Solution:Rising of underground water is primarily driven by pressure differences and permeability of soil and rock layers, rather than capillarity. Therefore, the rising of underground water is not primarily caused by capillarity but rather by hydrostatic pressure and other geological factors.
We can define capillary action as a phenomenon where the ascension of liquids through a tube or cylinder takes place. This primarily occurs due to adhesive and cohesive forces.
The liquid is drawn upward due to this interaction between the phenomena. The narrower the tube, the higher will the liquid rise. If any of the two phenomena, i.e., that of surface tension and a ratio between cohesion to adhesion, increase, the rise will also increase. Although, if the density of the liquid increases, the rise of the liquid in the capillary will lessen.
The amount of water that is held in the capillary also determines the force with which it will rise. The material that surrounds the pores fills the pores and also forms a film over them. The solid materials that are nearest to the molecules of water have the greatest adhesion property. The thickness of the film increases as water is added to the pore, and the magnitude of capillary force gets reduced.
The film that was formed on the outer surface of the soil molecules also may begin to flow. The capillary action is what causes the movement of groundwater through the different zones of soil. How the fluids are transported inside the xylem vessels of plants is also by the capillary action. As the water evaporates from the surface of the leaves, water from the lower levels, that is, the roots, is drawn up by this phenomenon.