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EGW40

Location: Gelantipy

Australian Soil Classification: Acidic, Regolithic, Bleached-Orthic TENOSOL

Map Unit: Wulgulmerang (Component 1)
Previous Site Name: EG40

General Landscape Description: Undulating rises
Site description: Upper slope of low hill, 4% slope, auger sample on roadside
Native Vegetation: Montane dry woodland
Geology: Devonian acid volcanics (Snowy River Volcanics)


Soils and landforms of the Buchan and Suggan Buggan region - Wulgulmerang EG40 landscape

Soil exposed adjoining road near site


Soil Profile Morphology:

Surface Soil
A1

0 – 10 cmWeak red (2.5YR4/2); sandy loam; weak angular blocky structure; very weak consistence moist, pH 6.2; clear change to:


A210 – 50 cmLight brownish grey (10YR6/4) mottled with pale yellow (2.5Y8/4); coarse sandy loam; single grain; very weak consistence dry; few small gravel; pH 5.0; gradual change to:


A350 – 70+ cmYellowish brown (10YR5/6), pale yellow dry; coarse loamy sand (2.5Y7/2); massive; weak consistence dry; common subangular small gravel; pH 5.0.

Key Profile Features:
  • Very sandy and no texture change throughout the profile.


Soil Profile Characteristics:

-

pH
Salinity
Surface soil
(A1 horizon)
Slightly Acid
Very Low
Non-sodic
Minimal Aggregation
Subsoil
(A2 horizon)
Strongly Acid
Very Low
Non-sodic
Minimal Aggregation
Deeper subsoil
(50-70 cm)
Strongly Acid
Very Low
Non-sodic
Minimal Aggregation


Chemical and Physical Analysis:
Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl
2)
EC
dS/m
Organic Carbon
%
Total
Nitrogen
%
Exchangeable Aluminium
ppm
Exchangeable Acididty
meq/100g
Exchangeable Cations
Coarse Sand
(0.2-2.0 mm)
%
Fine Sand
(0.02-0.2 mm)
%
Silt
(0.002-0.02 mm)
%
Clay
(<0.002 mm)
%
Field Capacity
% w/w
Wilting Point
% w/w
Ca
Mg
K
Na
meq/100g
A1
0-10
6.2
5.7
0.07
1.4
0.1
<1
4.8
5.5
1.0
0.31
0.05
38
31
18
9
23.9
6.0
A2
10-50
5.0
4.4
<0.05
83
4.9
0.94
0.26
0.16
0.06
33
36
22
8
18.2
3.6
A3
50-70
5.0
4.4
0.05
88
3.7
0.81
0.42
0.18
0.07
38
31
22
10
17.5
4.4


Management Considerations

Whole profile
  • Apart from the immediate surface soil, the soil is strongly acid throughout. The calcium levels and the pH of the surface soil indicate lime has possibly been applied in the past, but further evaluation may be needed in the future.
  • The plant available water content is low, estimated at 53 mm for a rooting depth of 70 cm. This figure will depend on the degree to which the roots can penetrate the massive A2 and A3 horizon, and overcome the strongly acid conditions.
Surface horizon (A1)
  • The organic matter content of the soil is very low. As the soil was sampled by auger on the road reserve, this may not reflect the conditions in the paddock.
  • The low wilting point of the surface horizons indicates plants will be able to use light rains when the soil is dry. Due to the low water storage capacity of the soil, plants will suffer water stress unless further rains occur.
  • The nutrient holding capacity of the soil is low (based on the sum of the exchangeable cations).
  • Potassium levels are bordering on deficiency level, but no response would be expected at this stage.
  • Strongly acidic subsurface horizon with moderate to high exchangeable aluminium levels may restrict growth of aluminium sensitive species such as lucerne.
Subsurface horizons (A2 and A3)
  • The hard setting nature of the A2 and A3 horizons, together with the strong acidity of the profile may impede root penetration.


Profile Described By: David Rees and Grant Boyle, 2000.
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