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GP21

Site GP21 Landscape

A1	0-20 cm	Dark greyish brown (10YR4/2); sandy loam; very weak consistence moist; weak crumb structure; pH 5.6; clear change to:	Site GP21 Profile
A2	20-35 cm	Greyish brown (10YR5/2); sporadically bleached loamy sand; weak consistence moist, firm to very firm dry; pH 5.7; sharp change to:
Subsoil
B21	35-70 cm	Dark greyish brown (10YR4/2) with brownish yellow (10YR6/8) and yellowish brown (10YR5/8) mottles; medium heavy clay; strong medium prismatic, parting to strong coarse blocky structure; contains dark organic stains on ped faces; very strong consistence dry; pH 6.1; clear change to:
B22	70-110 cm	Dark greyish brown (10YR4/2) with red (2.5YR4/8) and brownish yellow (10YR6/8) mottles; medium heavy clay; pH 6.4; clear and wavy change to:
2A	110-140 cm	Brownish yellow (10YR6/6) sandy loam (clayey); structureless; contains patches of bleached sand and a few ironstone gravels (1-2 mm size); pH 7.1.

• Strong texture contrast between surface (A) horizons (10 % clay) and subsoil (B21) horizon (48 % clay).
  
• Dense and coarsely structured (prismatic) subsoil.

The surface soil is moderately acid. The subsoil becomes decreasingly acidic with increasing depth down the profile.		The salinity rating is very low throughout the soil profile.
The upper subsoil is sodic and the profile becomes increasingly sodic with depth.		The clay content increases significantly at the A/B horizon interface.
The coarse sand percentage decreases in the upper subsoil but increases again at depth in the buried soil.

• Plant available water capacity (PAWC) is considered to be very low (estimated at 40 mm). This is based on available laboratory data and assumes an effective rooting depth of 35 mm. Rooting depth will be limited by the dense and coarsely structured clay subsoil which is sodic and magnesic.

• The sporadically bleached A2 horizon indicates that periodic waterlogging occurs above the slowly permeable subsoil. When waterlogging occurs, the subsurface layer is likely to become ‘spewy’. Sub-surface drainage is often required.

• The surface soil has a low inherent fertility (based on the sum of the exchangeable basic cations). Organic matter is important for soils such as these with relatively low clay contents in order to enhance nutrient holding capacity. Levels of exchangeable potassium are relatively low in the surface horizons which may lead to a potash deficiency for plants. This can be assessed by plant tissue analysis.

• The surface soil is moderately acid and soil pH may need to be raised to meet preferred ranges for vegetable crops.

• The water holding capacity of the surface soil is low. Organic matter is important for these soils in order to enhance water-holding capacity. Organic matter additions will also improve soil aggregation and enhance root and water movement in the surface soil.
  

• The dense and coarsely structured upper subsoil is sodic and has a very low exchangeable calcium:magnesium ratio. This results in dispersion when the clay soil swells after wetting. Clay dispersion causes subsoil pores to become blocked and this results in restricted subsoil drainage. Root penetration will also be restricted.

• Nutrient imbalances (e.g. calcium, potassium deficiency) may occur in the subsoil as it is dominated by exchangeable magnesium. Nutrient deficiencies can be assessed by plant tissue analysis.

• The fine surface sands can compact and restrict water movement. To overcome this the soil is ploughed into the clay layer (45 cm or more) and turned upside down once per year. Gypsum is also added.
• Leeks and parsnips grown here.
• Soil variability across the paddock is high.
• Extensive drainage required to set up operation (storm water and agricultural drains and irrigation).

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