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Ambyne (Symbol: Ae)

EG224 | EG242 | EG246

Geology
Granite.

Landform
The Ambyne map unit encompasses rolling hills at an elevation range of about 200 to 800 m and a relief range of up to 300 m.

The granitic hills between Suggan Buggan and Cabanandra have been subdivided into the Ambyne map unit, which has slopes generally less than 32% and the Tubbut map unit, with slopes generally greater than 32%.

The Ambyne map unit may be subdivided into three components: gentle to moderate slopes, crests and concave open depressions.

Soils and landforms of Far East Gippsland - Ambyne - landform
Cleared lower slopes near the Snowy River crossing near Suggan Buggan


Native vegetation
In the western part of the area, the native vegetation was mostly grassy dry forest, tending to grassy woodland west of Ambyne Crossing.

Land use
Mostly native vegetation, some land has been cleared for grazing.

Soils
Component 1: Soils on gentle to moderate slopes
The three soil profiles (EG224, EG242 and EG246) examined all had a high coarse sand component being described as coarse sandy loams to coarse sandy clay loam. Where the decomposing granite occurs at a shallow depth, the soils appear to be less acid with surface pH’s around 7.0. Where the depth to decomposing granite is deeper, the soils tend to be strongly to moderately acidic. This is probably because they are more deeply weathered.

Components 2 and 3: crests and concave open depressions.
No soil profiles were examined, but it is likely that those on the crests will be shallower and have occurrences of exposed rock.

Site EG224

Location: Ambyne Geo. Ref. 0636700E 5900700N
Australian Soil Classification: Haplic, Eutrophic, Red CHROMOSOLRed coarse sandy gradational soil
General landscape description: Rolling hills
Geology: Granite
Site description: Simple upper slope 15% south east
Land use: Grazing
Native vegetation: Grassy woodland
Mapping unit: Ambyne (Component 1)

Soils and landforms of Far East Gippsland - Ambyne - EG224 landscape

Photo taken about 1.5km north-west of Ambyne Crossing looking south-east along the Deddick River valley

Soil profile morphology

Surface soilSoils and landforms of Far East Gippsland - Ambyne - EG224 profile

A11

0 – 18 cm

Dark reddish brown (5YR3/3); coarse sandy loam; weak fine (2 – 5 mm) granular structure; weak consistence dry; pH 7.2; clear change to:

A12

18 – 40 cm

Yellowish red (5YR4/6); coarse sandy loam; weak medium (10 – 20 mm) polyhedral structure; firm consistence dry; pH 7.3; abrupt change to:
Subsoil

B2

40 – 70 cm

Dark red (2.5YR3/6); coarse sandy clay loam; moderate coarse (20 – 50 mm) polyhedral structure; strong consistence dry; passing to very weak rock; pH 6.3; diffuse change to:

C

70+

Weak granitic rock becoming more frequent with depth.
Key profile features
  • Lack of strong texture contrast between the surface (A) and subsoil (B) horizon.
  • Shallow depth to decomposing granite.

Soil profile characteristics
pHSalinity ratingSodicityDispersionSlaking
Surface soil
(A1 horizon)
Slightly alkalineVery lowNon sodicNoneSlakes partially
Subsoil
(B1 horizon)
Slightly alkalineVery lowNon sodicNone1Slakes considerably
Deeper subsoil
(80-110 cm)
Slightly acidVery lowNon sodicNoneSlakes considerably
1 Slight after remoulding.

HorizonDepth

cm
Field texturepH
water
pH

CaCl2
EC

dS/m
Coarse sand
%
Fine sand
%
Silt

%
Clay

%
Field cap.
% w/w
Wilt. point
% w/w
PAW*
water

% w/w
A10-18CSL7.26.3<0.05502591418.34.913.4
A218-40CSL7.36.2<0.054726111516.64.612.0
B240-70CSCL6.35.0<0.054020142222.29.013.2
* PAW is plant available water. This is the difference between the soil water content at field capacity and wilting point.

