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Site GN13

Location: Dookie.
Australian Soil Classification: Endohypersodic, Epipedal, Grey VERTOSOL.Great Soil Group: grey clay.
General Landscape Description: Level plain.Soil Mapping Unit: Congupna clay (Downes, 1949).
Soil Management Unit (Briggs 1995): 'Grey Clay - Dookie'.
Occurrence: Generally found on the outskirts of the Land Management Group area on the flat low-lying country, particularly along water courses and depressions.
Site Description: Pasture.
Native Vegetation: The dominant tree species are Grey box (Eucalyptus microcarpa) and Buloke (Casuarina luehmannii). Yellow box (Eucalyptus melliodora) and Sheoak (Casuarina stricta) can be found on the lighter and better-drained soils. River red gum (Eucalyptus camaldulensis) is associated with the water courses.
Graph: Site GN13 Landscape
Site GN13 Landscape

Soil Profile Morphology:

Surface Soil


A10-10 cmBrown (10YR4/3); light clay; weak medium blocky structure; strong consistence (dry); rusty root channel mottling (10%); pH 5.5; sharp change to:

Photo: Site GN13 Profile
Site GN13 Profile
A210-25 cmGreyish brown (10YR5/2); conspicuously bleached (10YR8/1 dry); silty clay; few (5%) hard ferruginous nodules (< 10 mm in size).

Note: There is a discontinuous A2 horizon that may or may not be present. It is probably associated with the depression component of gilgai microrelief.

Subsoil

B2110-25 cmDark grey (10YR4/1) with diffuse yellowish brown (10YR5/6) mottles; heavy clay; strong coarse blocky, parting to strong medium to coarse prismatic structure; strong consistence (moist); very few (2%) soft (manganiferous?) segregations ( 5 mm in size); pH 7.2; clear change to:

B2225-70 cmDark grey (10YR /1); heavy clay; strong coarse lenticular, parting to moderate fine lenticular structure; strong consistence (moist); pH 8.2; clear change to:

B2370+ cm Dark brown (10YR 4/3); heavy clay; firm consistence (moist); very few gypsum crystals (nests of 1-2 mm in size); slight effervescence; pH 8.3.


Key Profile Features:

Soil Profile Characteristics:

pH
Salinity Rating
Surface soil
(A1 horizon)
Strongly Acid
Low
Non-Sodic
None
Upper subsoil
(10 - 25 cm)
Slightly Alkaline
Very Low
Sodic
None1
Deeper subsoil
(at 70+ cm)
Moderately Alkaline
High
Strongly Sodic
None2
1Strong dispersion after remoulding. 2Probably due to high levels of soluble salts.
Graph: Site GN13 pH levels
Graph: Site GN13 Salinity levels
Graph: Site GN13 Sodicity levels
Graph: Site GN13 Clay%
Horizon
Horizon
Depth

(cm)
pH
(water)
pH
(CaCl
2)
EC 1:5
Exchangeable Cations
Exch.
Al

mg/kg
Exch.
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
0-10
5.5
4.8
0.20
6.5
6.3
0.7
0.4
<10
13
35.4
15.7
6.4
26.1
24.0
35.0
B21
10-25
7.2
5.9
0.06
12.1
16.2
1.1
2.3
<10
8.5
43.1
21.5
1.3
13.0
14.0
65.0
B22
25-70
8.2
7.0
0.16
12.1
18.3
0.8
4.1








B23
70+
8.3
7.8
1.04
10.1
17.0
0.8
6.3









Management Considerations (Briggs 1995):

Favourable Characteristics

Limiting Features
Cropping Considerations
Pasture Considerations

References:

Management Considerations based on booklet: ' Soil Management Units in the Dookie Land Management Group Area' - compiled by Suzanne Briggs. Agriculture Victoria,1995.

Downes R.G. (1949). 'Soil, Land-Use, and Erosion Survey around Dookie, Victoria' , Bulletin 243, CSIRO, Victoria.

Profile Described By: Mark Imhof, John Martin and Sonia Thompson (4/5/94).