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CTW Caltowie Land System

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CTW Caltowie Land System Report DEWNR Soil and Land Program

CTW Caltowie Land System

Flats, gentle slopes and undulating rises in the upper catchment of Yackamoorundie Creek, north and south of Caltowie.

Area: 134.0 km2

Annual rainfall 425 – 490 mm average

Geology: Fine to medium grained valley floor sediments capped by a veneer of wind deposited calcareous materials which are usually finely divided (silt and clay sized particles), but may be partially indurated into rubbly nodules or semi-hard massive sheets. Below the sediments and outcropping through them on the margins of the valley are siltstones of the Saddleworth Formation. These rocks are also capped by carbonates, but a greater proportion is in rubbly or sheet form.

Topography: The Land System comprises flat to gently inclined outwash fans of the upper Yackamoorundie Creek valley, although there is a small area in the north which drains into Appila Creek. The valley is bounded on the west by the Mt. Mary - Caltowie Hill Range and on the east by the Mt. Lock Range. The gentle slopes

abutting these ranges grade toward the creek flat running in a north - south direction down the centre of the valley. In the south west, where there is no well defined

flanking range, the Land System includes some gently undulating basement rock rises.

Elevation: The highest elevation is 530 m in the north east grading to 330 m where Yackamoorundie Creek flows into the Georgetown Land System.

Relief: Most of the Land System has even slopes with little relief. Rises formed on basement rock have up to 30 m of relief.

Soils: Most soils are deep overlying alluvium. Texture contrast and gradational forms are most common. Both have loamy surfaces and well structured red clayey subsoils.

Some are calcareous throughout. Shallower calcareous loams and loam over clay on bedrock occur on rises.

Main soils

Soils formed on lower slopes and flats on alluvium D2 Hard loam over red clay

A3 Calcareous loam Minor soils

Soils formed on lower slopes and flats on alluvium C3a Gradational loam

A4 Rubbly calcareous loam C3b Gradational loam over rubble Soils formed on basement rock on rises A2 Shallow calcareous loam C2/D1 Shallow loam over red clay

Main features: The Caltowie Land System is flat to gently sloping land characterized by deep loamy soils. These are inherently productive. Limitations are due to poor surface structure in texture contrast soils (with adverse effects on water infiltration, workability,

emergence and root growth), high subsoil alkalinity in calcareous soils, and saline seepage in the area east of Caltowie. Limited rising ground on basement rock has mainly shallow calcareous soils, productivity on which is mainly limited by lack of moisture holding capacity and sub optimal fertility.

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CTW Caltowie Land System Report DEWNR Soil and Land Program Soil Landscape Unit summary: 12 Soil Landscape Units (SLUs) mapped in the Caltowie Land System:

SLU area % of Main features # EGB

EGC

10.2

1.6 Rises formed on fine grained rock.

EGB Rises with slopes of 1-4%.

EGC Rises with slopes of 4-10%.

Main soils: shallow calcareous loam - A2 (V), with shallow loam over red clay - C2/D1 (E).

The rises are fully arable, although moisture shortages limit crops in dry finishes.

Improvement of hard setting surface soils to reduce water loss and erosion through runoff is the main management issue.

JDA JDB JDC JDE

20.2 34.9 2.4 0.2

Flats, outwash fans and drainage depressions formed on fine grained alluvium.

JDA Flats with slopes of less than 2%.

JDB Fans with slopes of 2-4%.

JDC Fans with slopes of 4-8%.

JDE Drainage depressions.

Main soils: hard loam over red clay - D2 (E), with calcareous loam - A3 (C), rubbly calcareous loam - A4 (L), and gradational loam - C3a/C3b (L). The entire unit is arable.

Hard setting surface soils are the main management problem, because of their adverse effects on runoff / erosion, workability, seedling emergence, and moisture retention. Most soils are reasonably fertile, deep and well drained.

JEA JEB JEE JEO JEP JEQ

3.6 14.3 4.4 1.3 5.3 1.6

Broad flats, outwash fans and creek flats formed on fine grained alluvium.

JEA Flats with slopes of less than 1%.

JEB Fans with slopes of 2-5%.

JEE Creek terraces.

