DYS99 (Plot 1)

Site: DYS99 (Plot 1)

Land Unit: Strathdownie

General Land Unit Description:

This land unit comprises the Quaternary lacustrine geology south of the Glenelg River. The lacustrine deposits include lagoonal, swamp and local colluvial deposits formed in low-lying wetlands and depressions between stranded beach ridges. Parent material in this land unit comprises of sand, silt, sandy clay, peat, marl and freshwater limestone, occurring in relatively unconsolidated forms.

The soils are variable throughout this land unit due to varying depositional environments. A common soil type is a strong texture contrast soil (Chromosol) commonly with a bleached A2 horizon and a mottled subsoil (indicative of impeded internal drainage). The sandy topsoil can be very deep in some soils. Vertosols are also common on the plains and swales in between the dunes. Podosols occur on the flats as well as on the dunes and that may have been mapped as part of this land unit due to restrictions of scale. Many of the soils are poorly drained and exhibit signs of a perched watertable.

This site has a 1.5 year old

Eucalyptus globulus

plantation on ex-agricultural land. The site is probably a heathland/bog. The trees in this plot have been severely affected by waterlogging.

Site Description:

Geology: Quaternary lacustrine	Landform pattern: Plain
Position in landscape: Flat	Internal drainage: Poorly drained

Soil Profile Morphology

A1	0-15 cm	Black (10YR2/1) medium clay; strong granular structure (5-10 mm); firm consistence when dry; few very fine macropores; areal porosity 0.02%; common very fine roots; clear and smooth transition to:
Subsoil
B21	15-65 cm	Black (10YR2/1), heavy clay; moderate polyhedral structure (50-100 mm) parting to moderate polyhedral structure (10-20 mm); weak consistence when moderately moist; few very fine macropores; areal porosity 0.02%; common very fine roots; gradual and smooth transition to:
B22	65-105 cm	Black (7.5YR2/0) heavy clay; strong prismatic structure (50-100 mm) parting to moderate prismatic structure (20-50 mm); weak consistence when moist; few very fine macropores; areal porosity 0.02%; common very fine roots; gradual and smooth transition to:
B23	105-150 cm	Yellowish brown (10YR5/8) with many very coarse prominent dark grey (7.5YR4/0) mottles, medium clay; moderate polyhedral structure (50-100 mm) parting to moderate granular structure (5-10 mm); weak consistence when wet; few very fine macropores; areal porosity 0.05%; few very fine roots.
	150-230 cm	Similar to layer above.
	230-390 cm	Light grey and yellow and red brown mottled clay, light clay in mottles with a heavy clay matrix, there appears to be a perched watertable at about 230 cm, no roots observed.

Notes: Sampled by: Ian Sargeant and Paul Feikema (13 December 2000)

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