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MM204
|
Site code |
|
| Location |
Rokewood Junction (Dereel Road), Rokewood district,
south-west Victoria
|
| Landform |
|
| Geology |
Neogene Hanson Plain Sand: fluvial gravel, sand, silt
|
| Element |
|
Profile morphology
| | |
A1 | 0–25 | Brown (7.5YR4/4); sandy loam; apedal massive structure; weak consistence (dry); common fine segregations; clear boundary to: |
A2 | 25–50 | Strong brown (7.5YR5/6), pink (7.5YR7/4 dry) conspicuously bleached; sandy loam; very many fine to coarse segregations; sharp boundary to: |
B21 | 50+ | Yellowish brown (10YR5/6) with red (2.5YR4/6) mottles; medium clay; moderate fine blocky structure; firm consistence (moderately moist); common fine segregations. |
ASC: Ferric,
Mottled-
Subnatric, Brown
Sodosol
Analytical data Source: Government of Victoria, State Chemistry Laboratory.
Site MM204 | Sample
depth | pH | EC | NaCl | Ex Ca | Ex Mg | Ex K | Ex Na | Ex Al | Ex acidity |
Horizon | cm | H2O | CaCl2 | dS/m | % | cmolc/kg | cmolc/kg | cmolc/kg | cmolc/kg | mg/kg | cmolc/kg |
A1 | 0–25 | 5.6 | N/R | 0.05 | N/R | 1.1 | 1.1 | 0.2 | 0.1 | N/R | 9.9 |
A2 | 25–50 | 6.1 | N/R | 0.03 | N/R | 1.2 | 1.2 | 0.1 | 0.1 | N/R | 5 |
B21 | 50+ | 6.3 | N/R | 0.05 | N/R | 0.5 | 0.5 | 0.2 | 0.7 | N/R | 4.7 |
Site MM204 | Sample
depth | FC
(-10kPa) | PWP
(-1500kPa) | KS | FS | Z | C | Org C | Bulk density |
Horizon | cm | % | % | % | % | % | % | % | t m-3 |
A1 | 0–25 | 13.1 | 5.7 | 56 | 28 | 7 | 6 | 1.6 | 1.65 |
A2 | 25–50 | N/R | N/R | 47 | 31 | 8 | 12 | 0.8 | N/R |
B21 | 50+ | 32.1 | 25.1 | 17 | 13 | 3 | 68 | N/R | 1.31 |
Management considerations
Strong texture contrast between the surface soil and the subsoil is a very important soil feature and may impact upon subsoil permeability. Conspicuously bleached A2 horizons containing Ferruginous and Ferromanganiferous nodules and concretions are key features of this profile. Sodic and mottled subsoils are other prominent features of this soil type.
The application of gypsum would be suitable for soil structure and improved permeability, while increasing organic matter and maintaining vegetative cover is important to help improve the soil structure. Penetration by deep-rooted crops is also useful as is minimum tillage practices which avoids bringing the sodic material to the surface.