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WCFA3

Location: Lower Norton

Australian Soil Classification: Hypercalcic, Mottled-Subnatric, Red SODOSOL


General Landscape Description: Rise of a ridge spur.
Site Description: Lower slope of a hillslope.
Geology: Parilla Sand

Image: WCFA3 landscape
WCFA3 Landscape

Soil Profile Morphology:

Surface Soil

Image: WCFA3 Profile
WCFA3 profile
A10-15 cmDark brown (7.5YR4/3); sandy loam; loose (cultivated) surface condition; weak very fine sub-angular blocky structure; rough fabric; firm consistence dry; contains a few, fine gravelly sub-rounded ferruginous fragments; pH 7.2; sharp and smooth change to:
Subsoil

B2115-30 cmRed (10R4/6) with many medium distinct pale brown (10YR6/3) and yellowish brown (5YR4/6) mottles; medium heavy clay; moderate coarse prismatic, parting to moderate medium prismatic structure; smooth fabric; strong consistence dry; contains very few fine gravelly sub-rounded ferruginous fragments; pH 6.9; clear and smooth change to:
B2230-45 cmWeak red (10R4/4) with common fine to medium, faint orange and grey mottles; heavy clay; moderate to strong coarse prismatic, parting to moderate to strong medium prismatic structure; smooth fabric; very strong consistence dry; contains very few fine gravelly sub-rounded ferruginous fragments; pH 7.8; clear and tongued change to:
B23k45-90+ cmMedium clay; strong, very coarse blocky, parting to strong medium blocky structure; smooth and rough fabric; very strong consistence dry; contains many coarse to extremely coarse calcareous segregations in patches; very highly calcareous; pH 8.7.

Soil Profile Characteristics:


pH
Salinity Rating
Surface
(A1 horizon)
Slightly Alkaline
Low
Non-Sodic
None1
Subsoil
(B21 horizon)
Slightly Acid
Low
Sodic
None2
Deeper Subsoil
(at 55-100 cm)
Strongly Alkaline
Medium
Sodic
None
1 Slight dispersion after remoulding. 2 Strong dispersion after remoulding.

Image: WCFA3 graphs
    The surface horizon is slightly alkaline. The upper subsoil is slightly acid. The deeper subsoil is strongly alkaline.
The salinity rating in the upper profile is low becoming medium at depth.
The surface is non-sodic. The subsoil is sodic.Boron content increases with depth.
    The clay content increases markedly at the surface / subsoil boundary.
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
7.2
6.9
0.2
-
8.3
0.95
1.1
0.17
B21
15-30
6.9
6.4
0.18
-
9.2
6.6
0.88
1.4
B22
30-45
7.8
7.2
0.28
<0.02
14
14
1.1
3.3
B23k
45-90
8.7
8.3
0.58
0.04
8.6
12
0.76
3.7

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
1.5
0.1
1
13.8
4.8
15
64
6
12
B21
15-30
2.5
26.4
15.4
11
38
5
42
B22
30-45
5.5
38.5
23.7
B23k
45-90
7.4
31.7
16.9

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