Description of soil BCKUEa~~~~A (KULLEET)

General Characteristics
Classification GL.SB

Gleyed Sombric Brunisol

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 Unspecified period

The water table is present in the soil during an unspecified period.

Root restrictions Fourth layer

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

Type of root restricting layer Undifferentiated


Drainage Imperfectly drained

Water is removed from the soil sufficiently slowly in relation to supply, to keep the soil wet for a significant part of the growing season. Excess water moves slowly downward if precipitation is the major supply. If subsurface water or groundwater, or both, is the main source, the flow rate may vary but the soil remains wet for a significant part of the growing season. Precipitation is the main source if available water storage capacity is high; contribution by subsurface flow or groundwater flow, or both, increases as available water storage capacity decreases. Soils have a wide range in available water supply, texture, and depth, and are gleyed phases of well drained subgroups.

Parent Materials
Mode of Deposition Texture Chemical properties
Uppermost Marine

Unconsolidated deposits of clay, silt, sand, or gravel that are well to moderately well sorted and well to moderately well stratified (in some places containing shells). The deposits have settled from suspension in salt or brackish water bodies or have accumulated at their margins through shoreline processes such as wave action and longshore drift. Nonfossiliferous deposits may be judged marine if they are located in an area that may reasonably be considered to have contained salt water at the time the deposits were formed.

Moderately Coarse

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

Extremely / Strongly Acidic

pH < 5.6

Below Glaciofluvial

Material moved by glaciers and subsequently sorted and deposited by streams flowing from the melting ice. The deposits are stratified and may occur in the form of outwash plains, deltas, kames eskers, and kame terraces. See also glacial drift and till.


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

Medium Acid to Neutral

pH 5.6 - 7.4

Soil Layer Characteristics
Classification Physical Chemical Water
Layer Number Upper
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 20 A p 0.99 5 35 50 15 F 9 6.0 -9 -9 4.2 4.8 45 0 88 0 1.0 63 39 34 14
2 20 37 B f 1.37 5 31 42 27 F 8 3.0 -9 -9 4.3 5.2 17 0 31 0 5.0 48 29 22 10
3 37 74 B m 1.34 5 35 50 15 F 9 2.0 -9 -9 4.5 5.3 61 0 18 0 7.0 50 35 27 10
4 74 100 2 BC 1.6 5 82 17 1 M 20 1.0 -9 -9 5.2 5.6 78 0 7 0 6.0 40 21 16 7