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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:


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 Surface horizon (A1) Subsurface horizons (A2 and A3)

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