Your gateway to a wide range of natural resources information and associated maps

Victorian Resources Online

SFS5b

Location: Brewster, Trawalla East Road (West of Ballarat)
Aust. Soil Class.:Vertic (& Sodic), Eutrophic, Brown CHROMOSOL

Site Description: Level plain with gilgai microrelief (this soil represents the puff component)
Landform: Undulating plain
Element: Simple slope
Slope: 2-5%
Geology: Quaternary - Newer Volcanics

Image:  SFS 5a & 5b landscape
SFS 5b

Soil Profile Morphology:

Surface Soil
Image:  SFS 5b profile
SFS 5b
Ap0 - 20 cmBrown (10YR4/3 moist) to pale brown (10YR6/3 dry), fine sandy loam to loam, weak to very firm consistence (depending on colour – lighter = stronger); highly variable and mixed material; Ap originally likely to be less than 10 cm and is now dominated by apedal, A2 material. pH 5.5; clear boundary to:
Subsoil
B21tg20 – 70 cmMottled light olive brown (2.5Y5/4) and olive yellow (2.5Y6/6); medium clay; irregular medium to coarse (40–80 mm) prismatic parting to medium to coarse (15–40 mm) angular blocky or polyhedral structure; roots between peds contrasts with lack of roots at this depth in the ‘hollow’ component of the gilgai; clear boundary to:
B22gss70 + cmOlive brown (2.5Y4/4 moist) with many (20-50%) light olive brown (10YR5/6) mottles; medium heavy clay; frequent small slickensides; less well developed structure than B21.

Key Profile Features:
  • Strong texture contrast between surface (A1) horizon and subsoils (B21) horizon.

Soil Profile Characteristics:


pH
Salinity Rating
Surface
(A1 horizon)
Strongly Acid
Low
Non-Sodic
None
Subsoil
(B21 horizon)
Slightly Acid
Low
Non-Sodic
None1
Deeper subsoil
(at 1 m)
Slightly Alkaline
Low
Sodic
None1
1 Moderate dispersion after remoulding

Image:  SFS 5b graphs

Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl2)
EC
dS/m
NaCl
Exchangeable Cations
Ca
Mg
K
Na
meq/100g
Ap
0-20
5.5
5.1
0.31
0.02
4.1
0.8
0.6
<0.1
B21tg
20-70
6.5
5.7
0.21
6.7
12
1.5
1.6
B21gss
70+
7.5
6.6
0.3
0.03
5.1
9.7
0.7
2.4

Horizon
Horizon Depth
(cm)
Exchangeable Aluminium
mg/kg
Exchangeable Acidity
meq/100g
Field
Capacity
pF2.5
Wilting Point
pF4.2
Coarse Sand
(0.2-2.0 mm)
Fine Sand
(0.02-0.2 mm)
Silt
(0.002-0.02 mm)
Clay
(<0.002 mm)
Ap
0-20
<10
1
33
9.1
4.1
37.7
27.5
20
B21tg
20-70
11
51.2
28.7
0.8
10.1
7.5
78
B21gss
70+
55.3
31.1
1.1
6.2
4.5
80

Image:  SFS 5a soil
Soil pit at SFS5 showing extremely variable horizon thickness associated with gilgai


Management Considerations:

Whole Profile
  • Described by the owner as ‘crabhole country’, this slightly elevated, gently sloping land has well developed ‘gilgai’ features in the subsoil. The very variable nature of this soil is evident in material in the beds which have white A2 horizon material, buckshot, pisolitic cemented buckshot and subsoil clay all present at the ground surface. ‘Spew’ or ‘hollow units’ are elongated downslope (~10 m). ‘Puffs’ are of smaller lateral dimensions than the ‘hollows’ being 1–3 metres across. In the excavated pit, two faces were picked back. SFS5a to show deep A2 with buckshot and SFS5b to show puff unit (shallow depth to clay).
  • This soil presents real problems to the agriculturalist. Water holding properties are extremely different in the ‘puff’ compared with the hollow and this is often evident in the crop. The topsoil is not well structured, disintegrates to a ‘flour’ when dry-tilled, is weak and ‘spewy’ when wet and hard set when dry. Protection of the surface with ground cover is essential to reduce the slaking and sealing effects of rain. Under high rainfall / runoff conditions this soil is potentially highly erodible. The subsoil is sodic and has a high clay content so this soil is also prone to severe waterlogging. The slope of the land and the forming of beds should alleviate this in the surface horizons but erosion is a potential hazard should the furrows carry excessive runoff.
Notes
  • Second pit opened at crest of hill. Abrupt and steeply inclined boundary between puff and hollow, photographed. Very cemented pisolitic ironstone at base of hollow, >30 cm thickness.
  • Soil profile described by Richard MacEwan, May 1999.


Page top