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Lindenow (Symbol: Li)

EG209 | Profile No. 24 | Profile No. 25

Geology
Recent alluvium.

Landform
Level plain with slopes generally less than 1% with a relief <9m. Alluvial plains, comprising flood plains, and stream channels.

An interactive visualisation of the landscape in the Lindenow mapping unit is provided here. Zooming and panning functionality is provided as well as the ability to click on icons to provide further information about the landscape (e.g. soils, geology).

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Photo

Panoroma

Information

Soil pit

Video

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This map unit is confined to the valleys of Mitchell River near Bairnsdale and the Tambo River south of Bruthen.

Soils and lanforms of the Bairnsdale Dargo region - a guide to the major agricultural soils of East Gippsland 2011 - Lindenow landform
Mitchell River flats looking south towards Lindenow


Original vegetation
Dry valley forest, minor areas of floodplain reed-bed.

Soils
Component 1: Soils on flood plains
Most of the soils of this map unit occur on the flood plains. Generally they are moderately to slightly acidic dark greyish brown deep fine sandy to silty loams and silty clay loams, but layers of coarser material such and stones and gravel may occur deeper in the subsoil. Three soil profiles are described: Mitchell River flats, Tambo River flats south of Bruthen and near the Tambo River mouth.

Component 2: The stream channel
This is a very minor component of the map unit. Bed and bank erosion is common along the stream channels.

Land use
Mitchell River flats are used extensively for vegetable production with some grazing and the Tambo River flats for grazing.

Site EG209

Location: LindenowGeo. Ref.: 545620E 5815860N
Australian Soil Classification: Melanic, Eutrophic, Brown KANDOSOLDark brown uniform textured soil
General landscape description: Level plain
Geology: Recent alluvium
Site description: <1% slope
Land use: Vegetable production
Native Vegetation: Dry valley forest, minor areas of floodplain reed-bed
Map unit: Lindenow (Component 1)


Soils and lanforms of the Bairnsdale Dargo region - a guide to the major agricultural soils of East Gippsland 2011 - Lindenow - EG209 landscape

Soil profile morphology

Surface soil
A11 0 – 15 cmDark brown (7.5YR3/2); silty loam; moderate fine granular structure; weak consistence dry; clear change to:
Soils and lanforms of the Bairnsdale Dargo region - a guide to the major agricultural soils of East Gippsland 2011 - Lindenow - EG209 profile
Subsurface soil
A1215 – 40 cmDark brown (7.5YR3/2); silty loam; weak coarse polyhedral structure; firm consistence dry; gradual change to:
A1340 – 70 cmBrown (7.5YR4/2); silty loam; apedal; firm consistence dry; gradual change to:
A1470 – 110 cmBrown (7.5YR4/2); silty loam; apedal; weak consistence dry; gradual change to:
A15110 – 140 cmBrown (7.5YR4/2); silty loam.
Key profile features
  • Uniform textures throughout.
Soil profile characteristics

pHSodicitySlakingDispersion
Dry
Dispersion
Remoulded
Surface soilSlightly acidNon-sodicNilNil (2 hours),
Nil (20 hours)
Nil (2 hours),
Moderate (20 hours)
Subsurface
(A12 horizon)
Moderately acidicNon-sodicConsiderableNil (2 hours),
Nil (20 hours)
Moderate (2 hours),
Moderate (20 hours)
Deeper subsoil
(70-110 cm)
Slightly acidNon-sodicConsiderableNil (2 hours),
Nil (20 hours)
Slight(2 hours),
Slight (20 hours)

HorizonDepth

cm
Field
texture
pH
water
pH
CaCl2
EC

dS/m
Coarse
sand
%
Fine
sand
%
Silt

%
Clay

%
Field
cap.
% w/w
Wilt.
point
% w/w
PAW*
water
% w/w
A110-15ZL5.95.10.06244192628.99.619.3
A1215-40ZL5.64.70.05046311628.28.220.0
A1340-70ZL6.45.40.05048301520.17.113.0
A1470-110ZL6.55.50.05046281926.35.720.6
* PAW refers to plant available water. This is the difference between the soil’s water content at field capacity and wilting point.

DepthOrgC#Total NFree
Fe2O3
Exch.
Al
Exchangeable cations
cmol(+)/kg
Ca:MgESP
cm%%% w/wppmCaMgKNaTotalHCEC
0-153.10.17<108.22.30.140.23118.519.53.51
15-402.20.10<1072.30.0950.159.58.918.731
40-701.8<0.05<106.54.20.0830.23115.716.71.61
70-1101.60.05N/A5.850.0910.32114.415.41.22
# Organic carbon

Management considerations

Whole profile
  • The brown colours throughout and lack of texture contrast indicate the profile is well drained internally.
  • Plant available water content capacity is considered to be low to moderate, (estimated at 62 mm) based on the laboratory data and an effective rooting depth of 70 cm.
Surface (A11) horizon
  • The soil has a normal organic matter content conferring average structural stability,
  • The nutrient holding capacity of the soil is moderate (based on the sum of exchangeable cations),
  • The potassium levels are low and the soil is expected to show a strong response to potassium fertilisers.
Subsurface soils
  • The soil has no impeding layers to restrict root development.

