Structure and Parent Material | Single grain; Weak ; Platy2 | Granular, Angular and Subangular Blocky; Prismatic | Structureless or Massive | |||||||||||||
Loess: Outwash; Alluvium; Lacustrine8 | Till3 | |||||||||||||||
Week | Moderate; Strong | Strong | Moderate; Strong | Loess; Outwash; Alluvium; Lacustrine8 | Till3 | |||||||||||
Moist Consistence | lo vfr fr | vfr fr | fi | vfr | fi | vfr fr | fi | fr | fi | vfi | vfr | fr | fi | vfr fr | fi vfi | |
Texture | A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | |
1. Fragmental; Ext. or Very gravelly sand | > 1.004 | N/A5 | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | |
2. Sand; Loamy course sand; Loamy sand; Gravelly sand; Coarse sand; Gravelly loamy sand | 1.00 | 1.00 | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | 1.00 | N/A | N/A | N/A | N/A | |
3. Fine sand; Loamy fine sand; Coarse sandy loam | 0.84 | 0.91 | N/A | N/A | N/A | N/A | N/A | N/A | N/A | N/A | 0.91 | 0.84 | N/A | N/A | N/A | |
4. Sandy loam; Fine sandy loam; Gravelly sandy loam; Gravelly loam; Gravelly silt loam | 0.75 | 0.75 | N.A | 0.84 | N/A | 0.69 | N/A | N/A | 0.75 | N/A | 0.84 | 0.75 | 0.69 | 0.62 | 0.52 | |
5. Loam; Silt loam; Very fine sandy loam; Sandy clay loam; Silt; Very fine sand; Loamy very fine sand; Gravelly clay loam | 0.62 | 0.69 | 0.62 | 0.75 | 0.52 | 0.456 | 0.406 | 0.62 | 0.52 | N/A | 0.62 | 0.52 | 0.456 | 0.276 | N/R7 | |
6. Silty clay loam (<35% c); Clay loam (< 35% c) | .052 | 0.52 | 0.456 | 0.62 | 0.52 | 0.408 | 0.276 | 0.52 | 0.406 | 0.276 | 0.52 | 0.456 | 0.276 | N/R | N/R | |
7. Silty clay loam (>35% c); Clay loam (>35% c) | N/A | N/A | 0.406 | 0.456 | 0.406 | 0.276 | 0.206 | 0.406 | 0.276 | 0.206 | N/A | 0.206 | N/R | N/R | N/R | |
8. Sandy clay; Clay | N/A | N/A | N/A | N/A | 0.206,9 | N/A | N/A | N/A | 0.206,9 | N/R | N/A | N/A | N/R | N/A | N/R | |
9. Organics; Fragic; Lithic; Paralithic | ---SOIL PROPERTIES HAVE VERY SEVERE LIMITATIONS; SUBSURFACE DISPOSAL NOT RECOMMENDED----- |
FOOTNOTES:
1 Disturbed soils are highly variable and require special on-site investigations.
2 Moderate or strong platy structure for the soil textures in Groups 4, 5 and 6 have a loading rate of 0.40 g/sq.ft/d. Platy structure having firm or very firm consistency or caused by mechanical compaction has a loading rate of 0.0 g/sq.ft/d.
3 Basal glacial tills structured by geogenic processes have the same loading rates as structureless glacial till.
4 This soil group is estimated to have very rapid permeability and exceeds the maximum established rate in Illustration H, Exhibit A.
5 N/A means not applicable.
6 These soil groups are estimated to have moderately slow to very slow permeability and are less than the minimum established rate in Illustration H, Exhibit A.
7 N/R means not recommended. These soils have loading rates considered too low for conventional subsurface disposal.
8 In some areas, lacustrine material may have physical properties similar to glacial till and should be placed in the glacial till columns.
9 Non-swelling (1:1 lattice) clays formed in bedrock residuum have a loading rate of 0.27 g/sq.ft/d. Swelling (2:1 lattice) clays are not recommended for subsurface disposal.
Ill. Admin. Code tit. 77, pt. 905, app A, ILLUSTRATION M, exh. B