MP28

Site MP28 Landscape.

Soil Profile Morphology:

Surface Soil

A1	0-15 cm	Brown (7.5YR4/4); loamy sand; weak consistence dry; pH 7.7; sharp change to:	Site MP28 Profile
A2	15-45 cm	Reddish yellow (7.5YR6/6), conspicuously bleached (7.5YR7/4d); loamy sand; massive; weak consistence dry; sharp change to:
Subsoil
B1	45-65 cm	Strong brown (7.5YR5/8); heavy sandy loam; weak blocky structure; weak consistence moist; pH 8.6:
B21	65-70 cm	Yellowish red (5YR5/8); light sandy clay loam; sharp change to:
B22	70-100 cm	Reddish yellow (7.5YR6/6); sandy clay loam; weak, coarsely structured; firm consistence, moist; pH 9.7:
B23k	100-150 cm	Yellowish red (5YR5/8); sandy clay; weak very coarse blocky structure; contains few fine earth carbonates and some hard carbonates (increasing with depth).

• The surface horizons have a low water holding capacity and are likely to become ‘droughty’ during periods of low rainfall. The low wilting point value (i.e. 3.5), however, indicates that plants will be able to utilise light rains falling on relatively dry soil. Heavier (i.e. more clayey) soils need to have considerable moisture stored before plants can have access to it.
• The surface soil has a low inherent nutrient status due to the high sand content and low clay content. Leaching of applied fertilisers is likely to be relatively high.
• Infiltration rates are likely to be relatively high for the sandy surface horizons.
• Organic matter and nitrogen levels are low for this pit site (which may or may not be representative of the whole paddock). Improving organic matter levels will increase soil fertility, water holding capacity and soil aggregation.

• Soluble salt levels are low throughout the subsoil.
• The deeper subsoil (from 80 cm depth) is extremely alkaline which indicates that phosphorus and some trace elements (e.g. iron, manganese, boron, copper and zinc) may be poorly available to plants. Deficiencies can be determined by plant tissue analysis.
• The subsoil is sodic and disperses. This is likely to restrict root and water movement at depth. In some ways this more restrictive layer can be of some benefit . It will ensure that water does not rapidly move beyond the root zone.