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CRC10

Location: Ararat

Australian Soil Classification: Mottled-Sodic, Magnesic, Yellow DERMOSOL
General Landscape Description: Mid-slope of hill (SE aspect) - colluvial slope.
Site Description: Grazing paddock – runoff demonstration site.
Geology: Ordovician thinly bedded shale (micaceous).


Image:  GH1-4 - Landscape
CRC10 Landscape


Soil Profile Morphology

Surface Soil


A1

0-5 cm

Brown (10YR4/3);
fine sandy loam; weak to moderate coarse-medium blocky structure; weak consistence, moderately moist; pH 4.9; clear change to:
Image:  GH1 profile
CRC10 Profile






A2

5-10 cm

Light yellowish brown (10YR6/4); some rusty mottling; sporadically bleached;
fine sandy loam; weak to moderate coarse-medium blocky structure; weak consistence, moderately moist; pH 5.2; clear change to:

A22

10-25 cm

Very pale brown (10YR7/3) with brownish yellow (10YR6/8) mottles;
light silty clay loam; weak to moderate medium-fine blocky structure; firm consistence, moderately moist; macropores (with some infill of A horizon material); pH 5.4; clear change to:
Subsoil

B1

25-45 cm

Light yellowish brown (10YR6/4) with brownish yellow (10YR6/8) mottles;
clay loam (very fine sandy); weak to moderate coarse-medium blocky structure; firm consistence, slightly moist; pH 5.8; gradual change to:

B21

45-55 cm

Light yellowish brown (10YR6/4) with reddish yellow (7.5YR6/8) mottles;
fine sandy light clay; firm consistence, moderately moist; pH 6.3; clear change to:

B22

55-70 cm

Brownish yellow (10YR6/6) with reddish yellow (7.5YR6/8) mottles;
medium clay; moderate-strong coarse-medium blocky structure; firm consistence, moist; pH 6.7; gradual change to:

B23

70-85 cm

Brownish yellow (10YR6/6) with brownish yellow (10YR6/8) mottles;
light clay (silty); moderate very coarse parting to strong coarse-medium blocky further parting to moderate-strong fine polyhedral structure; firm consistence, moist; very few quartz fragments; pH 7.0; gradual change to:

B24

85-110 cm

Brownish yellow (10YR6/6) with reddish yellow (5YR616) mottles;
light clay (silty); moderate-strong coarse, parting to medium, parting to fine polyhedral structure; firm consistence, moderately moist; some manganese staining (2%); pH 7.0; gradual change to:

BC

110+ cm

Light grey (10YR7/1) with reddish yellow (7.5YR6/8) and yellowish red (5YR5/8) mottles;
fine sandy clay loam; moderate coarse-medium polyhedral structure; weak consistence, moderately moist; manganese staining (5%); pH 7.8.

Key Profile Features
  • Gradual increase in clay content (texture) with depth down the upper soil profile.


Key Profile Characteristics

pH
Salinity Rating
Surface
(A1 horizon)
Very Strongly Acid
Very Low
Non-Sodic
None
Subsoil
(B21c horizon)
Slightly Acid
Very Low
Non-Sodic
None1
Deeper subsoil
(at 110+ cm)
Moderately Alkaline
Very Low
Sodic
Strong
1 Strong to complete dispersion after remoulding
Image: GH1 graphs


Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl
2)
EC
dS/m
Exchangeable Aluminium
ppm
Exchangeable Acididty
meq/100g
Exchangeable Cations
Coarse Sand
(0.2-2.0 mm)
%
Fine Sand
(0.02-0.2 mm)
%
Silt
(0.002-0.02 mm)
%
Clay
(<0.002 mm)
%
Field Capacity
% w/w
Wilting Point
% w/w
Bulk Density
g/cm3
Ca
Mg
K
Na
meq/100g
A1
0-5 cm
4.9
4.6
0.19
20
16
4.8
2
0.82
0.38
9
40
10
25
32.5
13.8
0.97-1.01
(1.00)
A21
5-10 cm
5.2
4.5
<0.05
33
6.4
1.6
1.1
0.11
0.17
1
53
24
16
22.4
5.7
1.02-1.16
(1.09)
A22
10-25 cm
5.4
4.6
<0.05
23
2.8
1.1
0.98
0.09
0.13
1
44
27
12
18.5
4.6
1.0-1.20
(1.11)
B1
25-45 cm
5.8
5
<0.05
19
4.1
1.1
3.1
0.12
0.25
4
49
24
22
19
8
B21
45-55 cm
6.3
5.2
<0.05
12
6
0.88
5.4
0.17
0.43
3
39
25
29
26
11.5
B22
55-70 cm
6.7
5.8
0.05
5.2
0.60
7.0
0.23
0.68
2
29
31
38
24.3
12.5
1.46-1.53
(1.48)
B23
70-85 cm
7.0
6.0
0.08
4.7
0.52
9.2
0.28
1
3
32
28
33
27.1
14
B24
85-110 cm
7.8
6.5
0.07
0.43
11
0.19
1.5
4
32
34
28
26.1
12.4
B/C
110+ cm
8.2
6.6
0.05
0.15
10
0.13
1.6
23.5
8.7
1.51-1.61
(1.54)


Management Considerations:
  • The subsoil has very low levels of exchangeable calcium compared to exchangeable magnesium (i.e. magnesic). This indicates that nutrient imbalances may occur (e.g. calcium deficiency).
  • The subsoil is dispersive (strongly dispersive at 70 cm depth), which will restrict the movement of roots and water at depth.


Profile described By: Mark Imhof, Austin Brown and Malcolm McCaskill - November 2003.
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