SG9

Site SG9 Landscape

Soil Profile Morphology:

Surface Soil			Site SG9 Profile
A11	0-20 cm	Black (10YR2/1); sandy loam; loose surface condition; weak fine crumb structure; pH 4.8; abrupt change to:
A12	20-40 cm	Dark grey (10YR4/1); loamy sand; structureless; pH 5.5; clear change to:
A2	40-50 cm	Greyish brown (10YR5/2) conspicuously bleached; sandy loam; structureless; pH 5.3; sharp change to:
Subsoil
Bh	50-55 cm	Black (10YR2/1); sandy loam; structureless; weak consistence wet; pH 4.6; abrupt and wavy change to:
Bhs	55-65 cm	Brown (10YR4/3); sandy clay loam; moderate blocky structure; contains some variably cemented "coffee rock" segregations; firm consistence wet; pH 4.6; clear change to:
D21	65-90 cm	Grey (10YR6/1) with strong brown (7.5YR5/6) mottles; sandy loam; very weak coarse blocky structure; firm consistence wet; pH 4.8; gradual change to:
D22	90+ cm	Grey (10YR6/1) with brownish yellow (10YR6/8) and red (2.5YR4/8) mottles; medium clay (sandy); weak coarse blocky structure; firm consistence wet; pH 4.8.

• The subsoil is saturated for a number of months of the year (i.e. Aquic)
• Subsoil accumulation of iron and organic matter (i.e. "coffee rock").

The surface soil is very strongly acid. The subsurface horizons are strongly acid. The subsoil (from 50 cm) is very strongly acid throughout.	Soluble salt levels are very low throughout the profile.	The exchangeable aluminium level is low in the surface horizons but becomes high in the subsoil (D) horizons (from 50 cm depth).	The clay content increases significantly at 55 cm depth.

Horizon	Horizon Depth (cm)	pH water	pH CaCl2	EC 1:5	Exchangeable Cations				Ex. Al mg/kg	Ex. Acidity meq/100g	Wilting Point pF 4.2	Coarse Sand (0.2 - 2 mm)	Fine Sand (0.02-0.2 mm)	Silt (0.002-0.02 mm)	Clay (<0.002 mm)
					Ca	Mg	K	Na
					meq/100g
A11	0-20	4.8	3.7	0.06	4.6	1.6	0.2	0.1	33	18.8	1	28	47	5	5
A12	20-40	5.5	4.0	<0.05	0.3	0.1	<0.1	<0.1
A2	40-50	5.3	4.1	<0.05					<10	<0.4
Bh	50-55	4.6	3.6	0.07					250	26.6	9.9
Bhs	55-65	4.6	4.0	0.09	0.6	1.1	0.2	0.1	180	31.4	17	17	32	7	38
D21	65-90	4.8	4.2	0.05	0.1	0.4	0.1	<0.1	250	6.8		32	48	6	14
D22	90+	4.8	4.0	0.08	1.4	0.4	0.1	0.1	260	9.8

• The presence of a deep water table which rises close to the surface in winter will result in the profile being saturated for a number of months. Root growth will be limited in such poorly aerated soils. Plant available water capacity (PAWC) will therefore be very low.

• The surface soil is very strongly acid but the exchangeable aluminium level measured in the laboratory is not high. A pH/aluminium test sampled across the paddock may be appropriate to determine whether lime is needed to raise the soil pH. Other factors need to be considered before lime is recommended (e.g pasture species grown, method of application, local trial responses, soil surface structure and likely cost/benefit). The pH increases in the subsurface (A12 and A2) horizons and negligible exchangeable aluminium is present.
• Deficiencies in molybdenum, phosphorus and potassium may occur in the very strongly acid surface soil. Potassium deficiency may also be induced by the high exchangeable magnesium percentage (i.e. 24%). Increasing soil pH by lime application will enable phosphorus (from superphosphate application) to be more available. If lime is required and pH is increased, the availability of major nutrients should improve.
• Trace elements such as copper and zinc are likely to be low. Plant tissue analysis may give a more accurate assessment of trace element requirements.
• Apart from the surface (A11) horizon, all the horizons below have a very low inherent fertility (based on the sum of the exchangeable basic cations).

• The exchangeable aluminium levels become high in the very strongly acid subsoil from 50 cm depth. These levels are likely to affect the growth of aluminium sensitive species.
• Inherent fertility is very low for the subsoil horizons (based on the sum of the exchangeable basic cations).
• The "coffee rock" layer is likely to result in some restriction to root and water movement.