Your gateway to a wide range of natural resources information and associated maps

Victorian Resources Online

OTR608

OTR608 landscape
Dissected sand hills near Chapple Vale

    Site Code
OTR608


OTR608 profile

Melacic, Humic/alsilic, Semiaquic, Podosol
    Location
Chapple Vale
    Landform
Hills
    Geology
Palaeogene Pebble Point Formation/Quaternary aeolian deposits
    Element
Hillslope –mid slope
    Slope
12%
    Aspect
North westerly
Horizon
Depth (cm)
Description
A1
0–25Very dark brown (10YR2/2); loamy fine sand; weak subangular blocky structure; gradual smooth boundary to:

A2
25–60Very dark greyish brown (10YR3/2); fine sand; weak subangular blocky structure; occasional quartz gravel; clear wavy boundary to:

B1
60–69Black (10YR2/1); loamy fine sand; apedal single grain structure; clear wavy boundary to:

B2
69–75Dark brown (10YR 3/2); sandy clay loam; apedal single grain sturcture; abrupt wavy boundary to:

2Cm
75+Dark yellowish brown (10YR4/4); cemented sand; apedal massive structure; extremely hard.

Management considerations
Deep sandy soils generally have poor plant water/nutrient holding capacity. The sandy nature of the soils make them prone to wind and sheet and rill erosion. Soils may be hydrophobic (in conjunction with organic coatings) when dried out, taking time to reabsorb moisture. These soils do however drain rapidly. The soil profile is consistently acidic (often associated with sandy surfaces due to the lack of base minerals) and may or may not have organic matter (humose or peaty surfaces). This restricts the uptake of certain nutrients as well as intolerance for some plant species (due in part to the increasing mobilisation of aluminium and manganese). Deficiencies of calcium, potassium and molybdenum are likely. Coffee rock is a pan of variable strength that is found beneath 75cm in these soils (Podosols) where sesquioxides (iron and aluminium) and organic matter have cemented soil material. Where this is only weakly developed then it is called a fragipan. This is often a restriction for root development by limiting water and gas movement. This may also have an influence on subsurface water movement such as lateral flow.

Analytical data
Site OTR608
Sample
depth
pH
EC
NaCl
Ex Ca
Ex Mg
Ex K
Ex Na
Ex Al
Ex acidity
FC
(-10kPa)
PWP
(-150kPa)
KS
FS
Z
C
Horizon
cm
H2O
CaCl2
dS/m
%
cmolc/kg
cmolc/kg
cmolc/kg
cmolc/kg
mg/kg
cmolc/kg
%
%
%
%
%
%
A1
0-10
4.6
N/R
0.058
0.006
0.5
0.7
0.2
0.3
N/R
N/R
N/R
N/R
70
10
4
6
A1
10-20
4.5
N/R
0.041
0.004
0.3
0.5
0.07
0.13
N/R
N/R
N/R
N/R
78
10
4
9
A2
30-60
4.6
N/R
0.018
0.001
0.08
0.14
<D.01
0.04
N/R
N/R
N/R
N/R
78
15
4
2
B1
60-69
4.3
N/R
0.047
0.004
0.05
0.17
0.03
0.22
N/R
N/R
N/R
N/R
70
13
3
9
B2
69-75
4.2
N/R
0.048
0.004
0.01
0.02
0.01
0.04
N/R
N/R
N/R
N/R
62
9
6
17
11Cm
90-120
4.8
N/R
0.015
0.001
0.01
0.05
0.02
0.10
N/R
N/R
N/R
N/R
72
20
2
3
Page top