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Soil/Landform Unit - Nurcoung plains

Landform Unit Description

WLRA Landform Nurcong plains
Plains surrounding West Wimmera wetlands near Minimay
      Area: 13 861 ha
      0.59% of CMA region

      This unit of consists of many small occurrences from Minimay in the west to Mitre in the east and also south of the Wimmera Highway east of Miga Lake. This plains complex unit is part of the North West Dunefields and Plains; ridges with sands and flats (5.5). These plains, depressions and lunettes of Quaternary sediments occur between the NNW/SSE orientated ridges between the Little Desert (5.2) and amongst more open sand plains and low ridges to the south. Dominated by the plain/open depression, dune slopes (lunettes) also occur. Site drainage is slow to very slow, but moderate on the dune slopes. Predominantly soils are grey and brown cracking clay soils (Vertosols) on the plains with sodic yellow, brown and grey texture contrast soils (Sodosols) on the dune slopes. Topsoils are often hardsetting and shallow, occasionally self-mulching. Soil compaction is also a susceptibility factor with these heavier soils and soils that are hardsetting. Broadacre dryland cropping is the major enterprise with some grazing (sheep, some cattle) depending on climate. Remnant vegetation consists of a number of vegetation communities including Plains Savannah, Shallow Sands Woodland, Plains Woodland, and Heathy Woodland for example.
WLRA Landform Nurcong plains

WLRA Landform Nurcong plains
Sequence of swamps and plains near Minimay between rises
WLRA Landform Nurcong plains

WLRA Landform Nurcong plains

WLRA Landform Nurcong plains
Bean crop on lower slopes

Component
1
2
Proportion of soil-landform unit
85%
15%
CLIMATE
Rainfall (mm)
Annual: 515
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
September–April
GEOLOGY
Age and lithology
Quaternary paludal silt and clay; Quaternary aeolian dune sand (Lowan Sand); Neogene marine sand and silt (Parilla Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation; water supply
Cleared areas: dryland cropping; sheep grazing
TOPOGRAPHY
Landscape
Plains
Elevation range (m)
123–195
Local relief (m)
3–4
Drainage pattern
Dendritic
Drainage density (km/km2)
0.6
Landform
Gently undulating plains
Landform element
Plain/open depression
Dune slope
Slope and range (%)
2 (1-6)
5 (2-9)
Slope shape
Straight
Convex
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (47.8%), Shallow Sands Woodland (14.9%), Plains Savannah (12.1%), Red Gum Wetland (8.9%), Other (16.3%)
SOIL
Parent material
Marine sand and silt, paludal silt and clay
Aeolian sand
Description
(Corangamite Soil Group)
Grey and brown cracking clay soils (37)
Sodic brown, yellow and grey texture contrast soils (38)
Soil type sites
LS3, LSWW9, LSWW5
LSWW11, LSWW17, LSWW13
Surface texture
Medium clay
Loamy sand
Permeability
Very slow
Moderate
Depth (m)
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Susceptible to inundation and waterlogging in depressions. 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 surfaces are exposed. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.
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