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Site G4

Location: Rosedale.

Australian Soil Classification: Haplic, Eutrophic, Brown KANDOSOL

Geology: Recent sediments.
General Landscape Description: Flood plain of the La Trobe River.
Mapping Unit: La Trobe River.
Site Description: Soil auger site within a grazing paddock.

PHOTO: Soil site G4 landscape
Site GP4 Landscape


Soil Profile Morphology:

Surface Soil

A10-30 cm Dark brown (10YR3/3); very fine sandy clay loam; weak fine polyhedral structure; weak to firm consistence dry; pH 5.8; diffuse change to:


Subsoil

B2130-60 cmBrown (10YR4/3); very fine sandy clay loam; diffuse change to:

B2260-90+ cmBrown (10YR4/3) with strong brown (7.5YR5/6) mottles, very fine sandy clay loam, weak medium polyhedral structure; firm consistence moist; many macropores present; pH 5.8.

Key Profile Features:

Soil Profile Characteristics:

Horizon
pH
Salinity Rating
Surface
(A1 horizon)
Moderately Acid
Very Low
Non-Sodic
none
Subsoil
(B21 horizon)
Moderately Acid
Very Low
Non-Sodic
none
Deeper subsoil
(at 90 cm)
Moderately Acid
Very Low
Non-Sodic
none


GRAPH: Soil site G4 pH




The soil profile is moderately acid
throughout.
GRAPH: Soil Site G4 salinity


The salinity rating is very low
throughout the soil profile.
GRAPH: Soil Site G4 Clay %


The clay content is fairly uniform

throughout the soil profile.



Soil auger site G4 (Sargeant and Imhof, 2000)
Depth
cm
Texture
pH
EC 1:5
Nitrogen %
Carbon
%
Ca meq%
Mg meq%
K meq%
Na meq%
H
meq%
Coarse
sand
%
Fine
sand %
Silt
%
Clay
%
LAT
%
0-30
FSCL
5.8
0.2
0.18
3.8
3.5
3.4
0.1
0.5
8.5
2
46
21
27
1
30-60
FSCL
5.8
0.06
2.0
2.1
<0.1
0.2
7.2
2
55
23
20
1
60-90
FSCL
5.8
0.07
1.7
2.2
<0.1
0.2
7.1
2
55
23
20
1

The following abbreviation was used to describe field texture: FSCL - fine sandy clay loam.

Other symbols include: pH - analysed in water; EC - electrical conductivity; Cl - chloride; Ca - exchangeable calcium; Mg - exchangeable magnesium, K - exchangeable potassium; Na - exchangeable sodium; H - exchangeable hydrogen; ESP - exchangeable sodium percentage.

For Soil Pit Sites (Sargeant and Imhof, 2000) exchangeable cations have been determined using Gilman method (where pH >7) and Tucker method (pH <7). Exchangeable Sodium % (ESP) has been calculated here as the percentage of sodium in relation to the sum of the exchangeable basic cations.

Management Considerations:

Whole Profile
Profile Described By: Mark Imhof and Ian Sargeant.

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