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Soil/Landform Unit 137

Landform Unit Description

Unit 137 image a
The gently undulating plains have dark texture contrast soils on slopes with poorly drained soils in depressions. Stones are common on some slopes
      Area: 4810 ha
      0.36% of CMA region

      This gently undulating plains unit (part of the volcanic Western Plains) has well developed drainage and deep regolith. This unit of basaltic and sedimentary plains is dominated by one large occurrence just north of Camperdown extending to the western boundary of the catchment. Eruption point complexes (Units 110, 98, 107) are to the south, and a lake and stony rises complex (Unit 112) to the north. Unit components include very low rises as well as plains with remnant Plains Grassy Woodland. The soils are black texture contrast soils (Chromosols) and are strongly sodic on the basalt (Sodosols). Some of these soils may have friable surface soils; however, lighter surface textures are more prone to nutrient decline and sheet erosion on the slopes, while the plains and depressions are more susceptible to waterlogging. Rainfall is sufficient to promote intensive grazing (mainly for dairying) and minor cropping.
Unit 137 geomorphology

Unit 137 image b
Gently undulating plains with annual pastures near Kariah
Unit 137 cross section

Unit 137 graph

Component
1
2
3
4
Proportion of soil-landform unit
20%
25%
50%
5%
CLIMATE
Rainfall (mm)

Annual: 750
Temperature (oC)
Minimum 8, Maximum 19
Precipitation less than potential evapotranspiration
November-March
GEOLOGY
Age and lithology

Neogene
fluvial and marine gravel, sand, silt and clay, Quaternary basalt and scoria deposits
Geomorphology
LANDUSE
Uncleared: Nature conservation
Cleared: Beef cattle and sheep grazing; dairy farming; cropping (ceral and summer fodder)
TOPOGRAPHY
Landscape

Undulating basalt plains
Elevation range (m)
140-220
Local relief (m)
3-5
Drainage pattern
Parallel
Drainage density (km/km2)
1.3
Landform
Gently undulating plains
Drainage depressions
Landform element
Broad crest
Slopes
Plains
Drainage lines
Slope and range (%)
2 (0-5)
5 (3-10)
2 (1-3)
2 (0-3)
Slope shape
Convex
Convex
Straight
Concave
NATIVE VEGETATION
Ecological Vegetation Class

Plains Grassy Woodland (3.1%)
SOIL
Parent material

Sand, silt and clay; basalt

Sand, silt and clay; basalt

Sand, silt and clay; basalt
Alluvial sand, silt and clay
Description
(Corangamite Soil Group)
Neutral mottled black texture contrast soils (13/35)
Neutral mottled black texture contrast soils (13/35)
Neutral mottled black texture contrast soils (13/35)
Alkaline black texture contrast soils (32)
Soil type sites
SFS20, SW88, SW95
Surface texture
Loamy sand; fine sandy loam
Loamy sand; fine sandy loam
Loamy sand; fine sandy loam
Fine sandy loam
Permeability
Low to moderate
Low to moderately high
Low to moderate
Low
Depth (m)
<2
<2
<2
>2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS
Texture contrast, low to moderate water holding capacity and nutrient holding capacity depending on depth and stoniness in upper soil, high in subsoil. Non-sodic (moderate structure) and strongly sodic (coarse structure) subsoils. Moderate site drainage. Some susceptibility to nutrient decline and sheet and rill erosion.
Texture contrast, low to moderate water holding capacity and nutrient holding capacity depending on depth and stoniness in upper soil, high in subsoil. Non-sodic (moderate structure) and strongly sodic (coarse structure) subsoils. Moderate site drainage. Some susceptibility to nutrient decline and sheet and rill erosion.
Texture contrast, low to moderate water holding capacity and nutrient holding capacity depending on depth and stoniness in upper soil, high in subsoil. Non-sodic (moderate structure) and strongly sodic (coarse structure) subsoils. Slow to moderate site drainage. Some susceptibility to nutrient decline and sheet and rill erosion.
Texture contrast, low to moderate water holding capacity and nutrient holding capacity depending on depth and stoniness in upper soil, high in subsoil. Non-sodic (moderate structure) and strongly sodic (coarse structure) subsoils. Very slow site drainage. Some susceptibility to waterlogging and nutrient decline.
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