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| SW89 | Endocalcareous, Self-Mulching, Black VERTOSOL | |
| Mount Pollock Road, 1 km south of Mount Pollock | |||
| Low hill associated with Mt Pollock | |||
| Quaternary Volcanics: basalt | |||
| Crest | |||
| 3% | |||
| North-east | |||
Horizon | Depth (cm) | Description | ||
A1 | 0-10 | Dark brown (7.5YR3/2 moist); light clay; very finely pedal, self-mulching, cracking to surface; pH 6.8; clear boundary to: | ||
B21t | 10-20 | Very dark brown (10YR2/2 moist); light medium clay; fine, smooth faced, angular blocky, parting to medium to fine (50-20 mm) polyhedral structure; firm consistence (moist); pH 7; clear boundary to: | ||
B22t(ss) | 20-50/70 | Very dark brown (10YR2/2 moist), with brown (7.5YR5/4 moist) mottles (<10%); medium to heavy clay; angular blocky, parting to coarse lenticular (20-50 mm) structure; obvious (<60 mm), frequent slickensides; strong consistence; pH 7.8; abrupt and wavy boundary to: | ||
B23k/R | 50/70 + | Brown (7.5YR4/3 moist), >50% soft carbonate in clay matrix, fragments of hard basalt; pH 8.6. | ||
Management considerations | ||||
Highly chemically fertile but of limited spatial extent at this site being confined to the crest of the hill and interspersed with a rockier variant.. The high clay content and swelling nature of the clay results in this soil being very sticky when wet and prone to damage by traffic. |
Site SW89 | 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 | 0-5 | 6.8 | 6.2 | 0.18 | N/R | 21.0 | 13.0 | 1.5 | 0.73 | N/R | N/R | 47.2 | 28.8 | 6.6 | 15.0 | 18.5 | 48.5 |
B21 | 10-20 | 7.0 | 6.2 | 0.15 | N/R | 22.0 | 17.0 | 1.3 | 1.3 | N/R | N/R | 60.9 | 35.8 | 3.9 | 10.7 | 12.0 | 63.5 |
B22 | 20-60 | 7.8 | 7.8 | 0.14 | N/R | 23.0 | 17.0 | 0.77 | 1.9 | N/R | N/R | 61.7 | 34.9 | 4.3 | 12.9 | 17.5 | 56.0 |
B23K | 60+ | 8.6 | 7.9 | 0.34 | 0.01 | 26.0 | 21.0 | 0.5 | 3.1 | N/R | N/R | 69.2 | 41.6 | N/R | N/R | N/R | N/R |