Property: Rutherglen Research Institute | Paddock #: 29 |
Aust. Soil Class.: Sodic, Mesotrophic, Yellow DERMOSOL | Northcote Factual Key: Gn 2.23 |
Great Soil Group: no suitable group | Map Unit: Stillards loam |
General Landscape Description: Lower slope of a gently undulating rise (2%). The original vegetation includes Yellow Box (E.melliodora). |
Soil Profile Morphology:
A11 | 0-10 cm | Dark brown (7.5YR3/4); light fine sandy clay loam; hardsetting; weakly structured; earthy fabric; weak consistence dry; contains a trace (1%) amount of quartz gravel; pH 6.4; abrupt change to: | NE5 Profile |
A12 | 10-25 cm | Yellowish red (5YR4/6); fine sandy clay loam; massive; earthy fabric; strong consistence dry; contains a trace (1%) amount of quartz gravel; pH 5.3; clear and wavy change to: | |
Subsoil | |||
B1 | 25-50 cm | Yellowish red (5YR5/8); clay loam, fine sandy (becoming light clay with depth); weakly structured; earthy fabric; firm consistence dry; contains a few (7%) ferromanganiferous nodules as well as a few (3%) angular quartz fragments (2-5 mm size); pH 6.5; gradual and wavy change to: | |
B21 | 50-75 cm | Brownish yellow (10YR6/6) with red (2.5YR4/8) mottles; light medium clay; moderate medium blocky structure; strong consistence dry; contains a few (10%) manganese stains in patches as well as a few (3%) quartz fragments (2-5 mm size), pH 7.1; gradual and wavy change to: | |
B22 | 75-110 cm | Light yellowish brown (10YR6/4) with red (2.5YR4/8) mottles; light clay; moderate medium polyhedral structure; strong consistence dry; contains a common (10-20%) amount of manganese segregations; pH 6.9; gradual change to: | |
B23 | 110+ cm | Brownish yellow (10YR6/6); light clay; strong medium polyhedral structure; strong consistence dry; contains a common (10%) amount of manganese segregations; pH 8.5. |
Key Profile Features:
The surface soil is slightly acid and the subsurface (A2) horizon is strongly acid. The upper subsoil is mainly slightly acid and the deeper subsoil (below 1 metre depth) is moderately alkaline. | The upper soil profile is non-sodic. The deeper subsoil (below 1 metre depth) becomes sodic. | ||
The level of soluble salts is very low throughout the profile. | The clay percentage increases gradually with depth. |
Management Considerations:
Surface (A) Horizons