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Description of soil MBSEU~~~~~A (Shellmouth)

General Characteristics
Classification O.R

Orthic Regosol

Profile Agricultural soil profile

The soil has been disturbed by agriculture.

Kind of material Mineral

The soil material is primarily composed of mineral particles.

Water table Never

The water table is not present in the soil at any time.

Root restrictions No root restricting layer

The growth of plant roots is not restricted by any soil layer.

Type of root restricting layer n/a

Not Applicable

Drainage Rapidly drained

Water is removed from the soil rapidly in relation to supply. Excess water flows downward if underlying material is pervious. Subsurface flow may occur on steep gradients during heavy rainfall. Soils have low available water storage capacity (2.5-4 cm) within the control section, and are usually coarse textured, or shallow, or both. Water source is precipitation.

Parent Materials
Mode of Deposition Texture Chemical properties
Colluvial

Massive to moderately-well stratified, nonsorted to poorly sorted sediments with any range of particle sizes from clay to boulders that have reached their present position only by direct, gravity-induced movement. Processes include slow displacements such as creep and solifluction and rapid movements such as earth flows.

Undifferentiated

Undifferentiated

Undifferentiated

Undifferentiated acidity and/or calcareousness

Soil Layer Characteristics

Soil Layer Characteristics
Classification Physical Chemical Water
Layer Number Upper
depth
Lower
depth
hzn_lit hzn_mas hzn_suf hzn_mod bd cofrag tsand tsilt tclay domsand vfsand orgcarb vonpost wood phca ph2 bases caco3 cec ec ksat kp0 kp10 kp33 kp1500
1 0 15 A p 1.4 0 85 10 5 F 35 4.8 -9 -9 7.2 7.6 100 0 21 0 10.0 47 17 13 6
2 15 20 B mgj 1.5 0 90 5 5 F 35 0.2 -9 -9 7.2 7.6 100 0 7 0 10.0 43 12 9 4
3 20 100 C kgj 1.5 0 90 5 5 F 35 0.0 -9 -9 7.4 7.8 100 5 3 0 10.0 43 12 9 4
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