Victorian Resources Online (archived)

GP76

Location: Boisdale.	Australian Soil Classification: Melanic, Eutrophic, Black DERMOSOL.
Geology: Holocene floodplain deposits.	General Landscape Description: Floodplain of Avon River.
Mapping Unit: Clydebank: Thomson.	Site Description: Dairy grazing paddock.

Site GP76 Landscape

Soil Profile Morphology:

Surface Soil

A1	0-30 cm	Very dark brown (10YR2/2); fine sandy clay loam; moderate coarse blocky, parting to strong fine polyhedral structure; strong consistence dry; pH 5.9; gradual change to:	Site GP76 Profile
Subsoil
B21	30-50 cm	Black (10YR2/1); fine sandy clay loam; weak coarse prismatic, parting to strong fine polyhedral structure; pH 6.3:
B22	50-90 cm	Dark brown (7.5YR3/2); fine sandy clay loam; moderate coarse prismatic structure; pores evident; pH 6.8:
B23	90+ cm	Brown (7.5YR4/2); fine sandy clay loam; weakly structured; pH 7.1.

Key Profile Features:

Uniform clay content throughout soil profile.
Well structured upper profile (parting to fine polyhedral shaped peds).

Soil Profile Characteristics:

Horizon	pH	Salinity Rating	Sodicity	Dispersion
Surface (A1 horizon)	Moderately Acid	Low	Non-Sodic	-
Subsoil (B21 horizon)	Slightly Acid	Very Low	Non-Sodic	None¹
Deeper Subsoil (at 90 cm)	Slightly Alkaline	Very Low	Non-Sodic	-

¹ Slight dispersion after remoulding.

	The surface is moderately acid. The upper subsoil is slightly acid becoming slightly alkaline at 90 cm.		The profile is non-sodic throughout.
	The surface salinity rating is low. The subsoil rating is very low throughout.		The clay content remains constant throughout the profile.

Horizon	Horizon Depth (cm)	pH (water)	pH (CaCl₂)	EC 1:5	ESP %	Exchangeable Cations
						Ca	Mg	K	Na
						meq/100g
A1	0-30	5.9	5.2	0.12		10	2.9	0.94	0.22
B21	30-50	6.3	5.3	<0.05		10	2.8	0.31	0.2
B22	50-90	6.8	5.7	<0.05		10	3.2	0.17	0.21
B23	90+	7.1	6	<0.05		7.3	4.3	0.08	0.24

Horizon	Horizon Depth (cm)	Exchangeable Aluminium mg/kg	Exchangeable Acidity meq/100g	Wilting Point pF2.5	Wilting Point pF4.2	Coarse Sand (0.2-2.0 mm)	Fine Sand (0.02-0.2 mm)	Silt (0.002-0.02 mm)	Clay (<0.002 mm)


A1	0-30				14.4	4	44	24	21
B21	30-50	<10	8.6		10.3	2	51	23	20
B22	50-90				9.5	2	52	22	19
B23	90+

Management Considerations:

Whole Profile

Plant Available Water Capacity (PAWC) is considered to be moderate (estimated at 105 mm) for this soil profile. This is based on an estimated effective rooting depth of 50 cm (i.e. surface soil and upper subsoil). The denser and more coarsely structured deeper subsoil is likely to restrict rooting depth, although not to the same extent as some of the more sodic subsoils in the region. Much of the plant available water (i.e. 70 mm) will be in the surface (A1) horizon. PAWC has been estimated using a model developed by Littleboy (1995) which uses analytical data for clay%, silt%, fine sand%, coarse sand % and wilting point
Infiltration of water will be rapid throughout the upper soil profile due to the well developed structure and pore space available

Surface (A) Horizons

The relatively deep surface soil is well structured (parting to many fine polyhedral shaped peds) and has a weak consistence. As a result, very good seed-bed conditions are provided
Infiltration of water into the well structured surface soil will be quite high. This horizon will also be well drained
The nutrient holding capacity of the surface (A1) horizon is moderate (based on the sum of the exchangeable cations). Organic matter is important in soils such as these with high fine sand contents for enhancing soil fertility, water holding capacity and aggregation. Nitrogen levels are also high reflecting the high organic matter levels

Subsoil (B) Horizons

The upper subsoil soil is also well structured (parting to many fine polyhedral shaped peds) and will provide a good environment for roots and relatively rapid water movement
The deeper subsoil becomes more coarsely structured and will be more restrictive to root movement

Comments from Landholder:

Black soil dries out more than red soil and becomes cloddier
Floods every 20 years or so.

Profile Described By: Mark Imhof and Ian Sargeant (22/04/1998).

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