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GHF07b

Location: Mumbannar

Australian Soil Classification: Melacic-Basic, Arenic, Bleached-Orthic TENOSOL (very thick sandy surface horizons / overlying clay)
General Landscape Description: Dune field
Site Description: Gently undulating plain
Land Unit: Follett Dunes and Plains
Geology: Quaternary aeolian

General Land Unit Description: The majority of this land unit falls south of the Kanawinka fault. This land unit comprises areas with deep sand deposits. The residual landscape is thought to be influenced by the retreat of the Murray Sea which left stranded beach ridges oriented south west–north east. These were subsequently covered by superficial sand sheets in later depositional phases, which formed the landscape seen today.

The major landforms in this land unit are dunes and swales. Podosols and Kurosols or Chromosols are the major soil types found on the dunes and rises. Podosols are soils with a ‘coffee rock’ layer. The Kurosols or Chromosols tend to have a deep sandy topsoil over the clay. The common soil types on the swales are black cracking clay (Vertosols) or Grey Sodosols. Some Ferric Kurosols or Chromosols can also occur on the swales or lower slopes of the dunes.

1.5 year old Eucalyptus globulus plantation on ex-agricultural land.


Soil pit Hun99 1-5 landscape

Soil Profile Morphology

A10-20 cmVery dark grey (10YR3/1); loamy fine sand; single grain structure; loose consistence, moderately moist; many medium roots present ; pH 5.3; clear and smooth change to:Soil pit Hun99 2 profile
A2120-40 cmLight yellowish brown (10YR6/4), with many coarse faint very pale brown(10YR8/3) mottles; fine sand; single grain structure; loose consistence, moist; few fine roots present; pH 5.7; gradual and smooth change to:
A2240-90 cmWhite (10YR8/2), conspicuously bleached; fine sand; single grain structure; loose consistence, moist; pH 6.1; diffuse and smooth transition to:
A2390-160 cmLight grey (10YR7/2), conspicuously bleached; fine sand; single grain structure; loose consistence, wet; pH 6.0; changes to:
Subsoil
B21160-190 cmLight grey; sandy clay; changes to:
190-210 cmGrey; clayey sand; changes to:
210-320 cmSand ; contains soft limestone (CaCO3) fragments, that become more concretionary (harder, denser) with increasing depth.

Soil Profile Characteristics:
-

pH
Salinity
Surface Soil
(A1 horizon)
Strongly Acid
Very Low
Subsurface
(90-160 cm)
Moderately Acid
Very Low




Chemical and Physical Analysis:
Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl
2)
EC
dS/m
Organic Carbon
%
Total
Nitrogen
%
A1
0-20
5.3
4.5
<0.05
1.6
0.14
A21
20-40
5.7
5.0
<0.05
A22
40-90
6.1
5.4
<0.05
A23
90-150
6.0
5.2
<0.05

Management Considerations: Free water entering pit at 90 cm, and also at 300 cm. The density of limestone at 320 cm suggests that there may be an impeding layer to root growth at this depth, but some data from Forestry SA indicates that the presence of shallow limestone may not necessarily restrict root development.

Profile Described By: Ian Sargeant, Paul Feikema, Martin Clark and Kiet Quach, 5th November 2000.
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