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Soil/Landform Unit - Tallageira swampy sand plains

Landform Unit Description

WLRA Landform Tallageira swamp sand plains
Eastern extent of an east-west sandy plain near Bringabert
      Area: 20 443 ha
      0.87% of CMA region

      This unit of low relative relief terrain consists of a major and minor occurrence north of Apsley on the South Australian border. This linear dunes subdivision (5.2.2) falls within the North West Dunefields and Plains siliceous dunefields. This dunefield and sand plain complex of Quaternary Lowan Sand (aeolian sediments) is a parallel feature of the Little Desert to the north. It is flanked to the north and south by plains as well as ridge topography. Dunefields and gently undulating plains are co-dominant. Soils are sandy (generally without a pan) within dunefields, and yellow grey sodic texture contrast soils (Sodosols) are found on the plains and local depressions. Sheet, wind and rill erosion are land degradation issues given the light sandy texture of the topsoils. Grazing (sheep, beef cattle) with occasional dryland cropping and nature conservation are major land uses. Remnant vegetation includes a number of communities found on damp sand or poorly drained soils. Plains Woodland, Damp Sands Herb-rich Woodland/Shallow Sands Woodland Mosaic, Damp Sands Herb-rich Woodland, Drainage-line Woodland, Plains Sedgy Woodland and Seasonally Inundated Shrubby Woodland occur here.
WLRA Landform Tallageira swamp sand plains

WLRA Landform Tallageira swamp sand plains
Sand component of swampy sand plain with remnant vegetation and improved pastures
WLRA Landform Tallageira swamp sand plains

WLRA Landform Tallageira swamp sand plains

WLRA Landform Tallageira swamp sand plains
Sheep grazing on a swampy sand plain

Component
1
2
Proportion of soil-landform unit
50%
50%
CLIMATE
Rainfall (mm)
Annual: 555
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
October–March
GEOLOGY
Age and lithology
Quaternary paludal silt and clay
Geomorphology
5.2.2 Linear dunes of the Siliceous North West Dunefields and Plains
LANDUSE
Uncleared areas: hardwood forestry for sawlogs, posts and poles; nature conservation
Cleared areas: sheep and beef cattle grazing; dryland cropping; nature conservation
TOPOGRAPHY
Landscape
Swampy sand plains
Elevation range (m)
97–158
Local relief (m)
2-3
Drainage pattern
Dendritic–deranged
Drainage density (km/km2)
0.2
Landform
Dunefields and plains
Landform element
Dunefield
Gentle undulating plain
Slope and range (%)
5 (1-10)
2 (1-5)
Slope shape
Straight
Convex
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (31.6%), Shallow Sands Woodland (13.9%), Shallow Sands Woodland/Plains Sedgy Woodland/Seasonally Inundated Shrubby Woodland/Damp Sands Herb-rich Woodland Mosaic (10.3%), Damp Sands Herb-rich Woodland (10.2%), Other (33.8%)
SOIL
Parent material

Aeolian sand

Marine sand and silt, paludal silt and clay
Description
(Corangamite Soil Group)
Sandy soils with and without pans (31)
Sodic yellow and grey texture contrast soils (32)
Soil type sites
LSWW8, LSWW7, WIA24, WIA31
Surface texture
Sand
Loamy sand
Permeability
High
Slow to moderate
Depth (m)
> 1.5
> 1.5
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Soils with low organic matter levels can be susceptible to wind and sheet erosion where exposed. Low inherent soil fertility.Susceptible to wind and sheet erosion where exposed. Low inherent fertility but well drained to pans or subsoil. Susceptible to compaction where hardsetting and poor drainage occurs.
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