Although in Mississippi organic matter normally accounts for less than 1 percent of the soil's volume, it is important. It enables individual soil particles to bind together into aggregates , it contributes to cation exchange capacity, and it provides water-holding ability. Humus is organic matter that is decomposed past recognition. Although humus is important to soil, it is relatively short-lived and must be replaced constantly by the action of microorganisms on undecomposed material. Smaller particles have a higher water-holding capacity because of the large surface area per unit of volume.
Water is retained by surface tension.
Surface tension is displayed in the beads of water that form on the outside of a cold glass. Until the beads gain enough weight to overcome the force holding them to the glass, they seemingly will defy gravity. Surface tension causes an interesting phenomenon in soils. Water will not move out of a small diameter void into a large diameter void until the force of gravity overcomes the surface tension. Therefore, soil with a mixture of large and small particles may have a higher water-holding capacity than a soil made up only of small particles.