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SW74

Location: Tulloh

Australian Soil Classification: Bleached-Vertic, Eutrophic, Brown CHROMOSOL

General Landscape Description: Undulating low hills.
Site Description: Waxing upper slope, western aspect.
Geology: Thin Tertiary (Dilwyn or Eastern View Formation) over Cretaceous (Otway Group) unconformity.

Image: SW74 Landscape
SW74 Landscape


Soil Profile Morphology:


Surface Soil


A10-15 cmVery dark grayish brown (10YR3/2 moist), dark gray (10YR4/1 dry); loamy sand; apedal; hardsetting; pH 5.4; clear change to:
South West Gasp Pipeline SW74 Profile
SW74 Profile. Note: Surface (A1) horizon has been stripped from the soil profile.
A215-40 cmOlive brown (2.5Y4/3 moist) with faint mottling, conspicuously bleached (2.5Y6/3 dry); sandy loam; apedal, massive; contains few medium ferruginous nodules; pH 5.6; sharp and wavy change to:
Subsoil

B21t40-70/80 cmSandy yellowish brown (10YR5/6) coarse angular blocky peds with dark grayish brown (10YR4/2) thick heavy clay coatings; some peds dominantly clay; vertic features; pH 6.0; gradual and wavy change to:
B22tg70/80-140+ cmWhite (gray N8/0) clay with gray (10YR5/1) coatings; red mottles in white clay; strongly vertic; pH 5.5. This horizon is probably a palaeosol developed on Otway Group sediments.

Key Profile Features:
  • Conspicuously bleached subsurface (A2) horizon
  • Strong texture contrast between surface (A) horizons and subsoil (B21) horizon.

Soil Profile Characteristics:

pH
Salinity Rating
Surface
(A1 horizon)
Strongly Acid
Low
Non-Sodic
None
Subsoil
(B21 horizon)
Moderately Acid
Very Low
Non-Sodic
None
Deeper Subsoil
(at 100+ cm)
Strongly Acid
Very Low
Non-Sodic
None


Image: SW74 Graphs

The surface soil is strongly acid. The subsoil is moderately acid becoming strongly acidic with depth.Salinity rating is low in the surface becoming very low in the subsoil.
    The soil is non sodic throughout.
The clay content increases markedly at the A/B boundary.

Horizon
Sample Depth
(cm)
pH
(water)
pH
(CaCl2)
EC
1:5
Organic Carbon
%
Nitrogen
%
Exchangeable Cations
Ca
Mg
K
Na
meq/100g
A1
0-15
5.4
4.7
0.14
7.6
0.65
2.6
0.97
0.37
0.27
A2
25-35
5.6
4.8
0.05
0.74
0.91
0.05
0.14
B21t
45-65
6
5.3
0.08
1.9
5.2
0.08
0.49
B22tg
100-120
5.5
4.4
0.08
1.4
8.2
0.11
0.8

Horizon
Sample 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
0-15
21
13
22.2
9.5
39
35
11
9
A2
25-35
15
5.3
13.7
4.2
46
28
13
10
B21t
45-65
<10
7.3
28.4
18.6
37
8
4
48
B22tg
100-120
13


Management Considerations:

Notes

  • Possible unconformity of Palaeocene over Cretaceous.
  • Strongly vertic with trench collapse.
  • This site stood out from adjacent sections of the trench, because of white subsoil material in trench spoil.

Profile Described By: Richard McEwan (April 1999).
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