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

Victorian Resources Online

GHF09b

Location: Byaduk

Australian Soil Classification: Ferric, Eutrophic, Brown CHROMOSOL
General Landscape Description: Level plain
Site Description: Flat
Land Unit: Warrabkook Basalts
Geology: Quaternary basalt

General Land Unit Description: This land unit consists of gently undulating basalt plains in the Macarthur area. In some drainage lines, the basalt has been dissected sufficiently to expose the underlying sediments. The soils on the basalt plains are commonly Brown Kurosols or Chormosols, intermixed with Sodosols, particularly on the lower slopes and drainage depressions. This site has two year old Eucalyptus globulus in a plantation on ex-agricultural land.

Soil pit Kan98 1-4 landscape



Soil Profile Morphology



Surface

A10-10 cmVery dark grey (10YR3/1); clay loam; weak medium polyhedral structure , parting to weak medium granular structure; very weak consistence when moist; contains a few medium ferruginous nodules; many medium roots present; pH 5.1; clear and smooth transition to:


Soil pit Kan98 2 profile
A210-22 cmVery dark greyish brown (10YR3/2); clay loam; contains , many medium ferruginous nodules, common subangular moderately strong cobbles; common medium roots present; pH 5.6; abrupt and smooth transition to:
Subsoil


B2122-70 cmYellowish brown (10YR5/6), with common medium distinct red (2.5YR5/7) mottles; medium clay; moderate coarse polyhedral structure, parting to moderate medium granular structure; weak consistence, moderately moist; contains a few medium ferruginous nodules; common subangular moderately strong cobbles present;contains a few medium roots; pH 5.6; diffuse and smooth transition to:


B2270-100 cmPale brown (10YR6/3), with common medium faint yellowish brown (10YR5/7) and red (2.5YR4/8) mottles; medium heavy clay; moderate coarse polyhedral structure, (parting to moderate medium granular structure; very weak consistence, moderately moist; contains a few medium ferruginous nodules; common subangular moderately strong cobbles present; a few very fine roots present; pH 6.7; clear and smooth transition to:


C100-140 cmLight grey (10YR7/1); light clay; very abundant coarse fragments present; very weak consistence, moist; contains very abundant subangular moderately strong cobbles; a few very fine roots present; changes to:


140-220 cmSimilar to layer above; changes to:


220-410 cmMixed mottled clays and decomposing vesicular basalt, the basalt between 100-220 cm is most likely a large floater, live roots observed to 410 cm.


Key Profile Features:
  • Strong texture contrast between surface (A) horizons and subsoil (B21) horizon.

Soil Profile Characteristics:
-

pH
Salinity
Surface Soil
(A1 horizon)
Strongly Acid
Very Low
Non-Sodic
None
Subsoil
(B21)
Moderately Acid
Very Low
Non-Sodic
None
Deeper Subsoil
(70-100 cm)
Slightly Acid
Very Low
Marginally Sodic
None




Chemical and Physical Analysis:
Horizon
Horizon Depth
(cm)
pH
(water)
pH
(CaCl
2)
EC
dS/m
Exchangeable Aluminium
ppm
Exchangeable Acididty
meq/100g
Exchangeable Cations
Coarse Sand
(0.2-2.0 mm)
%
Fine Sand
(0.02-0.2 mm)
%
Silt
(0.002-0.02 mm)
%
Clay
(<0.002 mm)
%
Field Capacity
% w/w
Wilting Point
% w/w
Ca
Mg
K
Na
meq/100g
A1
0-10
5.1
4.5
0.08
52
15
3.6
1.6
0.14
0.16
37
20
12
24
22.0
11.4
A2
10-22
5.6
4.8
0.07
15
11
3.2
1.6
0.10
0.22
38
22
12
26
34.7
11.7
B21
22-70
6.5
6.1
0.14
9.9
5.3
6.2
0.14
0.96
6
6
7
81
34.9
29.9
B22
70-100
6.7
6.0
0.14
9.6
6.4
10
0.14
1.8
6
13
13
68
37.7
29.2



Profile Described By: Ian Sargeant, Paul Feikema and Martin Clark, 3rd November 2000.
Page top