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Crooke (Ck)

Geology Quaternary (Late Pleistocene) alluvium. Landform Alluvial terrace - an earlier flood plain of the La Trobe River.

Original Vegetation

It is likely that this map unit carried little vegetation and was predominantly grassland. However, there is occasional red gum (Eucalyptus tereticornis).

Previous Maps and Reports

This map unit is included within the Valencia Land System as described by Aldrick et al. (1992). Drake and Poutsma (1956) mapped the soil as Crookes clay.

Soils

Crookes clay is the main soil type on the higher flood plain. The soil is often crabholey or “buckety” (gilgai) and its external drainage is poor in many places. It cracks when dry and areas are likely to be saline. The soil is a very dark grey or black medium to heavy clay becoming slightly paler in colour with depth. Occasionally the surface soil is a shallow clay loam. The soils which are clayey throughout are generally classified as Grey or Black Vertosols.

Chemical and Physical Analysis

An analysis of the soil to 1 metre is given for an auger site below.

La Trobe Valley - Soil Auger Site G3 (Sargeant & Imhof, 2000).

Depth cm	Texture	pH	EC dS/m	Cl %	Nitrogen %	Carbon %	Ca meq%	Mg meq%	K meq%	Na meq%	H meq%	ESP %	Gravel %	Coarse sand %	Fine sand %	Silt %	Clay %	LAT %
0-20	LC	6.3	0.66	0.11	0.21	2.8	4.2	8.8	0.2	2.2	7.2	10		10	24	21	41	2
20-50	MHC	5.9	1.7	0.38			2.9	7.9	0.2	2.9	7.3	14		6	21	21	49	2
50-85	MHC	6.9	2.4	0.42			3.2	9.9	0.2	4.0	4.8	18		5	16	20	57	1
85-100	MHC	7.2	2.2	0.10			3.3	12	0.4	7.9		33

The following abbreviations are used to describe field texture: S - sand; LS - loamy sand; ClS - clayey sand; SL - sandy loam; L - loam; CL - clay loam; SCL - sandy clay loam; SC - sandy clay; FSCL - fine sandy clay loam; FSC - fine sandy clay; LC - light clay; MC - medium clay; HC - heavy clay; GR - gravel; ZL - silty loam; ZCL - silty clay loam; ZLC - silty light clay; ZMC - silty medium clay.

Other symbols include: pH - analysed in water; EC - electrical conductivity; Cl - chloride; Ca - exchangeable calcium; Mg - exchangeable magnesium, K - exchangeable potassium; Na - exchangeable sodium; H - exchangeable hydrogen; ESP - exchangeable sodium percentage.

For Soil Auger Sites (Sargeant and Imhof, 2000) exchangeable cations have been determined using Gilman method (where pH >7) and Tucker method (pH <7). Exchangeable Sodium % (ESP) has been calculated here as the percentage of sodium in relation to the sum of the exchangeable basic cations.

Land Use

Grazing of sheep and cattle is generally carried out on this map unit. These soils are too clayey to have any horticultural potential.

Vertosols occur in the foreground on the Crooke mapping unit near Rosedale. Note the terrace (Loy Yang mapping unit) in the middle ground and the hills in the background (Stockdale/Gormandale mapping units). These were formed by uplift along the Rosedale fault.