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GP86

Location: near Lake Glenmaggie.Australian Soil Classification: Bleached-Mottled, Magnesic, Red KUROSOL (moderate profile depth).
Geology: Ordovician sediments.General Landscape Description: SE aspect, mid slope, hills.
Soil Mapping Unit: La TrobeSite Description: Roadside cutting adjacent to vegetation reserve.
Native Vegetation: Stringybark trees (approx. 15 m height).

Photo: Site EG4 Landscape
Site GP86 Landscape


Soil Profile Morphology:

Surface Soil

A10-5 cmBlack (10YR2/1); loam; pH 4.5:
Photo: Site EG4 Soil Profile
Site GP86 Profile
A215-25 cmBrown (10YR5/3) conspicuously bleached; light sandy loam; hydrophobic; pH 5.0:
A2225-40 cmYellowish brown (10YR5/4) conspicuously bleached; sandy loam; pH 5.1:
Subsoil
B2140-60 cmDark red (2.5YR4/6) with reddish yellow (7.5YR6/8) and grey (10YR6/1) mottles; medium heavy clay; moderate medium to fine polyhedral structure; pH 5.1:
C60 cmWeathered sandstone.

Key Profile Features:
  • Strong texture contrast between surface (A) horizons and subsoil (B21) horizon.

Soil Profile Characteristics:

Horizon
pH
Salinity Rating
Surface
(A1 horizon)
Very Strongly Acid
Very Low
Non-Sodic
None
Subsoil
(B21 horizon 40-60 cm)
Strongly Acid
Very Low
Non-Sodic
None

Graph: pH levels in Site EG4

Graph: Ex. Aluminium
Graph: Sodicity levels in Site EG4
Graph: Clay % in Site EG4


Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl2)
EC 1:5
NaCl
Exchangeable Cations
Ca
Mg
K
Na
meq/100g
A1
0-5
4.5
3.8
0.06
1.5
0.90
0.43
0.30
A21
5-25
5.0
4.5
0.08
0.27
0.61
0.20
0.26
A22
25-40
5.1
4.6
0.09
0.10
0.90
0.250
0.31
B21
40-60
5.1
4.2
0.07
0.15
4.9
0.51
0.54

Horizon
Horizon Depth
(cm)
Exchangeable Aluminium
mg/kg
Exchangeable Acidity
meq/100g
Field Capacity
pF2.5
Wilting Point
pF4.2
Coarse Sand
(0.2-2.0 mm)
Fine Sand
(0.02-0.2 mm)
Silt
(0.002-0.02 mm)
Clay
(<0.002 mm)
A1
0-5
82
16
23
50
11
7
A21
5-25
55
5.3
20
57
14
6
A22
25-40
71
5.9
20
52
14
11
B21
40-60
300
12
14
25
9
50

Management Considerations:

Subsoil (B) Horizons
  • The subsoil has very low levels of exchangeable calcium compared to exchangeable magnesium (i.e. magnesic). This indicates that nutrient imbalances (e.g. calcium deficiency) may occur.
  • The level of exchangeable aluminium becomes quite high in the strongly acid subsoil. This is likely to restrict the growth of aluminium-sensitive species.
  • The subsoil horizons are non-sodic and well structured (parting to fine polyhedral peds). This will enhance root and water movement (apart from any chemical restrictions to plant growth).
Profile Described By: Mark Imhof and Ian Sargeant (May 2004).
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