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Soil/Landform Unit - Douglas lakes and lunettes

Landform Unit Description

WLRA Landform Douglas lake and lunettes
Looking south down the Douglas Depression with Lake Copper Colour (kidney shaped lake to left), North Lake, Central Lake and White Lake the major lakes further south
      Area: 5759 ha
      0.25% of CMA region

      Within the Douglas Depression are a number of lakes and lunettes that vary from saline to freshwater in nature. As part of the salt lake depression of the North Western Dunefields and Plains, the soils of the lakes and lunettes include seasonally wet soils that are sodic yellow and grey texture contrast (Hydrosols) in lakes and grey to brown cracking clay soils (Vertosols) on plains and lunettes. The soils are very susceptible to seasonal inundation and waterlogging. Cracking clay soils have friable surfaces that can be vulnerable to compaction at critical moisture contents. Land use on these playa plain complexes is dryland cropping and grazing, while nature conservation is also a major use owing to high salinity levels and seasonally wet states. There are a number of woodland vegetation communities including Heathy Woodland, Low Rises Woodland, Lignum Swampy Woodland, Plains Woodland and Salt Paperbark Woodland. Other vegetation communities include Ridged Plains Mallee, Samphire Shrubland, Red Gum Wetland, Plains Savannah, Saline Lake Mosaic and Inland Saltmarsh.
WLRA Landform Douglas lake and lunettes

WLRA Landform Douglas lake and lunettes
Looking north up the Douglas Depression towards Mt Arapiles
WLRA Landform Douglas lake and lunettes

WLRA Landform Douglas lake and lunettes

WLRA Landform Douglas lake and lunettes
Saline lake within the Douglas Depression

Component
1
2
Proportion of soil-landform unit
70%
30%
CLIMATE
Rainfall (mm)

Annual: 460
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology

Quaternary paludal silt and clay; Quaternary fluvial silt, sand and minor gravel (Shepparton Formation); Quaternary aeolian dune sand (Lowan Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation; water supply
Cleared areas: sheep grazing; water supply
TOPOGRAPHY
Landscape

Lake and lunettes
Elevation range (m)
104–174
Local relief (m)
0–1
Drainage pattern
Centripetal–dendrtic
Drainage density (km/km2)
1.3
Landform
Lake and lunettes
Landform element
Playa/lunette complex including water bodies
Gently undulating plain
Slope and range (%)
4 (1-7)
5 (2-9)
Slope shape
Concave
Straight to convex
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (14.1%), Plains Savannah (13.2%), Salt Paperbark Woodland/Samphire Shrubland Mosaic (13.1%), Ridged Plains Mallee (12.3%), Other (43.5%)
SOIL
Parent material

Swamp deposits (sand, silt and clay), evaporites and aeolianites, aeolian dune sand and clay

Marine sand and silt, fluvial silt, sand and minor gravel
Description
(Corangamite Soil Group)
Seasonally wet soils: sodic yellow and grey texture contrast soils (33)
Grey and brown cracking clay soils (37)
Soil type sites
NA171, NA141, NA178
LS3, LSWW9, LSWW5
Surface texture
Sand
Medium clay
Permeability
Slow
Slow
Depth (m)
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Susceptible to seasonal inundation, waterlogging and ultimately soil salinity. Upper soils susceptible to sheet erosion and wind erosion when exposed. Susceptible to inundation and waterlogging in lower areas. Surface soils friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.
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