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HOR2

    Site Code
HOR2

    Location

Lower Norton, western Victoria

    Landform

Gently Undulating Plain

    Geology

Pliocene Parilla Sand:
marine sand and silt

    Element

Summit surface

    Aspect
3 %

Horizon
Depth (cm)
Description

A1

0–10

Dark brown (10YR3/3);
loamy sand; weak platy to single grain (structureless); weak consistence; abundant ferruginous concretions and sandstone; pH 5.9; sharp boundary to:

A2

10–15

Brownish yellow (10YR6/6); bleached white (10YR8/1 dry);
loamy sand; single grain (structureless); very weak dry consistence; abundant ferruginous concretions and sandstone; pH 8.2; sharp boundary to:

B21

15–75+

Red (2.5YR5/6) with many coarse distinct (7.5YR5/6) mottles;
medium clay; very strong consistence, slightly moist; pH 8.0.

B23k

100–120

Light yellowish brown (2.5Y6/4) with many distinct fine (5YR4/6) mottles;
medium clay; weak to moderate medium polyhedral structure; smooth ped-fabric; strong consistence, moderately moist; few fine to medium ferro-manganiferous concretions with common extremely coarse calcareous soft segregations; common distinct slickensides and clay skins; pH 9.2; clear and wavy boundary to:

B3k

120–145+

Light yellowish brown (2.5Y6/3) with few distinct fine (5YR4/4) mottles;
medium heavy clay; weak medium polyhedral structure; smooth ped-fabric; firm moist consistence; many fine manganiferous and coarse ferro-manganiferous concretions/nodules with few corse calcareous soft segregations; few distinct slickensides and clay skins; very strongly cemented broken nodular ferricrete pan; pH 9.2.
Chemical and Physical Analysis:

Horizon
Depth (cm)
pH (water)
pH (CaCl2)
EC
dS/m
NaCl
%
Exchangeable Cations
cmol-/kg
Field Capacity
(pF2.5)
Wilting Point
(pF4.2)
Ca
Mg
K
Na
A1
0–10
5.9
4.7
0.01
1.0
0.3
0.1
0.0
5.6
3.2
A2
10–15
8.2
7.5
0.10
0.02
1.3
1.2
0.1
0.7
7.8
2.3
B21
15–75+
8.0
7.1
0.25
0.00
2.9
7.2
0.4
2.8
22.3
15.3

Management Considerations:
  • Texture contrast soil, sodic and at depth.
  • Leached sub surface horizon.
  • Alkaline subsoil with coarse structure, roots confined to coarse structure.
  • Many ferruginous nodules/sandstone in deep subsoil.
  • Imperfect to slow subsoil drainage; clayey, coarse structure, highly dispersive, may be vertic at depth.
  • Moderate to high susceptibility to soil structure decline.
  • Moderate to high susceptibility to soil compaction, subsurface and upper subsoil.
  • Landscape position, long lower slope.
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