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most organic matter occurs in the soil profile in the form of soil aggregates (clumps or clods), which are either clay, sandy, or mixtures of two or more. the formation and stability of soil aggregates are determined by complex interactions among soil constituents, including soil pore solution, organic matter, air-filled spaces, microorganisms, and the physical connections they establish. organic matter is particularly important in binding soil aggregates. organic matter is usually a source of particles for soil aggregates. the aggregates are often held together by a cementing action of organic matter. the organic matter also contributes to stability, because it prevents loss of water-stable aggregate particles. during the formation of soil aggregates, clay particles begin to align themselves in the presence of organic matter. the particles in these aggregates are bound together to form stable clay aggregates and are less susceptible to fragmentation during wetting and drying. water-stable aggregates are a type of sediment that are composed primarily of clays, such as kaolin and illite, or mixtures of two or more clays, which clump together as they get wetted and are then cemented together.
features of surface soils that can impede and even preclude infiltration are essentially nonexistent. for example, the surface of snow is nearly impervious to water entry. the feature most commonly associated with imperviousness is a dense crust, but crust thickness and its association with the degree of imperviousness of the surface soil has been found to be highly variable. water movement through soil is, however, often impeded by surface features such as impervious layers of clayey soil near the top of the soil profile. impervious surfaces are common on snow and ice at the surface and may vary in depth (i.e., the imperviousness may be moderate or more extreme). impervious soil at any depth or combination of depths and topographic features can present a serious obstacle to infiltration.
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