DepthOrgC#Total NFree
Fe
2O3
Exch.
Al
Exchangeable cations
cmol(+)/kg
Ca:MgESP
cm%%% w/wppmCaMgKNaTotalHCEC
0-181.1<0.05<104.61.30.37<0.056.36.33.6
18-400.37<0.05<10220.360.0644.44.411
40-700.35<0.05204.24.70.370.119.45.414.80.91
# Organic carbon

Management considerations

Whole profile
  • Plant available water capacity is considered to be low (estimated at 62 mm) for the top 65 cm of the soil profile.
  • The low wilting points of each horizon to this depth (4.9, 4.6 and 9.0) indicates plants are able to use light rains when the soil is dry. Due to the low water storage capacity, plants will suffer moisture stress unless further rains occur.
Surface (A) horizons
  • As mentioned above, the soils surface soils can hold little water, but plants can use light rains following a dry spell.
  • The surface soil is slightly alkaline. Here the pH has no adverse implications for plant growth.
  • The nutrient holding capacity of the surface horizons is low (based on the sum of the calcium, magnesium, potassium and sodium cations).
  • The organic matter content of the surface soil is low. Increasing organic matter will help maintain soil fertility and water holding capacity.
  • The potassium is at a moderate level for pastures and no response to added potassium would be expected.
Subsoil (B) horizon
  • The slight increase in clay content is unlikely to restrict root penetration of deep rooted species until the decomposing granite is reached at about 70 cm.
Site EG242

Location: TubbutGeo. Ref. 0638200E 5896400N
Australian Soil Classification: Eutrophic, Red CHROMOSOLRed texture contrast soil
General landscape description: Rolling hills
Geology: Granite
Site description: Mid slope, south-east aspect, 10% slope
Land use: Grazing
Native vegetation: Grassy dry forest
Mapping unit: Ambyne (Component 1)

Soils and landforms of Far East Gippsland - Ambyne - EG242 landscape


Soil profile morphology

Surface soil
    Soils and landforms of Far East Gippsland - Ambyne - EG242 profile
    Road exposure down-slope from sampled site

A1


Subsoil

B2


0 – 20/35 cm




20/35 - 80+ cm

Brown (7.5YR4/4);
coarse sandy loam, weak fine granular structure; firm consistence dry; pH 5.5; abrupt and wavy change:



Reddish brown (2.5YR4/4); medium clay; moderate coarse polyhedral structure; very firm consistence dry; pH 6.0.
HorizonDepthEC
dS/m
pH
water
pH
CaCl2
Exchangeable cations
cmol(+)/kg
Ca:MgESP
cmCaMgKNaTotalHCEC
A10-20<0.055.54.62.41.50.370.074.36.210.51.6
B240-60<0.056.05.16.88.40.410.29167.423.40.81
Sampled by auger

Site EG246


Location: Chandlers Creek Geo. Ref. 0694600E 5865700N
Australian Soil Classification: Bleached-Mottled, Eutrophic, Red KANDOSOLRed coarse sandy gradational soil
General landscape description: Rolling to steep hills
Geology: Granite
Site description: Upper slope, 8% slope to north
Land use: Native forest
Native vegetation: Grassy dry forest
Mapping unit: Ambyne (Component 1)

Soil profile morphology

Surface soil
    Soils and landforms of Far East Gippsland - Ambyne - EG246 profile

A11


A2


Subsoil

B2


0 – 30 cm


30 – 60 cm




60 – 1.0+m


Pinkish grey (7.5YR6/2);
coarse sandy clay loam; weak coarse granular structure; weak consistence moist; pH 5.2; gradual change to:

Pinkish grey (7.5YR7/2); conspicuously bleached, coarse sandy loam; massive; weak consistence moist; gradual change to:


Mottled pinkish grey, yellowish red (5YR4/6) and strong brown (7.5YR4/6); coarse sandy light clay; weak coarse polyhedral structure; firm consistence moist; pH 5.9.

HorizonDepthEC
dS/m
pH
water
pH
CaCl2
Exchangeable cations
cmol(+)/kg
Ca:MgESP
cmCaMgKNaTotalHCEC
A10-20<0.055.24.41.51.10.20.122.90.93.51.43
B160-80<0.055.94.65.73.70.250.3410.01.211.01.53
Sampled from road exposure
Analysed by Industry and Investment NSW (2010)
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