Victorian Resources Online (archived)
Archived content — This page contains material from the Victorian Resources Online (VRO) website. It is no longer maintained and is provided for reference only. This content is hosted by CeRDI and is not endorsed by Agriculture Victoria.
Sitemap
MM111
|
Site code |
|
| Location |
Birregurra (Conns Lane), Colac district, south-west Victoria
|
| Landform |
|
| Geology |
|
| Element |
|
Profile morphology
| | |
A1 | 0–15 | Black (10YR2/1); medium clay; strong coarse blocky structure; strong consistence (dry); gradual boundary to: |
B21 | 15–30 | Very dark grey (10YR3/1) with brown (2.5Y5/4) mottles; medium heavy clay; strong coarse blocky structure; strong consistence (dry); boundary to: |
B22 | 30+ | Very dark gray (10YR3/1) with brown (2.5Y5/4) mottles; medium heavy clay; strong coarse blocky structure; strong consistence (dry). |
ASC: Eutrophic,
Mottled-
Subnatric, Black
Sodosol
Analytical data Source: Government of Victoria, State Chemistry Laboratory.
Site MM111 | 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 | 0–15 | 5.7 | N/R | 0.08 | N/R | 5 | 5 | 0.3 | 0.6 | N/R | 21.2 |
B21 | 15–30 | 7.1 | N/R | 0.23 | 0.02 | 7.5 | 7.5 | 0.2 | 1.8 | N/R | 6.3 |
B22 | 30+ | 7.6 | N/R | 0.34 | 0.08 | 7.7 | 7.7 | 0.2 | 3.7 | N/R | 4.6 |
Site MM111 | Sample
depth | FC
(-10kPa) | PWP
(-1500kPa) | KS | FS | Z | C | Org C | Bulk density |
Horizon | cm | % | % | % | % | % | % | % | t m-3 |
A1 | 0–15 | 35.5 | 22.8 | 1 | 36 | 23 | 33 | 4.5 | 1.31 |
B21 | 15–30 | 18.4 | 17.1 | 1 | 35 | 20 | 42 | N/R | 1.28 |
B22 | 30+ | N/R | 0 | 1 | 32 | 17 | 49 | N/R | N/R |
Management considerations
These soils are hardsetting surface and subsurface soils (A1 and A2) with medium to heavy textures. They are associated with sodic subsoils having poor structure. The poor structure results in dispersion and subsequent clogging of pores restricting water and gas movement through the subsoil. Mottled subsoils are common and are a further indication of periodic waterlogging and restricted water movement.
The soils are clay cracking soils throughout and vary in their workability depending on their moisture status (highly permeable when dry and impermeable when saturated). These soils are also prone to structure decline particularly when worked wet.
The application of gypsum is used to counter the effect of the sodicity and improve drainage properties. Penetration by deep-rooted crops is also useful as is minimum tillage practices which avoids bring the sodic, dispersive material to the surface.