soil profile

The following horizons are listed by their position from top to bottom within the soil profile.

The properties may vary through the depth of a soil profile.

The major emphasis had been on the soil profile.

The soil profile on the farm has been disrupted by the flooding.

The resulting soil profile reflects the balance of these processes, present and past.

These properties influence how energy is partitioned in the soil profile.

The manganese may be partly responsible for the dark color of the soil profile.

As a result, layers (horizons) form in the soil profile.

The observations are typically performed on a soil profile.

Entisols - do not show any "significant" soil profile development.

The average soil profile is 33 cm deep.

Few soil profiles have all the major horizons.

Part of this soil profile includes an underlying clay or iron hardpan.

It produces roots throughout the soil profile, rooting several feet deep in some soils.

Intact soils generally have very well-defined horizons, or soil profiles.

Water is central to the solution, precipitation and leaching of minerals from the soil profile.

The variation in soil profile characteristics are much more pronounced because of the regional climatic differences.

Soil profile and groundwater condition should be established.

There are several buried layers within the Hilo soil profile.

Humus composes the bulk of organic matter in the lower soil profile.

Cryoturbation moves carbon from the surface to depths within the soil profile.

Typically equipped with a central corridor with viewing windows into the soil profiles on either side.

These processes produce the characteristic soil profile.

For example, soil profiles can be used to make spatial prediction of different chemical and physical soil properties.

This layer helps prevent soil erosion from taking place and ruining the soils profile or layout.