Property: Rutherglen Research Institute.
Paddock Number: PTD 2 (native grass).
Australian Soil Classification: Vertic (and Hypocalcic), Mottled-Subnatric, Grey SODOSOL.
Northcote Factual Key: Dy 3.43.
General Landscape Description: This site occurs in a paddock which has never been cultivated. Well developed gilgai microrelief is present.
Soil Mapping Unit: Unit 2 which is a gilgai complex containing four soil types: Rutherglen Loam (deep and normal phases), Lilliput Loam, Type D and Type E.
Site Description: This soil occurs on the edge of the depression component of the gilgai microrelief. It is similar to Lilliput Loam as described by Poutsma and Skene (1961).
Native Vegetation: Wallaby Grass (Danthonia sp.) commonly grows in the gilgai hollows.
Site NE37a Landscape |
Surface Soil |
Site NE37a Profile | ||
A1 | 0-20 cm | Brown (10YR4/3); fine sandy clay loam; firm consistence dry; rusty root channel mottling present; pH 5.8; abrupt change to: | |
A2 | 20-25 cm | Very pale brown (10YR7/3) conspicuously bleached; fine sandy clay loam; contains a few (5%) ferruginous and manganiferous nodules (5-10 mm size); pH 6.6; sharp change to: | |
Subsoil | |||
B21 | 25-70 cm | Light brownish grey (10YR6/2) with yellowish brown (10YR5/8) mottles; heavy clay; deep cracks evident; moderate very coarse prismatic structure (slickensides present at 50 cm); bleached material from above present along ped faces; rigid consistence dry; pH 6.7; gradual change to: | |
B22 | 70-110 cm | Light olive brown (2.5Y6/4); heavy clay; coarsely structured; large slickensides present; contains very few (2%) ferromanganiferous nodules; clear change to: | |
B23 | 110-140 cm | Light olive brown (2.5Y5/4); heavy clay; slickensides present; contains a trace (< 2%) amount of carbonate-silica nodules (2-10 mm size) and a few (5-10%) ferromanganiferous nodules (2-5 mm size); slickensides present; pH 8.8. |
The surface soil is moderately acid. The upper subsoil is slightly acid and the deeper subsoil is strongly alkaline. | The upper subsoil is sodic. The deeper subsoil is strongly sodic. Strong to complete dispersion occurs throughout the subsoil. | ||
The salinity rating is very low throughout the upper metre of the soil profile. It becomes low-medium at 120 cm depth. | The clay % increases significantly at the A/B horizon interface. |
Horizon | Horizon Depth (cm) | pH (water) | pH (CaCl2) | EC 1:5 | Exchangeable Cations | Field Capacity pF 2.5 | Wilting Point pF 4.2 | Coarse Sand (0.2 -2.0 mm) | Fine Sand (0.02 -0.2 mm) | Silt (0.002 -0.02 mm) | Clay (<0.002 mm) | |||
Ca | Mg | K | Na | |||||||||||
meq/100g | ||||||||||||||
A1 | 0-20 | 5.8 | 4.6 | <0.05 | 3.6 | 1.8 | 0.54 | 0.26 | 29 | 9 | 8 | 46 | 19 | 26 |
A2 | 20-25 | 6.6 | 4.9 | <0.05 | 2.7 | 2 | 0.18 | 0.46 | 22 | 6 | 10 | 49 | 22 | 21 |
B21 | 25-70 | 6.7 | 5.1 | 0.05 | 9.7 | 8.5 | 0.43 | 1.9 | 39 | 22 | 4 | 23 | 12 | 62 |
B22 | 70-100 | 6.9 | 6.1 | 0.37 | 8.9 | 10 | 0.4 | 4.2 | ||||||
B23 | 100-140 | 8.8 | 8.1 | 0.54 | 11 | 14 | 0.5 | 5 |