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Soil Characterisation Site data sheet

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EL144 Soil Characterisation Site data sheet DEWNR Soil and Land Program

LOAM OVER RED CLAY ON ROCK (Calderwood soil)

General Description: Loam over a well structured red clay, occasionally calcareous with depth, grading to fine grained weathering basement rock.

Landform: Undulating to rolling low hills.

Substrate: Amphibolites of the Hutchison Group.

Vegetation: Eucalyptus cladocalyx woodland.

Type Site: Site No.: EL144 50,000 mapsheet: 6029-2 (Koppio)

Hundred: Koppio Easting: 584050

Section: 113 Northing: 6195950

Sampling date: 1982 Annual rainfall: 480 mm average Lower slope in a landscape of rolling low hills, 10% slope.

Soil Description:

Depth (cm) Description

0-10 Dark reddish brown loam with granular structure and 10-25% amphibolite fragments (10-50 mm).

Clear to:

10-40 Dark red medium clay with blocky structure and 2-10% amphibolite fragments (10-50 mm).

Gradual to:

40-80 Dark red medium clay with blocky structure in pockets within plates and lamellae of hard weathering amphibolite.

Classification: Haplic, Eutrophic, Red Chromosol; medium, gravelly, loamy / clayey, moderate

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EL144 Soil Characterisation Site data sheet DEWNR Soil and Land Program

Summary of Properties

Drainage: Moderately well drained. Water perches on the clayey subsoil for a week or so following heavy or prolonged rainfall.

Fertility: Inherent fertility is high, as indicated by the exchangeable cation data. Nutrient retention capacity is favoured by the relatively high clay content to the surface, and the absence of paler coloured sub surface layers indicates that leaching is not a significant factor. Phosphorus levels are low, as are zinc levels in the clayey subsoil.

Organic carbon levels are satisfactory.

pH: Slightly acid at the surface, neutral with depth.

Rooting depth: Not recorded. Estimate 40 cm in pit.

Barriers to root growth:

Physical: The clayey subsoil from 10 cm restricts root growth to some extent, but effects are likely to be minimal. Basement rock at shallower depths than at the sampling site is a more significant determinant of the rootzone.

Chemical: There are no apparent chemical barriers apart from low zinc availability in the subsoil.

Waterholding capacity: Approximately 75 mm in the rootzone.

Seedling emergence: Satisfactory, although hard setting in some soils affects establishment.

Workability: Satisfactory, although some surfaces may set hard, limiting cultivation effectiveness.

Erosion Potential:

Water: Moderately high.

Wind: Low.

Laboratory Data

Trace Elements mg/kg (DTPA)

Exchangeable Cations cmol(+)/kg Depth

cm Sand

% Silt

% Clay

% pH H2O

pH CaC12

CO3

% EC1:5

dS/m ECe dS/m

Org.C

% Avail.

P mg/kg

Cu Fe Mn Zn CEC cmol (+)/kg

Ca Mg Na K ESP

0-10 68 18 14 6.4 - 1.0 0.09 1.28 1.48 9 7.84 33 >50 0.90 15 5.1 1.4 0.16 0.85 1.1 10-40 28 5 67 7.0 - 2.0 0.03 0.14 0.72 3 8.48 15 33 0.16 29 11.0 8.2 0.45 1.10 1.6

40-80 - - - - - - - -

Note: CEC (cation exchange capacity) is a measure of the soil's capacity to store and release major nutrient elements.

ESP (exchangeable sodium percentage) is derived by dividing the exchangeable sodium value by the CEC.

Further information: DEWNR Soil and Land Program

Referensi

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