Soil color has absolutely no influence on the rate at which water can pass through it.
Red soils are red because a microscopically thin layer of an iron oxide coats the mineral soil particles. If the Fe oxide coating is on sand particles, water will pass through it quickly. If the Fe oxide coating is on silt or clay particles, water will pass through it more slowly, unless the soil has favorable structure.
Take a sample of the red soil and wet it. If you can mold it and work it with your fingers to any extent, it has some clay in it. If it can be molded like modeling clay, it has a lot of clay in it.
the soil that allows water to pass through very slowly is clay
sand
percolation
Such soil or rock is 'impervious'.
11234567890-=-09876543wawzsr
the soil that allows water to pass through very slowly is clay
sand
percolation
Such soil or rock is 'impervious'.
11234567890-=-09876543wawzsr
Maybe because when the water is in the soil and is going through the roots up the stem some soil particles can go in the water and travel with it.
Loose and sandy soils allow water to pass through them faster as they have larger inter-particle spaces b/w particles of soil
A paper filter will allow water to pass slowly through, leaving the soil particles behind.
A paper filter will allow water to slowly pass through, leaving the soil particles behind.
The word is porous.
A layer of rock or soil that does not allow water to pass through it .
The water stays there and forms a water table, like when you dig down in sand and reach water.