the amount of open space in the soil. Permeability can also be low in Antarctic soil because the frozen ground restricts the movement of water and gases through the soil. These characteristics make it challenging for plants to grow in Antarctic soil.
Soil permeability refers to the soil's ability to transmit water through it. It is influenced by factors such as soil texture, structure, and compaction. A high-permeability soil allows water to flow through it easily, while a low-permeability soil restricts water movement.
Permeability of soil is a measure of how easily water can flow through it. It is determined by the size and arrangement of soil particles, with sandy soils typically having higher permeability than clay soils. Permeability influences drainage, groundwater recharge, and the movement of contaminants in the soil.
The pH of soil has a great importance for the growth of plants.
Soil particle size influences the soil's physical properties like porosity, permeability, and water holding capacity, which affect plant growth. It also plays a role in determining soil fertility and the rate at which nutrients are released to plants. Additionally, soil particle size affects soil composition and structure, influencing its ability to support various types of vegetation.
Permeability is when water can pass through different types of soil and rocks. Therefore the permeability affects the soil and rocks because if the soil or rock is PERMEABLE then the groundwater can easily flow through it :)
permeability
Soil permeability is a measure of how easily water can flow through soil. It is an important factor in determining the ability of soil to absorb and drain water, which can impact plant growth and soil erosion.
Soil permeability refers to the ability of soil to allow water or other liquids to flow through it. It is dependent on factors such as the soil composition, texture, structure, and porosity. Soils with high permeability allow water to pass through quickly, while those with low permeability hold water and may become waterlogged.
Soil permeability is important because it determines how easily water, nutrients, and gases can move through the soil. This affects plant growth and root development, as well as the risk of water runoff and erosion. Understanding soil permeability helps to make informed decisions about irrigation, drainage, and soil management practices.
Tundra soil has low permeability due to the presence of permafrost, which is frozen soil and rock that acts like a barrier to water infiltration. The ice in permafrost prevents water from moving through the soil easily, resulting in a low permeability. Additionally, the cold temperatures in the tundra can slow down soil processes, further reducing permeability.