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EGW25

Location: Buchan

Australian Soil Classification: Haplic, Calcic, Brown DERMOSOL

Map Unit: Taravale (Component 1)
Previous Site Name: EG25

General Landscape Description: Steep hills
Site description: Mid slope, NE aspect, 27% slope
Land Use: Road reserve
Native Vegetation: Grassy woodland
Geology: Devonian limestone


Soils and landforms of the Buchan and Suggan Buggan region - Tarravale EG25 landscape


Soil Profile Morphology:

Surface soil
Soils and landforms of the Buchan and Suggan Buggan region - Tarravale EG25 profile
A0 – 25 cmVery dark brown (7.5YR4/2); clay loam (sub plastic); strong medium polyhedral structure; moderate amount (20-50%) subangular limestone pebbles (6 – 20 mm); clear change to:
Subsoil
B25 – 65 cmDark brown (7.5YR4/3); heavy clay; strong medium prismatic parting to fine prismatic structure; common (10-20%) subangular limestone pebbles (6 – 20 mm; abrupt change to:
C65– 85+ cmLight yellowish brown (10YR6/4) rubbly limestone.

*As the roadside cutting did not have a vertical slope the measurements on the tape will not show the true vertical depth
.
Key Profile Features:
  • High clay content throughout.
  • Strongly structured and deep soil.


Soil Profile Characteristics:

-

pH
Salinity
Sodicity
Surface soil
(A horizon)
Moderately acid
Very low
Non sodic
None
Subsoil
(B horizon)
Slightly acid
Very low
Non sodic
None


Chemical and Physical Analysis:
Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl
2)
EC
dS/m
Organic Carbon
%
Total
Nitrogen
%
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
A
0-25
5.9
5.3
0.1
2.3
0.18
9.1
11
1.4
0.72
0.17
12
19
26
40
33.8
16.6
B
25-65
6.7
5.9
0.1
9.4
19
2.2
0.71
0.27
2
6
11
78
40.9
25.3


Management Considerations
  • Plant available water (PAW) here is considered to be high, estimated to be 115 mm. Because of the variability in the depth of soil cover within this map unit, many soils will have low to very low water-holding capacity. Effective rooting depth is limited by the depth to rock.

Surface (A) horizons
  • The surface soil here is moderately acid. However because the soil has limestone in the subsoil, no response to additional lime would be anticipated.
  • The soil is low in soluble salts.
  • Potassium levels are high and plant responses to potassium fertiliser are unlikely.
  • The nutrient holding capacity of the surface A horizon is high (based on the sum of the exchangeable calcium, magnesium, potassium and sodium cations).

Subsoil (B) horizons
  • The subsoil would be relatively well drained and strongly structured which will enable plant roots to penetrate easily until they reach rock.

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