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| SW60 | Reticulate, Mesotrophic, Brown CHROMOSOL | |
| South of Simpson: Cooriemungle Road and Princetown Road | |||
| Gently undulating plain | |||
| Neogene Hanson Plain Sand Formation | |||
| Level to slightly sloping plain | |||
| <1% | |||
| 0 | |||
Horizon | Depth (cm) | Description | ||
Ah | 0-25 | Very dark greyish brown (10YR3/2 moist and dry); loamy sand, apedal, pH 5.1; abrupt and smooth boundary to: | ||
A2 | 25-40 | Brownish yellow (10YR6/8); sandy clay loam; massive; pH 6.0; clear and wavy change to: | ||
B21t | 40-70/90 | Light olive brown (2.5Y5/3) ped exterior, yellowish brown (10YR5/6) to red (2.5YR5/8) interiors; medium clay; fine to coarse (5-30 mm) polyhedral structure; smooth ped faces; very firm consistence; pH 5.8; irregular and clear change to: | ||
B/C | 70/90+ | Light grey (2.5Y7/1) ped exterior, with yellowish brown (10YR5/8) to yellowish red (5YR5/6) interiors conspicuous coarse (50-100 mm) reticulate mottling; very coarse to coarse (30-100 mm) polyhedral, parting to medium to fine (5-30 mm) polyhedral structure; smooth faced peds; pH 5.5. | ||
Management considerations | ||||
This is one of the better soils of the dairying country in the south east of the region. It has generally higher clay content and better structure than other soils derived from the Hanson Plain Sand (compare SW61 Podosol and SW62 Hydrosol). Topsoils across all of the Hanson Plain Sand soils are very sandy and acid. The soil at this dairy farm will have had lime added, hence the favourable surface horizon pH. Low Ca:Mg ratio in the subsoil could limit plant growth. The change from one soil type to another is quite abrupt across the plains and it is virtually impossible to know the soil type at any point on the plain unless excavation is carried out.(See image upper left) |
Site SW60 | 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 | 0-25 | 6.2 | 5.6 | 0.15 | N/R | 6.2 | 0.55 | 0.51 | 0.18 | <10 | 9.3 | 17.6 | 7.4 | 29.3 | 45.6 | 12 | 7.5 |
A2 | 25-40 | 6 | 5.4 | 0.08 | N/R | 1.8 | 0.92 | 0.24 | 0.09 | <10 | 4.3 | 15.5 | 8.9 | 27.1 | 40.9 | 8 | 24 |
B21 | 40-80 | 5.8 | 5.6 | 0.09 | N/R | 1.7 | 5 | 0.45 | 0.25 | <10 | 8 | 32.7 | 24.4 | 15.4 | 17.6 | 6 | 57.5 |
B22 | 80-105 | 5.5 | 5.1 | 0.08 | N/R | 0.82 | 4.7 | 0.17 | 0.33 | <10 | 6.8 | 31.7 | 21.1 | 25.1 | 16.2 | 3.5 | 52 |