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YP4

Location: Wallup


Australian Soil Classification: Epicalcareous-Endohypersodic, Self-Mulching, Grey VERTOSOL

General Landscape Description: Clay plain.
Site Description: Cropping paddock.
Geology: Quaternary alluvial and aeolian deposits.

Image: YP4 landscape

YP4 Landscape


Soil Profile Morphology:

Surface Soil

Ap10-4 cmGrey (10YR5/1); self-mulching surface condition; light medium clay; very highly calcareous; pH 8.1; clear change to:Image: YP4 profile
YP4 Profile
Ap24-18 cmGrey (2.5Y5/1); medium clay; moderate coarse blocky structure; firm to strong consistence dry; highly calcareous; pH 8.3; clear change to:
Subsoil
B2118-45 cmDark grey (10YR4/1); medium heavy clay; moderate to coarse prismatic, parting to strong coarse angular blocky, parting to strong fine sub-angular blocky structure (in patches); very highly calcareous; pH 8.9; clear change to:
B22

45-80 cmDark grey (10YR4/1); medium heavy clay; moderate coarse prismatic, parting to strong coarse sub-angular blocky structure; few (5%) fine-earth carbonates; very highly calcareous; gradual change to; pH 9:
B2380-120 cmLight yellowish brown (10YR6/4); light medium clay; strong very coarse prismatic structure; very highly calcareous; pH 9.
Soil Profile Characteristics:

-

pH
Salinity
Surface
(A1 horizon)
Moderately Alkaline
Low
Non-Sodic
Strong
Subsoil
(B21 horizon)
Moderately Alkaline
Low
Sodic
None 1
Deeper Subsoil
(at 80-100 cm)
Strongly Alkaline
High
Extremely Sodic (40%)
Slight 2
1 Slight dispersion after remoulding. 2 Reduced dispersion due to high level of soluble salts - moderate to strong dispersion occurs after remoulding.

Image: YP4 graphs
The surface is moderately alkaline. The upper subsoil is moderately alkaline, becoming strongly alkaline with depth.The salinity rating is low in the surface and upper subsoil, becoming high in the deeper subsoil.The surface is non-sodic. The upper subsoil is sodic becoming extremely sodic with depth.
    The clay content is high throughout the profile.
Boron is relatively low in the upper soil profile, but becomes high below 50 cm depth.

Chemical and Physical Analysis:


Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl2)
EC
dS/m
Sodium Chloride
%
Exchangeable Cations
Organic Carbon
%
Total Nitrogen
%
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)
Ca
Mg
K
Na
meq/100g
Ap1
0-4
8.1
7.6
0.28
29
5.6
2.3
0.37
1
0.096
1.7
37.8
19.2
15
18
15
42
Ap2
4-18
8.3
7.7
0.17
36
5.2
1.7
0.42
0.96
0.094
1.4
38.4
19.4
17
18
13
44
B21
18-45
8.9
7.9
0.19
6.5
5
0.18
0.86
0.68
0.061
2.3
40
21.4
20
20
13
44
B22
45-80
9
8.4
1.1
0.14
14
13
1.4
13
16
51
24.3
14
14
13
51
B23
80-100
9
8.5
1.6
0.22
11
11
1.7
16
24
49.4
23.7
12
14
11
48

Profile Described By:
Mark Imhof (October 2008).
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