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SW69

Location: Barongarook West.

Australian Soil Classification: Bleached-Ferric (& Reticulate), Eutrophic, Brown CHROMOSOL (very thick loamy surface horizons)

General Landscape Description: Gently inclined undulating rises.
Site Description: Waning mid slope.
Geology: Hanson Plain Sand

Image: SW69 Landscape
SW69 Landscape


Soil Profile Morphology:


Surface Soil


A1h0-15/20 cmVery dark greyish brown (10YR3/2 moist and dry); sandy loam; apedal; pH 6.3; weak consistence; gradual change to:
South West Gasp Pipeline SW69 Profile
SW69 Profile. Note: Surface (A1) horizon has been stripped from the soil profile.

A21e

20-40 cm

Very pale brown (10YR7/4 moist), conspicuously bleached (10YR7/2 dry); sandy loam; clear change to:

A22g

40-60 cm

Very pale brown (10YR7/4 moist), conspicuously bleached (10YR7/2 dry); sandy loam; many (>25%) light yellowish brown (10YR6/4 moist) and dark yellowish brown (10YR4/6 moist) mottles; pH 5.7; clear change to:

A23c

60-100 cm

Irregular to rounded iron gravel (>80%) (10-30 mm) in very pale brown (10YR7/4 moist), conspicuously bleached (10YR7/2 dry); sandy loam matrix; abrupt change to:

Subsoil

B21tg100-150 cmVery dark grey (10YR3/1 moist) on ped faces, very distinct large reticulate mottles 40% grey (7.5YR6/1 moist), 50% yellowish brown (10YR5/8 moist), 10% yellowish red (5YR5/8 moist), brightest in ped centres; sandy light medium clay; medium polyhedral/blocky structure (<50 mm); pH 5.9:

C/Bg

150-230 cm

Very dark grey (10YR3/1 moist) on ped faces, mottled <20% grey (7.5YR6/1 moist), >60% yellowish brown (10YR5/8 moist), 10% yellowish red (5YR5/8 moist), brightest in ped centres; apedal except for B component; more sand than B21; pH 5.2:

2Bgb(?)

230 cm+

Very dark grey (10YR3/1 moist) on ped faces, 60% grey (7.5YR6/1 moist), 20% yellowish brown (10YR5/8 moist), 20% yellowish red (5YR5/8 moist), brightest in ped centres; pedal with dark clay/organic coatings (cutans); pH 5.2.


Key Profile Features:
  • Very thick conspicuously bleached subsurface (A2) horizons.
  • Larger amounts of ironstone gravel in deeper subsurface (A23) horizon.
  • Strong texture contrast between surface (A) horizons and subsoil (B21) horizon.
  • Strong reticulate mottling in deep subsoil.

Soil Profile Characteristics:

pH
Salinity Rating
Surface
(A1 horizon)
Slightly Acid
Very Low
Non-Sodic
None
Subsoil
(B21 horizon)
Moderately Acid
Very Low
Non-Sodic
None
Deeper Subsoil
(at 200-220 cm)
Strongly Acid
Very Low
-
-


Image: SW69 Graphs

The surface is slightly acid. The subsoil is moderately acid becoming strongly acid with depthSalinity rating is very low throughout the profile.The soil is non sodic throughout.Clay levels jump markedly at the surface / subsoil boundary.

Horizon
Sampling Depth
(cm)
pH
(water)
pH
(CaCl2)
EC
1:5
Organic Carbon
%
Nitrogen %
Exchangeable Cations
Ca
Mg
K
Na
meq/100g
A1
0-10
6.3
5.6
0.12
3.3
0.21
7.1
0.38
0.24
0.13
A22
40-55
5.7
4.7
<0.05
0.95
0.37
<0.05
<0.05
B21
110-130
5.9
5
0.06
0.79
6.6
0.11
0.55
C/Bg
200-220
5.2
4.3
0.05
2Bgb
260-280
5.0
4.1
0.09

Horizon
Sampling 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
0-10
<10
6.5
18.5
6.2
26.9
45.9
14.5
9
A22
40-55
26
3.9
12.7
2.8
30.4
42
18
9.5
B21
110-130
11
6.5
23
14.4
29.2
24.4
6
40
C/Bg
200-220
2Bgb
260-280



Notes:
Mapped as Tpb. Upslope (west of this profile) soil becomes much browner in B21 (7.5YR4/6). Gravel in A2 as before but finer and possibly more manganiferous (darker). Middle layer has angular, irregular and rounded iron-rich fragments of sandstone. Other fine (<10 mm) alluvials-rounded quartz gravel present.

Profile Described By: Richard McEwan (March1999).

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