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IS34

Location: Longerenong


Australian Soil Classification: Calcic, Mesonatric, Red SODOSOL

Northcote Factual Key: Dr2.33
Great Soil Group: red brown earth
Soil Type: Drung Sandy Clay Loam

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

Soil Profile Morphology:

Surface Soil

A10-5 cm Dark reddish brown (5YR3/4); fine sandy clay loam; hardsetting surface condition; strong very coarse platy structure; strong consistence dry; pH 7.2; sharp boundary to:
Subsoil

B215-30 cm Dark reddish brown (5YR3/4); sporadically bleached (7.5YR7/3d); medium clay; moderate coarse blocky structure; strong consistence dry; pH 8.4; clear boundary to:


B22130-60 cmYellowish red (5YR4/6); light clay; subplastic; weak coarse blocky structure; very firm consistence dry; field pH 9.0; clear boundary to:

B22260-90 cmLight brown (7.5YR6/4) with faint pale brown (10YR6/3) mottles; light clay; subplastic; weak coarse blocky structure; very few (<2%) medium (2-6 mm) hard carbonate segregations; pH 9.0; gradual boundary to:

B22390-120 cmLight brown (7.5YR6/4) with faint pale brown (10YR6/3) mottles; light clay; subplastic; weak coarse blocky structure; very few (<2%) medium (2-6 mm) hard carbonate segregations; pH 9.0; diffuse boundary to:

B224120-150 cmBrown (10YR5/3) with faint reddish brown (5YR5/4) mottles; medium clay; weak very coarse blocky structure; strong consistence dry; very few (<2%) medium (2-6 mm) hard carbonate segregations; pH 9.0; clear boundary to:

B231k150-185 cmYellowish brown (10YR5/4) with faint reddish brown (5YR4/4) mottles; light medium clay; subplastic; weak coarse blocky structure; strong consistence dry; many (20-50%) coarse (6-20 mm) soft carbonate segregations; pH 9.0; gradual boundary to:

B232k185-200 cmBrown (10YR5/3) with faint reddish brown (5YR5/4) mottles; medium clay; weak coarse blocky structure; strong consistence dry; many (20-50%) coarse (6-20 mm) soft carbonate segregations; pH 9.0; gradual boundary to:

B233k200-215 cmBrown (7.5YR5/4) with faint reddish brown (5YR4/4) mottles; medium clay; weak very coarse blocky structure; strong consistence dry; many (20­50%) coarse (6­20 mm) soft carbonate segregations; pH 9.0.


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
Total
Nitrogen
%
Organic
Carbon
%
Exchangeable Acidity
cmol-/kg
Field
Capacity
-30okPa
Permanent
Wilting
Point
-1500okPa
Coarse
Sand
%
Fine
Sand
%
Silt
%
Clay
%
A1
0–5
7.2
0.12
0.03
3.9
4.5
1
1.1
0.09
1.0
4.5
20.7
10.3
23
38
12
26
B21
5–30
8.4
0.5
0.15
8.9
13.8
2
7.3
0.09
0.8
47.8
29.5
7
19
7
65
B221
30–60
B222
60–90
B223
90–120
B224
120–150
B231k
150–185
B232k
185–200
B233k
200–215

Management Considerations:
  • Strong texture contrast profile, possible uniform clay soil in places.
  • Neutral surface soil over alkaline subsoil, slightly decreasing at depth, high level of nutrients in upper subsoil (B22 horizon).
  • Thin surface soil with, poor structure and fine sand component; susceptible to compaction.
  • Upper subsoil is red, whole coloured suggesting oxidation and little water and air movement restriction.
  • Subsoil is sodic, becoming strongly sodic with depth and moderate to high salinity values in subsoil.
  • Subsoil is paler coloured and mottled below upper subsoil indicating some restricted drainage.
  • Landform element, plain; slow site drainage, unless near drainage line.

Profile Described By: John Martin, Nabil Badawy, Ron Cawood, Geoff Pope, John Galea, John Turner (1970).
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