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IS35

Location: Longerenong

Australian Soil Classification: Episodic, Epipedal, Grey VERTOSOL

Northcote Factual Key: Ug5.5
Great Soil Group: grey clay
Soil Type: Murtoa Clay.


General Landscape Description: Anastomotic plain.
Geology: Quaternary Coonambidgal Formation: fluvial to lacustrine clays and sands.

Soil Profile Morphology:

Surface Soil

A10-5 cmGrey (10YR5/1) conspiuously bleached (10YR5/1); medium heavy clay; cracking surface condition; massive very coarse blocky, parting to strong medium blocky structure; very strong consistence dry; pH 7.1; sharp boundary to:
Subsoil

B2115-30 cmDark grey brown (10YR4/2); heavy clay; strong coarse prismatic structure; very strong consistence dry; pH 7.7; clear boundary to:

B21230-60 cmDark grey brown (2.5Y4/2); light medium clay; subplastic; moderate very coarse blocky structure; very strong consistence dry; pH 7.5; gradual boundary to:

B21360-85 cmDark grey brown (2.5Y4/2); medium clay; weak coarse blocky structure; very strong consistence dry; pH 8.0; gradual boundary to:

B2285-120 cmGrey brown (2.5Y5/2); light clay; weak coarse blocky structure; very strong consistence dry; field pH 8.0; clear boundary to:

B231120-150 cmLight brownish grey (2.5Y6/2); light clay; weak very coarse blocky structure; very strong consistence dry; field pH 8.0; gradual boundary to:

B232150-215 cmLight brownish grey (2.5Y6/2); light clay; weak very coarse blocky structure; very strong consistence dry; field pH 7.5.

Chemical and Physical Analysis:


Horizon
Sample Depth cm
pH
H2O
EC
dS/m
Sodium Chloride
%
Exchangeable Calcium
cmol-/kg
Exchangeable
Magnesium
cmol-/kg
Exchangeable Potassium
cmol-/kg
Exchangeable Sodium
cmol-/kg
Organic
Carbon
%
Exchangeable Acidity
cmol-/kg
Field
Capacity
-30okPa
Permanent
Wilting
Point
-1500okPa
Coarse
Sand
%
Fine
Sand
%
Silt
%
Clay
%
A1
0–5
7.1
0.16
0.04
5.4
10.2
0.8
1.7
0.7
5.9
29.2
16.8
2
31
24
42
B211
5–30
7.7
0.37
0.09
8
13.3
0.6
5.9
0.6
4.8
42
27.2
1
16
19
63
B212
30–60
B213
60–85
B22
85–120
B231
120–150
B232
150–215

Management Considerations:
  • Cracking clay profile, high clay percentage.
  • Neutral thin surface soil and alkaline below.
  • Massive, occasionally moderately structured surface, does not have high level friability/self-mulching, making plant germination more difficult.
  • Calcium percentage relatively low and sodium comparatively high in surface and upper subsoil, greater structural resistance to plant growth.
  • Lighter coloured deep subsoil, poorer internal drainage.
  • Subsoil is likely to be strongly sodic and salinity increases at depth.
  • Cracking may allow air and seasonal moisture to penetrate.
  • Very strong consistence when dry, implications for compaction and implement use.
  • Landform element, plain: poor site drainage.
Profile Described By: John Martin, Nabil Badawy, Ron Cawood, Geoff Pope, John Galea, John Turner (1970).
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