JEO Creek terraces with sporadic saline seepage.

JEP Marginally saline flats.

JEQ Marginally saline fans.

Main soils: hard loam over red clay - D2 (V), with gradational loam - C3a (C). Most of this land has deep well drained fertile soils with only slight limitations to agriculture. Hard setting surface soils are the main limitation, causing reduced water infiltration, restricted opportunities for working and patchy emergence. They add to the erosion potential on sloping land. Salinity is a problem east of Caltowie.

# PROPORTION codes assigned to soils within Soil Landscape Units (SLU):

(D) Dominant in extent (>90% of SLU) (V) Very extensive in extent (60–90% of SLU) (E) Extensive in extent (30–60% of SLU) (C) Common in extent (20–30% of SLU) (L) Limited in extent (10–20% of SLU) (M) Minor in extent (<10% of SLU)

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CTW Caltowie Land System Report DEWNR Soil and Land Program

Detailed soil profile descriptions:

A2 Shallow calcareous loam (Paralithic Calcic / Supracalcic Calcarosol)

Calcareous loam grading to soft or rubbly carbonate over weathering rock within 50 cm.

A3 Calcareous loam (Regolithic, Calcic Calcarosol)

Calcareous loam grading to highly calcareous clay loam over alluvium.

A4 Rubbly calcareous loam (Regolithic, Supracalcic / Lithocalcic Calcarosol)

Calcareous loam becoming more clayey with depth over rubbly Class III B/C carbonate grading to alluvium below 100 cm.

C2/D1 Shallow loam over red clay (Supracalcic / Hypercalcic, Red Dermosol / Chromosol)

Hard loam over a well structured red clay with soft or rubbly carbonate at shallow depth grading to weathering rock within 100 cm.

C3a Gradational loam (Hypercalcic, Red Dermosol)

Friable clay loam grading to a well structured red clay with soft Class I carbonate from about 60 cm, over alluvium deeper than 100 cm.

C3b Gradational loam over rubble (Supracalcic / Lithocalcic, Red Dermosol)

Friable clay loam grading to a well structured red clay with rubbly Class III B or III C carbonate from about 60 cm, over alluvium deeper than 100 cm.

D2 Hard loam over red clay (Calcic / Hypercalcic, Red Chromosol)

Hard setting sandy loam to clay loam overlying a strongly structured red clay with soft Class I carbonate at about 65 cm grading to alluvium below 100 cm.

Further information: DEWNR Soil and Land Program

Referensi

Dokumen terkait

Main soils L1a Shallow stony loam A2 Shallow calcareous loam to clay loam RR Rock outcrop Minor soils On rock C2 Gradational loam to clay loam on rock D1 Loam to clay loam over

Main soils: L1 39% Shallow soil on rock Rocky Rudosol-Tenosol A2 29% Calcareous loam on rock Paralithic Calcarosol A3 11% Deep moderately calcareous loam Calcic Calcarosol Minor

Main soils: L1 23% Shallow soil on rock Rocky Rudosol-Tenosol A3 14% Deep moderately calcareous loam Calcic Calcarosol A2 12% Calcareous loam on rock Paralithic Calcarosol C3 11%

Main soils L1a Shallow stony loam L1b Shallow stony sandy loam K4 Sandy loam over brown sandy clay K2b Loam over red clay Minor soils C2 Shallow gradational red loam on calcareous

Annual rainfall: 365 – 425 mm average Main soils: A6 gradational calcareous clay loam A5-A4 calcareous loam C4-D3 clay loam to loam over red clay Minor soils: B2 shallow calcareous

Main soils Soils formed on basement rocks on slopes D7a Sandy loam over dispersive red clay - Extensive on slopes in the eastern areas D1a Loam over red friable clay - Extensive on

Main soils: A7 22% Calcareous clay loam on marl Marly Calcarosol B5 18% Shallow dark clay loam on limestone Petrocalcic Black-Grey Dermosol N1 12% Peaty soil Organosol N3 11% Wet

K2 Acidic loam over red to brown clay K3b Acidic sandy loam over sodic red clay on non calcareous rock K4 Acidic sandy loam over brown clay Soils formed on lateritic residuals J2