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Talbotville (Symbol: Te)

Profile No. 11 (Aldrick et al, 1967)

Geology
Palaeozoic sediments, mudstones, siltstones, sandstones and shales, occasionally metamorphosed.

Landform
In the context of this report, the Talbotville map unit encompasses rolling to steep hills with an elevation range of about 350 to 1200 m. The slope gradients exceed 15% but are generally much steeper, commonly 40 – 70%. The relief ranges from 90 – 300 m.

Soils and landforms of the Omeo/Benambra and Tambo Valley region - soil-landform unit Talbotville landform
Talbotville map unit: Looking east from the Omeo Valley Road

Soils
Steep slopes, slow-weathering sedimentary rocks and rainfall inadequate enough to support vigorous and dense vegetation, give rise to active natural erosion and slow soil formation. Thus the soils tend to be shallow, stony, leached, acidic and weakly structured. Where areas have been denuded of vegetation, for example north of Smoking Hill where it was removed to support the mining industry, the soils are prone to severe sheet erosion. On the valley floors where eroded soil has accumulated, gully erosion can be quite severe.

Vegetation
Shrubby dry forest with montane dry woodland at higher altitudes.

Profile No. 11 (Aldrick, et al 1992)

Location: 17 km NW DargoGeo. Ref. 0511900E 5967236N
Australian soil classification: Acidic, Dystrophic,Brown KandosolShallow soil on fractured rock
General landscape description: Steep hills
Geology: Palaeozoic siltstones and shales
Site description: North aspect (28% slope)
Land use: Forest
Native vegetation: Shrubby dry forest
Mapping unit: Talbotville
    Soils and landforms of the Omeo/Benambra and Tambo Valley region - soil-landform unit Talbotville soils
    Severe gully erosion often occurs in the cleared valleys

Soil profile morphology

Surface soilSoils and landforms of the Omeo/Benambra and Tambo Valley region - soil-landform unit Talbotville Pro11 profile
Photo: Typical Talbotville soil profile: Cutting along Omeo-Benambra Road
A10 – 5 cmDark brown to brown (7.5YR4/4); gravelly clay loam; apedal; slightly hard dry; 30% small bedrock fragments up to 20 mm, clear boundary to:
Subsoil
B5 – 22 cmStrong brown (7.5YR5/6); gravelly clay loam; apedal; friable, moist; 30% small bedrock fragments up to 20 mm; fragments up to 80 cm common below 10 cm, change to:
R22+ cmBedrock
Key profile features
  • Shallow stony soil will only support shrubby vegetation

Soil profile characteristics
HorizonDepth

cm
Field texturepH
water
pH
CaCl
2
EC
dS/m
Coarse sand
%
Fine sand
%
Silt

%
Clay

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

% w/w
A10-5ZL4.8<0.0518183119
B5-10ZL5.0<0.0515233423
B10-20ZCL5.0<0.0513223528

DepthOrg C#Total NFree
Fe2O3
% w/w
Exch.
Al
Exchangeable cations
meq/100 g
Ca:MgNa
%
cm%%ppmCaMgKNaTotalHCEC
0-53.80.192.60.050.090.70.070.930.531.4<1
5-101.80.112.9<0.050.050.70.090.920.721.6<1
10-201.80.103.3<0.050.080.70.050.921.222.1<1
# Organic carbon

Management considerations

Whole profile
  • Plant available water will be low for pasture species where the roots are unable to find their way through cracks in the rock.
  • The shallow soils have extremely low nutrient and water holding capacity.
  • The surface soils are strongly acid. If pastures are to grow the soils need lime and heavy amounts of fertiliser. They are best left under native vegetation.
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