Sitemap

EGW59

Location: Omeo West

Australian Soil Classification: Bleached, Eutrophic, Red Chromosol

Map Unit: Minor map unit A
Previous Site Name: EG59

General Landscape Description: Alluvial terrace
Site description: Alluvial terrace, Simple slope, gradient unspecified
Land Use: Grazing on annual pasture
Native Vegetation: Montane grassy woodland
Geology: Pleistocene (Neogene) alluvium and colluvium.



Alluvial terrace near where soil samples were taken. The Livingston Fault formed the steep hills in the background.
No soil pit photo available, but the deep profile exposed in the first photo serves as an indication.

• Strong texture contrast between the surface soils (A1 and A2 horizons).
• High amounts of gravel in the subsoil.

• The soil shows marked texture contrast between the surface soil and the subsoil.
• Plant available water content is moderate, based on a root depth of 50 cm. The dense and coarsely structured subsoil is likely to restrict root growth and confine most of the roots to the surface soil.
• Roots will be impeded by the very stony subsoil.
• The soil profile is strongly acid throughout.
• The whole profile has very low amounts of soluble salts.

• The low wilting points (8.0 and 4.4 %) of the surface soils indicates the plants are able to utilize very light rains when the soil is dry. However, due to the low water storage capacity, plants will soon suffer moisture stress unless further rains occur.
• The surface soils are strongly acid. However the level of exchangeable aluminium is low and is unlikely to affect the growth of aluminium sensitive species, except the most sensitive. Lime can be used to increase soil pH but a pH/aluminium test is best performed by taking samples across the paddock and bulked together. The use of test strips to observe lime response could be used as an aid in evaluating its cost/benefit. For this soil a response to lime (about 2 tonnes/ha) would be expected.
• The organic matter content of the soil is low for such a high rainfall area. Such levels result in a low structural condition and low structural stability. Careful pasture management is needed to increase organic matter levels.
• Potassium is high and no response to potassium fertilisers would be expected.
• The nutrient status of the surface (A1 and A2) horizons is low (based on the sum of the exchangeable calcium, magnesium, potassium and sodium cations). The addition of lime will increase the Ca:Mg ratio and the exchangeable calcium.
• The bleached subsurface layer lacks structure, sets hard when dry, impedes plant growth and slakes partially when wet.

• The strongly structured clay subsoil is non-sodic and does not disperse. These soils appear to be strongly structured which should allow good root penetration.
• Root movement is likely to be restricted in the gravelly deep subsoil. Reddish colours indicate the soil is well drained internally.

This page contains material sourced from the Victorian Resources Online (VRO) website, originally published by the State Government of Victoria.

The content is provided under the Creative Commons Attribution 4.0 Australia licence (CC BY 4.0 AU).

This material is presented in an archived form and is no longer maintained or updated. It is provided for general information only and should not be relied upon as current advice.

This site is hosted by the Centre for eResearch and Digital Innovation (CeRDI), Federation University Australia. It is not endorsed by Agriculture Victoria.

Agriculture Victoria does not accept liability for any loss, damage or consequences arising from the use of, or reliance on, this material.