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Site CFTT9

Location: Maryvale.

Australian Soil Classification: Bleached-Sodic (& Vertic), Magnesic, Grey KUROSOL.
Great Soil Group: grey soloth.

Geology: Late Tertiary sediments.
General Landscape Description: Simple 2% slope to north west.
Mapping Unit: Maryvale.
Site Description: Eucalypt plantation.


Soil Profile Morphology:

Surface Soil

A10 – 20 cmVery dark greyish brown (10YR3/2); fine sandy loam; weak medium polyhedral structure; very weak consistence moderately moist; pH 5.1; clear and sharp transition to:

Photo: Site CFTT 9 Soil Profile
Site CFTT 9 Soil Profile
A220 – 40 cmBrown (10YR5/3), conspicuously bleached with a few medium distinct yellowish brown (10YR5/6) mottles; fine sandy loam; massive; very weak consistence dry; pH 5.0; abrupt and smooth transition to:

Subsoil

B2140 – 90 cmLight brownish grey (2.5Y6/2) with many coarse prominent yellowish brown (10YR5/6) mottles; medium clay; strong coarse prismatic, parting to moderate medium prismatic structure; strong consistence moist; pH 5.3; diffuse and smooth transition to:

B2290 – 125 cmLight grey (10YR7/1) with many prominent red (2.5YR4/6) mottles (and decreasing yellowish brown (10YR5/6) mottles); medium clay; moderate to coarse prismatic, parting to weak fine prismatic structure; strong consistence moist; pH 5.0; diffuse and smooth transition to:

B23125 – 200 cmLight grey (10YR7/1) with many, very coarse sized, prominent, red (2.5YR4/6) mottles; medium clay; moderate prismatic, parting to coarse lenticular structure, slickensides evident on ped faces; strong consistence moist.


Key Profile Features:


Soil Profile Characteristics:

Horizon
pH
Salinity Rating
Surface
(A1 horizon)
Strongly acid
Very low
Non-sodic
None
Subsoil
(B21 horizon)
Strongly acid
Low
Sodic
Slight 1
Deeper subsoil
(at 1 m)
Very strongly acid
Medium
Sodic
None
1Strong dispersion after remoulding.


Graph: Site CFTT 9, pH levels



The soil profile is strongly to very
strongly acid throughout.
Graph: Site CFTT 9, Exchangeable Aluminium



The level of exchangeable aluminium
is highest in the upper subsoil.
Graph: Site CFTT 9, Salinity Levels



The level of soluble salts increases
in the deeper profile.
Graph: Site CFTT 9, Clay %



There is a significant increase in clay
content at the A/B horizon interface
Graph: Site CFTT 9, Sodicity Levels




The subsoil becomes increasingly
sodic with depth.

Horizon
Horizon Depth
(cm)
pH
(water)
pH (CaCl2)
EC 1:5
NaC
%
Exchangeable Cations
Exchangable Aluminium
mg/kg
Exchangable Acidity
meq/100g
Field Capacity

pF 2.5
Wilting Point

pF 4.2

Coarse Sand (0.2 - 2 mm)
Fine Sand
(0.02 -0.2 mm)
Silt
(0.002 -0.02 mm)
Clay
(<0.002 mm)
Ca
Mg
K
Na
meq/100g
A1
0-20
5.1
4.3
0.06

1.2
0.68
0.16
0.15
62
9.4
23
5
14
52
19
10
A2
20-40
5
4.3
<0.05

0.24
0.28
0.09
0.09
43
4
15
3
17
54
19
9
B21
40-90
5.3
4.3
0.3
0.05
0.2
6.4
<0.1
1
120
8.8
32
18
9
24
15
48
B22
90-125
5
4.4
0.53
0.11
0.2
6.5
<0.1
2.1
84
7.8
36
19
5
20
21
52

Management Considerations:
Profile Described By: Ian Sargeant and Justin Wong (3/6/99).

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