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GL100

Location: Casterton

Australian Soil Classification: Melanic, Subnatric, Brown SODOSOL (confidence level 1)
General Landscape Description: Rises, low hills
Site Description: Upper slope, 10%.
Land Unit: Merino Tablelands
Geology: Cretaceous non-marine sandstone

General Land Unit Description: This unit consists of the Cretaceous non-marine sandstone of the dissected Merino Tablelands. The tablelands were thought to have formed under swamp conditions and a warm climate. As a result, the soils tend to be high in clay and there tends to be carbon rich seams of charcoal deposits at depth in some of the profiles. The main soil type used to represent this land unit is black cracking clays (Vertosols) that can be sodic at depth. This soil type, along with Black Sodosols, Chromosols and Dermosols, are commonly found on the broad crests or drainage lines. The slopes often consist of Brown Chromosols, Sodosols or Dermosols, although black soils can also occur on the slopes. The lower slopes commonly have Grey Vertosols or Sodosols as the major soil type. The reasonably deep sodic soils on short steep slopes tend to be prone to landslips. The grey soils, in particular are prone to water erosion.

Soil pit GL99 landscape

Soil pit GL100 auger




Soil Profile Morphology


A10-20 cmVery dark brown (10YR2/2); clay loam; strong very fine subangular blocky structure; very firm consistence, dry; contains very few sedimentary fragments; pH 5.8; changes to:


Subsoil


B2120-40 cmDark brown (10YR3/3); light medium clay; medium to strong medium columnar to subangular blocky structure; very firm consistence, dry; pH 6.2; changes to:


B2240-60 cmDark brown (10YR3/3), with common orange mottles; medium clay; weak to medium subangular blocky structure; very firm consistence, moderately moist; pH 7.3; changes to:


B2360-80 cmBrown (10YR4/3), with many light brown mottles; medium heavy clay; weak to medium subangular blocky structure; very firm consistence, moderately moist; pH 8.3; changes to:


B380-95 cmLight olive brown (10YR5/4); fine sandy light clay; very firm consistence, moderately moist; pH 9.1; changes to:


BC95-105 cm



C105+ cm

Key profile features:
  • Alkaline subsoil
  • Sodic subsoil
  • Mottled subsoil
  • Topsoil dispersive when worked when wet
  • Top of subsoil dispersive when worked when wet



Soil Profile Characteristics:
-

pH
Salinity
Surface Soil
(A1 horizon)
Moderately Acid
Low
Non-Sodic
None1
Subsoil
(20-40cm)
Slightly Acid
Very Low
Sodic
None2
Deeper Subsoil
(80 -95 cm)
Very Strongly Alkaline
Medium
-
Strong2
1Strong dispersion after remoulding (20 hrs). 2Compete dispersion after remoulding (20 hrs).

Soil pit GL100 graphs

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
0-20
5.8
4.8
0.14
2.5
0.25
27
16
4.9
5.3
0.84
1.3
2
32
27
34
36.5
18.4
B21
20-40
6.2
4.7
0.11
63
15
3.7
8.2
0.98
3.2
1
25
26
45
39.0
20.6
B22
40-60
7.3
6.1
0.22
6.1
16
1.3
5.6
1
19
21
58
48.2
25.7
B23
60-80
8.3
7.3
0.25
6.9
18
1.2
6.5
1
22
23
54
49.1
28.6
B3
80-95
9.1
8.2
0.39
5
28
29
37
47.4
28.8


Profile Described By: Natalie Baxter and Grant Boyle, 9th October 2000.
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