Its not absorbed really is it, its more a matter of drainage.
If your being all technical, then I guess its osmosis, that's the travel of water between cells.
but soil is like, well, dead, so its gonna just drain through it.
Soils with high clay content have smaller pore spaces which can limit the infiltration of water. This means that water is more likely to run off the surface rather than being absorbed into the soil. Clay soils also tend to form a crust when dry, further decreasing water absorption.
Water that is absorbed through the soil surface is called seepage. This is water that soaks into the ground, usually in a low spot of the area.
Soils with high clay content have smaller pores and low infiltration rates, making it harder for water to penetrate and be absorbed by the soil. This leads to an increase in surface runoff or water not being absorbed, especially during heavy rain events when the soil becomes saturated quickly.
Clay soils can absorb water, but do so only slowly because they are very fine grained, and the spaces between the grains are very small. This is in contrast to sandy soils where the spaces are big and water penetrates easily. During periods of heavy rain you can quickly get standing water on the surface of clay soils, which soon leads to run-off.
Most of the sun's energy is absorbed in the top few meters of water, where sunlight can penetrate. This energy is absorbed by water molecules and particles in the water, which then transfer heat to the surrounding water through conduction and convection.
Water and dissolved minerals are absorbed by plants through their roots. The roots have tiny root hairs that increase surface area, allowing for absorption. Water moves from the soil into the roots through a process called osmosis, and minerals are absorbed through active transport mechanisms.
Water cannot be absorbed through the surface of a leaf.
Water cannot be absorbed through the surface of a leaf.
No, different soils absorb rain water at different rates.
Water primarily enters the plant through the roots, where it is absorbed from the soil. The root hairs increase the surface area for absorption, allowing the plant to take in necessary water and nutrients. While some water can be absorbed through the leaves via foliar uptake, the roots remain the main pathway for water entry.
Clay soils get waterlogged because of their small particle size and high level of compaction, which restricts water drainage. This leads to poor aeration and limits the movement of water through the soil profile, causing water to pool on the surface.
Surface runoff occurs more often in areas with soils high in clay content because clay has poor permeability, leading to water being unable to infiltrate into the soil. This results in increased surface runoff as the water flows over the impermeable clay layer instead of being absorbed into the ground. Additionally, clay soils have a tendency to become compacted, further reducing infiltration capacity and increasing runoff.