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WCFA1

Location: Lower Norton

Australian Soil Classification: Endocalcareous-Endohypersodic, Epipedal, Grey VERTOSOL


Soil Map Unit: Similar to Murtoa Clay.

General Landscape Description: Rise within a ridge spur. Wind erosion evident.
Site Description: Mid to upper hill slope.
Land Use: Cropping paddock.
Geology: Parilla Sand.

Image: WCFA1 landscape
WCFA1 Landscape

Soil Profile Morphology:

Surface Soil
Image: WCFA1 Profile
WCFA1 profile
A10-15 cmVery dark greyish brown (10YR3/2); light clay; loose surface condition; weak fine sub-angular blocky structure; strong consistence dry; rough fabric; contains very few fine gravely sub-angular quartz fragments; pH 7.6; gradual and smooth change to:
Subsoil
B2115-40 cm Very dark grey (10YR3/1); light clay; strong coarse prismatic, parting to strong medium angular blocky structure; smooth fabric; strong consistence dry; contains very few soft calcareous segregations; few distinct slickensides evident; pH 8.3; gradual and smooth change to:
B2240-60 cmDark grey (2.5Y4/1); medium clay; strong coarse prismatic, parting to strong medium angular blocky structure; smooth fabric; very strong consistence dry; contains very few soft calcareous segregations; many distinct slickensides evident; pH 8.7; clear and irregular change to:
B23k60-80+ cmMedium heavy clay; strong coarse to medium angular blocky structure; smooth fabric; very strong consistence dry; soft calcareous segregations common; many distinct slickensides evident; pH 8.9.

Soil Profile Characteristics:


pH
Salinity Rating
Surface
(A1 horizon)
Slightly Alkaline
Low
Non-Sodic
None
Subsoil
(B21 horizon)
Moderately Alkaline
Low
Sodic
None
Deeper Subsoil
(at 60-80 cm)
Moderately Alkaline
Low-Medium
Strongly Sodic
None1
1 Slight dispersion after remoulding.

Image: WCFA1 graphs
    The surface is slightly alkaline. The subsoil is moderately alkaline.
The salinity rating is low to medium throughout the whole profile.
The surface is non-sodic. The upper subsoil is sodic and the deeper subsoil becomes strongly sodic.The boron content increases with depth.
    The clay content is high throughout and gradually increases with depth.
Chemical and Physical Analysis:

Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl2)
EC
dS/m
NaCl
%
Exchangeable Cations
Ca
Mg
K
Na
meq/100g
A1
0-15
7.6
7.3
0.24
-
27
4.7
1.4
0.45
B21
15-40
8.3
7.8
0.29
<0.02
23
9.4
0.57
2.1
B22
40-60
8.7
8.1
0.41
<0.02
21
14
0.55
4.1
B3k
60-80
8.9
8.3
0.51
<0.02
18
16
0.63
6.3

Horizon
Horizon Depth
(cm)
Oxidisable Organic Carbon
%
Total
Nitrogen
%
Available
Boron
mg/kg

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
1.7
0.16
2
34.4
21.1
12
34
12
35
B21
15-40
2
31.6
19.2
11
39
9
37
B22
40-60
5.1
38.3
21.5
11
33
9
43
B3k
60-80
11
40.9
23.4

Profile Described By:
Nathan Robinson, Grant Boyle and John Martin (October 2006).
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