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Site LP64

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Group: Lexton Landcare Group

Australian Soil Classification: Vertic, Mottled-Mesonatric, Grey SODOSOL; (very deep surface horizons)

General Landscape Description: Lower midslope position of a rolling low hill landscape unit. The geology is Devonian granite.

Photo: Soil Site LP64 Landscape
Soil Site LP64 Landscape


Soil Profile Morphology:

Surface Soil
Photo: Site LP64 Soil Profile
Site LP64 Soil Profile
A110-30 cmDark brown (7.5YR3/2); light sandy clay loam; moderate very fine granular structure, becoming weak medium blocky structure with depth; pH 5.7; clear change to:
A2130-50 cmBrown (10YR5/3); light very fine sandy loam; massive; firm consistence moist; pH 4.8; abrupt change to:
A2250-75 cmBrown (10YR5/3) with yellow brown (10YR5/8) mottles; conspicuously bleached; light sandy clay loam; firm consistence dry; contains very few (2%) ferro-manganiferous nodules (8 mm size) and few (3%) quartz fragments; pH 6.1; abrupt change to:
A2375-85 cmGreyish brown (10YR5/2); conspicuously bleached (10YR7/2d); light coarse sandy clay loam; very firm consistence dry; pH 6.6; sharp change to:
Subsoil
B2185-110 cmDark grey brown (10YR4/2) with red (2.5YR4/6) and yellow brown (10YR5/8) mottles; medium-heavy clay; very coarse prismatic structure; strong consistence moist; pH 6.9; gradual change to:
B22110 + cmGreyish brown (10YR5/2) with red (2.5YR4/6) and yellow brown (10YR5/8) mottles; medium-heavy clay; strong consistence moist; quartz and gravel present in patches; slickensides present; pH 6.9.

Key Profile Features:
  • Very thick subsurface (A2) horizons (to 85 cm depth).
  • Strong texture contrast between surface (A) horizons (<20% clay) and subsurface (B21) horizon (46% clay).
  • Conspicuously bleached subsurface (A2) horizons.
Soil Profile Characteristics:


pH
Salinity Rating
Surface
(A1 horizon)
moderately acid
very low
-
none
Subsoil
(B21 horizon)
slightly acid
very low
strongly sodic
complete
Deeper subsoil
(at 1 m)
slightly acid
low
strongly sodic
complete
Graph: Soil Site LP64 pH levels
Graph: Soil Site LP64 Salinity levels
Graph: Soil Site LP64 Sodicity levels
Graph: Soil Site LP64 Clay%

Horizon
Horizon Depth
pH
(water)
pH
CaCl2
EC
dS/m
NaCl
%
Exchangeable Cations
Ex Al
mg/kg
Ex Ac
meq/100g
Field
pF2.5
Wilting Point
pF4.2
Coarse Sand
(0.2-2.0mm)
Fine Sand
(0.02-0.2mm)
Silt
(0.002-0.02mm)
Clay
(<0.002mm)
Ca
Mg
K
Na
meq/100g
A1
0-30
5.7
4.7
0.09

2.9
1.9
0.2
0.1


23
10
34
29
19
15
A21
30-50
6
4.9
0.05

1.5
1.5
0.2
0.1


16.8
6.6
A22
50-75
6.1
5
0

1.4
1.6
0.1
0.1


18.7
8.9
28
36
18
18
A23
75-85
6.6
5.3
0

0.7
1.1
0.1
0.2


10.9
5.8




B21
85-110
6.9
5.8
0.16

2.9
11
0.3
3.2


39.8
26.6
13
16
20
46
B22
110+
6.9
5.9
0.22

2.7
11
0.3
3.7









Management Considerations:

Whole Profile
  • Plant available water capacity (PAWC) is estimated to be relatively low (estimated at 65 mm). This is based on available laboratory data and assumes an effective rooting depth of 100 cm. Effective rooting depth will be restricted by the strongly sodic and dispersive subsoil. The low PAWC will limit pasture growth into dry a spring and summer.
Surface (A) Horizons
  • The surface (A) horizons have a much higher level of coarse sand than for the other sites examined. This will contribute to increased infiltration of water and reduced plant available water holding capacity.
  • Organic carbon and total nitrogen levels are reasonable for the A1 horizons. Organic matter is important for maintaining surface soil aggregation. The relatively deep A1 horizon is important for plant growth as the deeper A2 horizons have a very low inherent fertility (based on the sum of the exchangeable cations).
Subsoil (B) Horizons
  • The dense and coarsely structured subsoil is strongly sodic and disperses completely (and has a low calcium:magnesium ratio of 0.3). This is likely to significantly restrict water and root movement through the subsoil. The conspicuously bleached A2 horizon above the sodic subsoil indicates that periodic waterlogging occurs. On sloping country there is likely to be significant lateral flow of water downslope, above the more impermeable clay subsoil.
Comments from Landholder:
  • Was native pasture until ripped up 12 years ago. Fescue, phalaris and cocksfoot now grown. (Cocksfoot performs better than phalaris).
  • More likely to get bogged here than on Site LP65.
Profile Described By: Mark Imhof, Paul Rampant, Karen de Plater (12/4/95).

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