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Soil/Landform Unit - Edenhope plains and sub-dunes

Landform Unit Description

WLRA Landform Edenhope plains and sub-dunes
Looking south-west over plains with subdued rises (ridges) and sand plains (often denoted by remnant vegetation of the Kowree unit) east of Edenhope
      Area: 19591 ha
      0.84% of CMA region

      Plains in the south-west of the catchment with subdued ridges show a recurring sequence of very gentle topography from slight ridges to freshwater lakes with lunettes. Ridges have a NNW/SSE trend and plains are also associated with drainage complexes. Located within the low ridges and oriented swales of the North Western Dunefields and Plains (5.5.2), the unit is contiguous with much of the Kowree unit around Edenhope, and grades into the Apsley unit to the west and Ullswater unit to the north. Soils include sodic red texture contrast soils (Sodosols) that occur mainly on ridges and plains while sodic brown, yellow and grey texture contrast soils (Sodosols) occur mainly on plains and drainage depressions. Land use is mainly cereal cropping and pasture production along with sheep and cattle grazing. The main vegetation communities include Heathy Woodland, Damp Sands Herb-rich Woodland, Plains Sedgy Woodland, Shallow Sands Woodland, Plains Woodland, Red Gum Wetland and several woodland mosaic vegetation formations.
WLRA Landform Edenhope plains and sub-dunes

WLRA Landform Edenhope plains and sub-dunes
Plains east of Wombelano with subdued rises
WLRA Landform Edenhope plains and sub-dunes

WLRA Landform Edenhope plains and sub-dunes

WLRA Landform Edenhope plains and sub-dunes
Remnant vegetation stand south-east of Edenhope

Component
1
2
3
4
Proportion of soil-landform unit
20%
70%
7%
3%
CLIMATE
Rainfall (mm)

Annual: 615
Temperature (oC)
Minimum 8, Maximum 20
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology

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

Plains with subdued ridges
Elevation range (m)
146–199
Local relief (m)
2–3
Drainage pattern
Dendritic
Drainage density (km/km2)
0.3
Landform
Rises
Plains and drainage complex
Landform element
Ridge slope
Plain
Drainage depression
Swamp bed
Slope and range (%)
2 (1-5)
1 (0-2)
0 (0-2)
0 (0-1)
Slope shape
Convex
Straight
Concave
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Shallow Plains Woodland (30.0%), Plains Woodland (13.7%), Heathy Woodland (13.3%), Damp Sands Herb-rich Woodland (7.3%), Other (33.4%)
SOIL
Parent material

Marine sand and silt

Marine sand and silt

Fluvial gravel, sand and silt

Swamp silt and clay
Description
(Corangamite Soil Group)
Sodic red texture contrast soils (39)
Sodic brown, yellow and grey texture contrast soils (38)
Grey and brown cracking clay soils (37)
Seasonally wet soils: sodic yellow and grey texture contrast soils (33)
Soil type sites
LSWW11, LSWW17, LSWW13
LS3, LSWW9, LSWW5
NA171, NA141, NA178
Surface texture
Sandy loam
Loamy sand
Medium clay
Sand
Permeability
Moderate
Moderate
Slow
Slow
Depth (m)
> 1.2
1.3
> 2
> 1.5
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 where exposed. Compaction of upper soil variable depending on soil depth and moisture content. Upper soil is susceptible to acidification.Susceptible to wind and sheet erosion where surfaces with little organic matter are exposed. Susceptible to compaction where hardsetting and restricted drainage.Susceptible to inundation and waterlogging in lower areas, but can be variable due to micro relief (gilgai). Surface soils are friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.Susceptible to seasonal inundation, waterlogging and soil salinity. Upper soils susceptible to sheet erosion and wind erosion when exposed.
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