Description of soil BCSPFansadN (SPETIFORE)

Rego Gleysol

The soil is in native condition (undisturbed by agriculture).

The soil material is primarily composed of mineral particles.

The water table is always present in the soil.

The growth of plant roots is restricted by the third layer.

Salinity (conductivity > 4 dS/m)

Water is removed so slowly in relation to supply that the soil remains wet for a comparatively large part of the time the soil is not frozen. Excess water is evident in the soil for a large part of the time. Subsurface flow or groundwater flow, or both, in addition to precipitation are the main water sources; there may also be a perched water table, with precipitation exceeding evapotranspiration. Soils have a wide range in available water storage capacity, texture, and depth, and are gleyed subgroups, Gleysols, and Organic soils.

Materials modified by people,including those associated with mineral exploitation and waste disposal. They include materials deposited as a result of human activities or geological materials modified artificially so that their physical properties (structure, cohesion, compaction) have been drastically altered. Examples are areas of landfill, spoil heaps, open-pit mines and levelled irrigated areas.

Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL).

pH < 5.6

These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand.

Medium (USDA Texture Classes: VFSL,L,SIL,SI,GL,GSIL).

pH < 5.6

These sediments generally consist of gravel and sand with a minor fraction of silt and rarely of clay. The gravels are typically rounded and contain interstitial sand.

Coarse (USDA Texture Classes: FS,LCS,LS,LFS,GLS,CBLS).

pH < 5.6