Laboratory number: | 0953 | Profile Description | |||
Site number: | 400 | A1 | 0-5 cm | Very dark greyish brown (10YR 3/1) organic sand; apedal; earthy fabric; soft when dry; abundant small roots; pH 4.5; abrupt smooth boundary; hydrophobic | |
Classification: | Northcote (1979) - Dy3.21 Stace et al. (1972) - Yellow Podzolic Soil | A2 | 5-50 cm | Light yellowish brown (10YR 6/4) loamy sand; few faint yellowish brown mottles (>5 mm); apedal; earthy fabric; hard when dry; abundant small roots; pH 5.5; abrupt smooth boundary | |
Location: | Bairnsdale 8422, grid ref. 834203 Railway cutting, 12 km SE of Bruthen | B21 | 50-80 cm | Yellowish brown (10YR 5/6) medium clay; common prominent reddish brown mottles (5 - 15 mm), abundant prominent grey mottles (>15 mm); strong medium angular blocky structure (20 mm); smooth-ped fabric; firm when moist; abundant small roots; pH 5.0; clear smooth boundary | |
Land system, component: | Clifton, 2 | B22 | 80-160 cm | Yellowish brown (10YR 5/8) medium clay; abundant prominent grey and reddish brown mottles (>15 mm); strong coarse angular blocky structure (30 mm); smooth-ped fabric; very firm when moist; 2% quartz gravel up to 40 mm; pH 5.0; abrupt smooth boundary | |
Topography: | 2% slope on plateau, NW aspect | C | 160-180 cm | Yellow (IOYR 7/8) sandy clay; abundant prominent reddish brown mottles (>15 mm); apedal; earthy fabric; hard when dry; pH 4.5 | |
Elevation: | 120 m | ||||
Drainage: | Good | ||||
Parent material: | Tertiary sediments | ||||
Vegetation: | Open forest II: Eucalyptus sieberi, E. globoidea and E. cypellocarpa and with Kunzea ericoides predominant in the shrub layer | ||||
Remarks: |
LABORATORY ANALYSES 953 | |||||||||||||||||||
Horizon | Sample Depth cm | Lab. texture | Particle size distribution | Atterberg limits | 1:5 soil water suspension | Clay mineralogy by x-ray diffraction | |||||||||||||
Gravel % | Coarse sand % f.e. | fine sand % f.e. | Silt % f.e. | Clay % f.e. | liquid limit % | plastic limit % | plasticity index % | linear shrinkage % | pH | EC 25°C uS/cm | Cl- % | Depth cm | Composition % | ||||||
Al | 0 - 5 | LS | 1 | 42 | 38 | 10 | 8 | 4.4 | 48 | 0.004 | 60 - 80 | kaolinite 75; | |||||||
A2 | 30 - 50 | LS | 2 | 42 | 40 | 9 | 7 | 13 | 12 | 1 | 0.8 | 4.9 | 17 | 0.001 | montmorillonite | ||||
B21 | 60 - 80 | C | 2 | 12 | 12 | 2 | 71 | 100 | 29 | 71 | 23 | 4.4 | 34 | 0.002 | (chloritized) 25 | ||||
B22 | 80 - 90 | 2 | 4.4 | 33 | 0.002 | 160 - 180 | kaolite 80; | ||||||||||||
B22 | 90 - 120 | C | 2 | 12 | 10 | 2 | 73 | 4.5 | 46 | 0.003 | illite 20 | ||||||||
C | 160 - 180 | C | 1 | 36 | 12 | 11 | 38 | 5.0 | 51 | 0.003 | |||||||||
Horizon | Sample Depth cm | Org. C % | Total N % | 1.3C N | Free Fe2O3 % | Available | HCl extract | Exchangeable cations | |||||||||||
P ppm | K ppm | P % | K % | Ca | Mg | K | Na | CEC | Ca % of CEC | Mg | K | Na | H | ||||||
Milliequivalents/100g | |||||||||||||||||||
Al | 0 - 5 | 1.79 | 0.094 | 25 | 0.4 | 6 | 60 | 0.005 | 0.038 | 0.6 | 0.4 | 0.2 | 0.1 | 11.3 | 5 | 4 | 2 | 1 | 88 |
A2 | 30 - 50 | 0.3 | 0.002 | 0.01 | 0.1 | 0.2 | 0.04 | 0.1 | 2.1 | 5 | 10 | 2 | 5 | 78 | |||||
B21 | 60 - 80 | 5.4 | 0.003 | 0.08 | 0.1 | 4.2 | 0.1 | 0.6 | 23.5 | <1 | 18 | <1 | 3 | 79 | |||||
B22 | 80 - 90 | 0.3 | 4.1 | 0.2 | 0.5 | 23.9 | 1 | 17 | 1 | 2 | 79 | ||||||||
B22 | 90 - 120 | 5.2 | 0.003 | 0.08 | 0.04 | 4.6 | 0.2 | 0.9 | 25.9 | <1 | 18 | 1 | 3 | 78 | |||||
C | 160 - 180 | 3.5 | 0.003 | 0.10 | 0.1 | 3.7 | 0.1 | 0.9 | 18.6 | 1 | 20 | 1 | 5 | 73 |