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| OTR608 | Melacic, Humic/alsilic, Semiaquic, Podosol | |
| Chapple Vale | |||
| Hills | |||
| Palaeogene Pebble Point Formation/Quaternary aeolian deposits | |||
| Hillslope –mid slope | |||
| 12% | |||
| North westerly | |||
Horizon | Depth (cm) | Description | ||
A1 | 0–25 | Very dark brown (10YR2/2); loamy fine sand; weak subangular blocky structure; gradual smooth boundary to: | ||
A2 | 25–60 | Very dark greyish brown (10YR3/2); fine sand; weak subangular blocky structure; occasional quartz gravel; clear wavy boundary to: | ||
B1 | 60–69 | Black (10YR2/1); loamy fine sand; apedal single grain structure; clear wavy boundary to: | ||
B2 | 69–75 | Dark brown (10YR 3/2); sandy clay loam; apedal single grain sturcture; abrupt wavy boundary to: | ||
2Cm | 75+ | Dark yellowish brown (10YR4/4); cemented sand; apedal massive structure; extremely hard. | ||
Management considerations | ||||
Deep sandy soils generally have poor plant water/nutrient holding capacity. The sandy nature of the soils make them prone to wind and sheet and rill erosion. Soils may be hydrophobic (in conjunction with organic coatings) when dried out, taking time to reabsorb moisture. These soils do however drain rapidly. The soil profile is consistently acidic (often associated with sandy surfaces due to the lack of base minerals) and may or may not have organic matter (humose or peaty surfaces). This restricts the uptake of certain nutrients as well as intolerance for some plant species (due in part to the increasing mobilisation of aluminium and manganese). Deficiencies of calcium, potassium and molybdenum are likely. Coffee rock is a pan of variable strength that is found beneath 75cm in these soils (Podosols) where sesquioxides (iron and aluminium) and organic matter have cemented soil material. Where this is only weakly developed then it is called a fragipan. This is often a restriction for root development by limiting water and gas movement. This may also have an influence on subsurface water movement such as lateral flow. |
Site OTR608 | 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 | 0-10 | 4.6 | N/R | 0.058 | 0.006 | 0.5 | 0.7 | 0.2 | 0.3 | N/R | N/R | N/R | N/R | 70 | 10 | 4 | 6 |
A1 | 10-20 | 4.5 | N/R | 0.041 | 0.004 | 0.3 | 0.5 | 0.07 | 0.13 | N/R | N/R | N/R | N/R | 78 | 10 | 4 | 9 |
A2 | 30-60 | 4.6 | N/R | 0.018 | 0.001 | 0.08 | 0.14 | <D.01 | 0.04 | N/R | N/R | N/R | N/R | 78 | 15 | 4 | 2 |
B1 | 60-69 | 4.3 | N/R | 0.047 | 0.004 | 0.05 | 0.17 | 0.03 | 0.22 | N/R | N/R | N/R | N/R | 70 | 13 | 3 | 9 |
B2 | 69-75 | 4.2 | N/R | 0.048 | 0.004 | 0.01 | 0.02 | 0.01 | 0.04 | N/R | N/R | N/R | N/R | 62 | 9 | 6 | 17 |
11Cm | 90-120 | 4.8 | N/R | 0.015 | 0.001 | 0.01 | 0.05 | 0.02 | 0.10 | N/R | N/R | N/R | N/R | 72 | 20 | 2 | 3 |