Some soils have a large volume of pore space, but the individual pores are too small to allow water to pass through.
Some soils have a large volume of pore space,but the individual pores are too small to allowwater to pass through.
Well, in Antarctica, the soil is called Permafrost. It is very silty/sandy-like.The porosity is very low, the soil cannot hold very much water. And as you may know, if soil has low porosity, then it must have high permeability.Now I'm not really going to get into details, but that is the main idea. If you are looking for more of a detailed explanation, then I will link a website you can get some more information on.Here it is: http://en.wikipedia.org/wiki/Permafrost
The state of Texas has many types of soils. Some of the soils are Trans-Pecos, Upper Pecos, High Plains and Rolling Plains soil.
best example of cohesive soil is the soil which have high content of clay or clay.
It is important for soil to hold water for plants to grow, but the soil cannot be so porous that no water is retained for plants to grow in (especially those with shallow root systems), nor can the soil be not porous since plants drown from access to too much water. The majority of crops rely on soils that have some porosity in them versus ones that have no porosity or too much porosity since, for the former, crops like corn and wheat have very shallow root systems that do not grow deep enough to reach water, and for the latter are intolerant of too much water (exceptions are rice patties).
Some soils have a large volume of pore space,but the individual pores are too small to allowwater to pass through.
Sand has several physical properties. Some of the most important are porosity, mineral composition, grain size, grain shape, and permeability.
soils with low permeability
Well, in Antarctica, the soil is called Permafrost. It is very silty/sandy-like.The porosity is very low, the soil cannot hold very much water. And as you may know, if soil has low porosity, then it must have high permeability.Now I'm not really going to get into details, but that is the main idea. If you are looking for more of a detailed explanation, then I will link a website you can get some more information on.Here it is: http://en.wikipedia.org/wiki/Permafrost
Sand content is part of many different native "soils", but they are not exactly the same thing. Loam soil - the best kind for growing things - is made up of fairly equal proportions of sand, silt, clay and organic matter. Some soils are high in clay (called "heavy" soils). Some soils are high in sand content - the soil in my own yard for example. So in a sentence: Sand is a component of most soils - it is not "soil" by itself.
The state of Texas has many types of soils. Some of the soils are Trans-Pecos, Upper Pecos, High Plains and Rolling Plains soil.
selective permeability or semi-permeability
selective permeability or semi-permeability
selective permeability or semi-permeability
best example of cohesive soil is the soil which have high content of clay or clay.
It is important for soil to hold water for plants to grow, but the soil cannot be so porous that no water is retained for plants to grow in (especially those with shallow root systems), nor can the soil be not porous since plants drown from access to too much water. The majority of crops rely on soils that have some porosity in them versus ones that have no porosity or too much porosity since, for the former, crops like corn and wheat have very shallow root systems that do not grow deep enough to reach water, and for the latter are intolerant of too much water (exceptions are rice patties).
Selective Permeability