Site LS6

Location: Diapur Ridge

Australian Soil Classification: Calcic, Mottled-Hypernatric, Grey SODOSOL (sandy)

Northcote Factual Key: Dy5.43
Great Soil Group: solodized solonetz

General Landscape Description: Lower slope on the eastern flank of a north-south trending ridge. Slope 4%. Shallow erosion gullies (1-1.5 m deep) are present.
Native Vegetation: Yellow Gum (Eucalyptus lecoxylon) is the dominant tree species.

LS6 Landscape

A1	0-15 cm	Very dark greyish brown (10YR3/2); loamy sand; weakly structured; weak consistence dry; pH 6.1:	LS6 Profile
A2	15-20 cm	Conspicuously bleached; loamy sand; structureless; weak consistence dry; contains a common (10 %) amount of ironstone nodules; pH 7.4; sharp change to:
A3	20-21 cm	Conspicuously bleached; cemented sand capping; pH 7.8:
Subsoil
B21	21-35 cm	Dark greyish brown (10YR4/2) with yellowish brown (10YR5/4) and strong brown (7.5YR4/6) mottles; heavy clay; moderate columnar structure; very strong consistence dry; pH 8.3:
B22	35-65 cm	Yellowish brown (10YR5/6) with yellowish red (5YR5/6) mottles; medium heavy clay; strong prismatic, breaking to strong blocky structure; strong consistence moist; contains very few (2 %) ironstone nodules and many (50 %) soft calcareous segregations; pH 8.9:
C	65+ cm	Weathered sandstone.

• Strong texture contrast between sandy surface (A) horizons and subsoil (B21) horizon.
• Non hardsetting nature of surface soil.
• Coarse columnar structure at top of subsoil.

The surface soil is slightly acid. The subsoil is moderately alkaline becoming strongly alkaline with depth.

The salinity rating is very low in the surface and upper subsoil becoming moderate with depth.

The surface is non-sodic. The subsoil is strongly sodic.

• The surface horizon has a moderate amount of organic carbon and nitrogen but a very low nutrient status overall. Trace element (e.g. zinc and copper) deficiency may occur. Organic matter is important in these light textured soils for holding nutrients.
• The surface horizon has a low plant available water holding capacity due to the sandy texture. However, the low wilting point value (ie. 4 %) indicates that plants will be able to utilise light rains falling on relatively dry soil.
• The sandy surface horizons are prone to wind erosion. Removal of these horizons would expose the highly dispersible subsoil to water erosion and could lead to gully erosion.
• After heavy rainfall, saturation of the subsurface (ie. A2) horizon is likely to occur above the relatively impermeable B horizon. The conspicuous bleaching indicates that this horizon is periodically waterlogged.
• The surface horizon is non hard-setting and weakly coherent; therefore it should not restrict seedling emergence and is relatively easy to work.
• Water infiltration rates are high. However, in some instances the dry sandy surfaces may develop water repellent properties which reduces initial wetting up and hence infiltration.

• The strongly sodic subsoils which disperse completely are likely to restrict water and root movement down the profile from 25 cm and below. The hard capping on top of the subsoil columnar structure will also be restrictive. Restricted root movement through the subsoil will reduce the ability of crops to utilise subsoil moisture and nutrients.

• Prone to gully erosion. The gullying at this site is largely the result of poor contouring in 1954 and a subsequent heavy rainfall event.
• Used for pasture (rye grass and clover) only due to high erodibility.