Profile No. 24 (Aldrick et al, 1992)

Location: BruthenGeo. Ref.: 0572400E 5824200N
Australian Soil Classification: Melanic, Eutrophic, Brown DERMOSOLDark brown uniform textured soil
General landscape description: Flood plain (hummocky)
Geology: Recent alluvium
Site description: 1% slope
Land use: Grazing on annual pasture
Native Vegetation: Dry valley forest, minor areas of floodplain reed-bed
Map unit: Lindenow (Component 1)

No photo available


Soil profile morphology

Surface soil
A110 – 7 cmVery dark greyish brown (10YR3/2); silty loam; moderate crumb structure; friable consistence moist; clear wavy change to:

A12

7 – 17 cm

Very dark greyish brown (10YR3/2) abundant distinct brown
mottles; silty loam; moderate fine (<5 mm) subangular blocky structure; friable consistence moist; diffuse wavy change to:

AC

17 – 27 cm

Very dark greyish brown (10YR3/2), abundant distinct brown (<5 mm) mottles; silty loam (
with thin fine sand lenses); moderate fine (<5 mm) subangular blocky structure; friable consistence moist; abrupt smooth change to:

11A1

27 – 52 cm

Very dark greyish brown (10YR3/2), abundant distinct brown (5 -15 mm) mottles;
silty clay loam (with thin fine sand lenses); moderate coarse angular blocky structure; firm consistence moist; abrupt change to:

11C

52 – 90+ cm

Yellowish brown (10YR5/6), abundant distinct grey (5 -15 mm) mottles;
silty loam; massive

Key profile features
  • Little change in clay content down the profile.
Soil profile characteristics

HorizonDepth

cm
Field
texture
pH
water
EC

dS/m
Gravel

%
Coarse
sand
%
Fine
sand
%
Silt

%
Clay

%
Field
cap.
% w/w
Wilt.
point
% w/w
PAW*
water
% w/w
A110-7ZL6.20.2102431817
A1210-17ZL6.30.1401541815
11A130-52ZCL6.10.310<1373419
11C52-60ZL6.30.230<1552615
* PAW refers to plant available water. This is the difference between the soil’s water content at field capacity and wilting point.

DepthOrgC#Total NExch.
Al
Exchangeable cations
cmol(+)/kg
Ca:MgESP
cm%%ppmCaMgKNaTotalHCEC
0-74.00.438.76.00.40.515.611.326.91.52
10-172.30.208.04.30.10.512.98.020.91.92
30-521.40.158.25.10.091.014.410.124.51.64
52-601.50.117.04.10.040.811.99.321.21.74
# Organic carbon

Profile No. 25 (Aldrick et al, 1992)

Location: Tambo MouthGeo. Ref.: 0570700E 5810300N
Australian Soil Classification: Melanic-Sodic, Eutrophic, Brown DERMOSOLDark brown uniform textured soil
General landscape description: Delta
Geology: Recent alluvium
Site description: 1% slope on river delta
Land use: Grazing on annual pasture
Native Vegetation: Dry valley forest, minor areas of floodplain reed-bed
Map unit: Lindenow (Component1)

No photo available


Soil profile morphology

Surface soil
A110 – 20 cmVery dark brown (10YR2/2); silty loam; moderate crumb structure; friable consistence when moist; gradual wavy change to:

A12

20 – 35cm

Black (10YR2/1);
silty clay loam; moderate crumb structure; friable consistence moist; clear smooth change to:

C1

35 – 46 cm

Dark brown (10YR4/3), abundant distinct grey (5-15 mm) mottles;
silty clay loam; massive; friable consistence moist; clear smooth change to:

C2

46 – 68 cm

Dark brown (10YR4/3), abundant distinct grey (5-15 mm) mottles) mottles;
loamy sand; massive, firm consistence moist; clear change to;

C3

68 – 90 cm

Dark yellowish brown (10YR4/6), abundant prominent grey (5 -15 mm) mottles;
silty clay loam; massive; very firm consistence moist
Note: Mica throughout the profile.

Key profile features
  • Apart from a sand layer at 46 to 68 cm, there was little change in clay content down the profile.
Soil profile characteristics

HorizonDepth

cm
Field texturepH
water
EC

dS/m
Gravel

%
Coarse sand
%
Fine sand
%
Silt

%
Clay

%
Field cap.
% w/w
Wilt. point
% w/w
PAW*
water
% w/w
A110-10ZL5.40.0602342219
A1110-20ZCL5.60.0202412419
A1230-35ZCL6.20.0202512316
C135-46ZCL6.50.0203542314
C368-90ZCL6.90.1202532018
* PAW refers to plant available water. This is the difference between the soil’s water content at field capacity and wilting point.

DepthOrgC#Total NExch.
Al
Exchangeable cations
cmol(+)/kg
Ca:MgESP
cm%%ppmCaMgKNaTotalHCEC
0-103.90.532.73.10.90.77.429.336.70.82
10-204.00.331.82.10.50.65.027.732.70.92
30-351.60.142.23.50.30.96.913.620.50.64
35-461.10.082.74.70.21.18.77.616.3067
68-902.45.40.53.611.94.116.00.422
# Organic carbon
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