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Soil/Landform Unit - West Wimmera swamp, lake and lunette complex

Landform Unit Description

WLRA Landform West Wimmera lake and lunette complex
String of lakes orientated north-south between former stranded beach ridges south of Wombelano
      Area: 12 889 ha
      0.55% of CMA region

      This unit of swamps and lunettes occurs south of the Little Desert and west of the Douglas Depression. As part of the North West Dunefields and Plains, these swamps and wetlands of Quaternary lacustrine and aeolian sediments occur between the NNW/SSE orientated ridges as gently undulating plains and depressions. Lakes and swamps, lunettes, backplains and low rises are all prominent land components. Drainage is very slow and is restricted to draining to the local depressions. Grey cracking clay soils (Vertosols) and sodic, yellow and grey texture contrast soils (Sodosols) occur in the drainage depressions with sodic red texture contrast soils (Sodosols) occurring on the low rises. Periodic to seasonal inundation and waterlogging are the main land issues of the flat terrain and in depressions. Land use is mixed between grazing (sheep and cattle), dryland cropping, water supply and recreation. Vegetation found includes communities such as Lignum Swampy Woodland, Shallow Sands Woodland, Plains Woodland, Freshwater Lake Mosaic, Dune Soak Woodland, Brackish Wetland, Lignum-Cane Grass Swamp and Red Gum Wetland.
WLRA Landform West Wimmera lake and lunette complex

WLRA Landform West Wimmera lake and lunette complex
Swamp located within east-west sand plains south of Goroke
WLRA Landform West Wimmera lake and lunette complex

WLRA Landform West Wimmera lake and lunette complex

WLRA Landform West Wimmera lake and lunette complex
Wetland bordering east-west sand plain

Component
1
2
3
4
Proportion of soil-landform unit
5%
10%
15%
70%
CLIMATE
Rainfall (mm)
Annual: 550
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
September–April
GEOLOGY
Age and lithology
Quaternary paludal silt & clay; Neogene marine sand & silt (Parilla Sand); Quaternary Aeolian dune sand (Lowan Sand)
Geomorphology
LANDUSE
Uncleared areas: Water supply; nature conservation
Cleared areas: Sheep and beef cattle grazing; dryland cropping; water supply
TOPOGRAPHY
Landscape
Swamp, lake and lunette complex
Elevation range (m)
94–184
Local relief (m)
5
Drainage pattern
Dendritic
Drainage density (km/km2)
1.6
Landform
Rises
Plains
Lakes, swamps and lunettes
Landform element
Low rises
Backplain
Lunette
Lake and swamp beds
Slope and range (%)
3 (1-8)
0 (0-1)
3 (1-10)
0 (0-1)
Slope shape
Convex
Linear
Convex
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (35.1%), Red Gum Wetland (12.7%), Shallow Sands Woodland (11.3%), Plains Savannah 5.8%), Other (28.8%)
SOIL
Parent material

Marine sand and silt

Paludal silt and clay

Aeolian sand, silt and clay

Paludal sailt and clay
Description
(Corangamite Soil Group)
Sodic red texture contrast soils (39)
Grey and brown cracking clay soils (37)
Sodic brown, yellow and grey texture contrast soils (38) and sodic red texture contrast soils (39)
Seasonally wet soils: sodic yellow and grey texture contrast soils (33)
Soil type sites
LS3, LSWW9, LSWW5
LSWW11, LSWW17, NA174
NA171, NA141, NA178
Surface texture
Sandy loam
Medium clay
Loamy sand
Sand
Permeability
Moderate
Slow
Moderate
Very slow
Depth (m)
> 1.2
> 2
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Hardsetting upper soil susceptible to sheet and rill erosion along with wind erosion when exposed. Dispersive and deep subsoils susceptible to gully erosion on steeper slopes.Susceptible to inundation and waterlogging on backplain. Surface soils friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.Susceptible to wind and sheet erosion where sandy surfaces with little organic matter are exposed. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Susceptible to seasonal inundation, waterlogging and ultimately soil salinity. Upper soils susceptible to sheet erosion and wind erosion when exposed.
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