The correct option is D Hygroscopic, capillary and bound water
Field water capacity is defined by the Soil Science Glossary Terms Committee (2008) as the content of water, on a mass or volume basis, remaining in a soil 2 or 3 days after having been wetted with water and after free drainage is negligible. Gravitational water would reach the water table deep down and runaway water flows on the surface, hence not being available in the soil.