Your gateway to a wide range of natural resources information and associated maps

Victorian Resources Online

LP42

Mapsheet: ST. ARNAUDAust. Soil Class.: Vertic (and Hypocalcic), Mesonatric, Brown SODOSOL
Northcote Factual Key: Dy 3.43Great Soil Group: solodized solonetz
General Landscape Description: Lower slope of rise near Reedy Creek. Original vegetation included Grey Box (E. microcarpa) and River Red Gum (E. camaldulensis).
Geology: Tertiary (Miocene) deposits. [Note: soil below 110 cm depth is part of an older landsurface].

Photo: Soil Pit Site LP42 Landscape
Soil Site LP 42 Landscape

Soil Profile Morphology

Surface Soil
A10-10 cmBrown (7.5YR4/4); sandy loam; very firm consistence dry; pH 5.6:Photo: Soil Pit Site LP42 Profile
Soil Site LP42 Profile
A210-15 cmYellowish brown (10YR4/4) conspicuously bleached; fine sandy loam; structureless; strong consistence dry; contains a few (10%) ferruginous nodules (3-8 mm size) and a few (5%) quartz fragments (3-8 mm size); tends to form a hard capping above underlying columnar structure; pH 5.9; sharp change to:
Subsoil
B2115-50 cmYellowish brown (10YR5/6) with yellowish red (5YR4/6) diffuse mottles; light medium clay; strong very coarse columnar, parting to weak coarse blocky structure; rigid consistence dry; pH 7.1:
B2250-110 cmYellowish red (5YR5/8); light clay; moderate very coarse blocky structure; slickensides present; very strong consistence dry; pH 8.6:
B3110 cm +Dark red (2.5YR4/6) and light grey (5YR7/1); light clay; moderate medium prismatic, parting down to moderate coarse blocky structure; strong consistence dry; contains a few (5%) quartz fragments (up to 10 cm size); pH 6.2.
Photo: Soil Pit Site LP42 Profile
Columnar structure in upper
Key Profile Features
  • Strong texture contrast between surface (A) horizons and subsoil (B21) horizons.
  • Dense and coarse columnar structure in upper subsoil.
  • Vertic properties in lower subsoil (evident by presence of slickensides and deep cracking).
  • The deep subsoil (from 110 cm+) is part of an older land surface (note the distinctive red and grey mottled colour, acid pH and prismatic structure).

Key Profile Characteristics

pH
Salinity Rating
Surface
(A1 horizon)
moderately acid
very low
non-sodic
none
Subsurface
(10 - 20 cm)
slightly alkaline
very low
strongly sodic
complete
Subsoil
(20 - 70 cm)
slightly acid
very low
strongly sodic
complete

Graph: pH levels in Soil Pit Site LP42
Graph: Salinity levels in Soil Pit Site LP42
Graph: Sodicity levels in Soil Pit LP 42

Horizon
Horizon Depth
pH (water)
pH CaCl2
EC 1:5
NaCl
Exchangeable Cations
Ca
Mg
K
Na
Meq/100g
A1
0-10
5.6
4.4
0.1
2.3
2.2
0.3
0.1
A2
10-15
5.9
4.5
<0.05
0.7
1.2
0.1
0.4
B21
15-50
7.1
4.7
<0.05
3.7
8.6
0.9
3.4
B22
50-110
8.6
4.7
0.05
4
8.8
0.2
6
B3
110
6.2
5.4
0.11
1.8
6.1
0.1
3.30

Horizon
Horizon Depth
Ex Al
mg/kg
Ex Ac
meq/100g
Field
pF2.5
Wilting Point
pF4.2
Coarse Sand
(0.2-2.0mm)
Fine Sand
(0.02-0.2mm)
Silt
(0.002-0.02mm)
Clay
(<0.002mm)
A1
0-10
18.7
5.4
A2
10-15
12.6
3.5
B21
15-50
30.7
17.1
B22
50-110
B3
110
Management Considerations:
Whole Profile
  • Plant available water capacity (PAWC) is likely to be low. Effective rooting depth will be restricted by the dense and coarsely structured sodic subsoil.
Subsoil (A) Horizons
  • Organic matter is important for enhancing soil aggregation, fertility and water holding capacity. Organic matter levels will build up under pasture but will decline if cultivation takes place. Practices such as residue retention, minimum tillage and including pasture rotations should be utilised if cropping occurs.
  • The bleached subsurface (A2) horizon indicates that periodic waterlogging occurs due to the slowly permeable subsoil.
  • The surface soil has a low inherent fertility (based on the sum of the exchangeable basic cations).
  • The low wilting point value for this soil suggests that plants will be able to utilise light rains falling when the soil is dry. However, if further rains do not occur the soil will become quite ‘droughty’.
Subsoil (B) Horizons
  • The dense and coarsely structured subsoil is strongly sodic, has a low Ca:Mg ratio, and is dispersive. As a result, root and water movement will be significantly restricted in the subsoil. After heavy rains, water will build up on top of the subsoil and waterlogging will result.
  • The dispersive subsoil is prone to water erosion if exposed by removal of the surface soil. Maintaining a protective cover of surface soil and vegetation is important, especially on sloping land. Also, sodic soils present constraints for dam construction which need to be managed.
  • The high levels of exchangeable sodium in the subsoil may also result in nutrient imbalances and may even have a toxic effect on some plants.
  • The subsoil displays vertic properties (i.e. slickensides and deep cracking) that indicate that significant shrinking and swelling occurs in the deeper subsoil. This may have implications for engineering purposes (e.g. disturbance to fences and tree roots).
Notes:
Profile described by Mark Imhof, Paul Rampant and Karen De Plater (22/3/95).
Page top