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Soil/Landform Unit - Kanawinka sandsheets and dunes

Landform Unit Description

WLRA Landform Kanawinka sand sheets and dunesSeasonally wet soils with heath woodlands of manna, swamp, yellow or pink gums
      Area: 385 ha
      0.02% of CMA region

      Sandsheets and plains in the south-west corner of the Wimmera CMA region consist of sand dunes with gentle slopes and crests as well as sandsheets on plains with scattered swamps. As the only unit in the region to be part of the Western Plains, land use includes grazing by sheep and cattle along with irrigated agriculture where sandy surface soils are used as part of centre pivot systems. Soil profiles are sandy throughout except in swamps where cracking clays occur and on plains where deep sand overlies heavier subsoils as Sodosols. Remnant vegetation is largely either Plains Grassy Woodland or Damp Sands Herb-rich Woodland/Plains Swampy Woodland/Aquatic Herbland Mosaic vegetation community. The main form of land degradation is wind erosion where sandy surfaces lack sufficient ground cover.
WLRA Landform Kanawinka sand sheets and dunes

WLRA Landform Kanawinka sand sheets and dunes
Stringybarks with heath understorey
WLRA Landform Kanawinka sand sheets and dunes

WLRA Landform Kanawinka sand sheets and dunes

WLRA Landform Kanawinka sand sheets and dunes
Treeless heaths with sandy surface soils

Component
1
2
3
4
5
Proportion of soil-landform unit
10%
30%
30%
10%
20%
CLIMATE
Rainfall (mm)

Annual:
Temperature (oC)
Minimum 8, Maximum 20
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology

Neogene marine sand and silt (Parilla Sand);
Quaternary aeolian dune sand, paludal silt and clay
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep and cattle grazing; irrigated horticulture; softwood plantations
TOPOGRAPHY
Landscape

Sandsheets and dunes
Elevation range (m)
126–139
Local relief (m)
5
Drainage pattern
Dendritic
Drainage density (km/km2)
0.3
Landform
Low lying regular dunes
Plains and swamps
Landform element
Gentle dune crest
Dune slope
Plains and gentle slope
Swamp bed
Sandsheet
Slope and range (%)
2 (0-8)
3 (1-15)
3 (1-7)
0 (0-1)
2 (1-5)
Slope shape
Convex
Concave
Straight
Concave
Straight
NATIVE VEGETATION
Ecological Vegetation Class
Plains Grassy Woodland (33.3%), Damp Sands Herb-rich Woodland/Plains Swampy Woodland/Aquatic Herbland Mosaic (33.3%)
SOIL
Parent material

Aeolian sand and silt

Aeolian sand and silt

Paludal silt and clay

Paludal silt and clay

Aeolian sand and silt
Description
(Corangamite Soil Group)
Sandy soils with and without pans (31)
Sandy soils with and without pans (31) and sodic brown, yellow and grey texture contrast soils (38)
Sodic brown, yellow and grey texture contrast soils (38)
Grey and brown cracking clay soils (37)
Sodic brown, yellow and grey texture contrast soils (38)
Soil type sites
WLRA74, WLRA85, LSWW11
LSWW11, LSWW17, LSWW13
LS3, LSWW9, LSWW5
LSWW11, LSWW17, LSWW13
Surface texture
Sand
Loamy sand
Loamy sand
Medium clay
Loamy sand
Permeability
High
High
Moderate
Slow
Moderate
Depth (m)
> 1.5
> 1.5
1.3
> 2
1.3
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.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 and surfaces with little organic matter. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Susceptible to seasonal inundation and waterlogging. Slightly susceptible to surface sheet erosion where soils are exposed. 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 exposed and surfaces with little organic matter. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.
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