Description of soil SKHTAR~~~~A (HATTON O.BC)

General Characteristics
Classification O.BC

Orthic Brown Chernozem

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 Fourth layer

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

Type of root restricting layer Lithic

Lithic (consolidated bedrock)

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
Uppermost Fluvial

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.

Moderately Coarse

Moderately Coarse (USDA Texture Classes: VFS,LVFS,CSL,SL,FSL,GSL,CBSL,GFSL).

Moderately / Very Strongly Calcareous

6 - 40 CaCO3 equivalent (%)

Below Residual

Unconsolidated, weathered, or partly weathered mineral soil material that accumulates by in situ disintegration of bedrock.

Very Fine

Very Fine (USDA Texture Classes: HC (more than 60% clay).

Medium Acid to Neutral

pH 5.6 - 7.4

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 13 A p 1.4 0 74 16 10 M 15 1.2 -9 -9 6.4 6.7 100 0 12 0 20.81 47 -9 17 9
2 13 49 B m 1.4 0 77 11 12 M 11 0.5 -9 -9 6.8 7.0 100 0 11 0 21.81 47 -9 15 9
3 49 80 C k 1.6 0 84 7 9 M 19 0.2 -9 -9 7.9 8.0 100 10 8 0 31.1 40 -9 13 8
4 80 100 R -9.0 -9 -9 -9 -9 - -9 -9.0 -9 -9 -9.0 -9.0 -9 -9 -9 -9 -9.0 -9 -9 -9 -9
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