Site: ASH98 (Plot1) | Land Unit: Dundas Redgum |
Site Description:
Geology: Cainozoic duricrust | Landform pattern: Undulating plain |
Position in landscape: Lower slope | Internal drainage: Imperfectly drained |
Soil Profile Morphology
A1 | 0-15 cm | Very dark greyish brown (10YR3/2) loam; weak polyhedral structure (20-50 mm) parting to weak granular structure (5-10 mm); weak consistence when dry; few medium ferruginous nodules; common very fine macropores; areal porosity 0.3%; many medium roots; clear and smooth transition to: | |
A1 | 15-28 cm | Dark brown (10YR4/3) loam; unable to assess structure of consistency due to the presence of very many segregations; dry; very many coarse ferruginous nodules; common very fine roots; sharp and smooth transition to: | |
Subsoil | |||
B21 | 28-60 cm | Yellowish brown (10YR5/6) with common medium distinct reddish brown (5YR5/5) mottles, light medium clay; strong polyhedral structure (10-20 mm) parting to strong granular structure (5-10 mm); firm consistence when moderately moist; very few medium ferruginous segregations; few very fine macropores; areal porosity 0.05%; few very fine roots; diffuse and smooth transition to: | |
B22 | 60-100 cm | Yellowish brown (10YR5/6) with many coarse prominent red (2.5YR4/8), red (2.5YR4/6) and yellow (10YR7/8) mottles, light medium clay; moderate polyhedral structure (20-50 mm) parting to weak polyhedral structure (10-20 mm); firm consistence when moderately moist; few very fine macropores; areal porosity 0.03%; no roots observed; diffuse and smooth transition to: | |
B23 | 100-150 cm | Yellowish brown (10YR6/2) with many coarse prominent brownish yellow (10YR6/6) and red (2.5YR4/8) mottles, light medium clay; strong polyhedral structure (20-50 mm) parting to moderate polyhedral structure (10-20 mm); firm consistence when moderately moist; few very fine macropores; areal porosity 0.03%; no roots observed. | |
150-250 cm | Similar to layer above. | ||
250-400 cm | Fine sandy light clays and silty clays (grey, red, orange), no calcium carbonate observed. |
Sampled by: Ian Sargeant, Paul Feikema and Martin Clark (6 December 2000)