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LP64

Location: Lexton

Australian Soil Classification: Vertic, Mottled-Mesonatric, Grey SODOSOL (very deep surface horizons)

General Landscape Description: Lower midslope position of a rolling low hill landscape unit.
Geology: Devonian granite.

LP64 Landscape

Surface Soil			LP64 Profile
A11	0-30 cm	Dark brown (7.5YR3/2); light sandy clay loam; moderate very fine granular structure, becoming weak medium blocky structure with depth; pH 5.7; clear change to:
A21	30-50 cm	Brown (10YR5/3); light very fine sandy loam; massive; firm consistence moist; pH 4.8; abrupt change to:
A22	50-75 cm	Brown (10YR5/3) with yellow brown (10YR5/8) mottles; conspicuously bleached; light sandy clay loam; firm consistence dry; contains very few (2%) ferro-manganiferous nodules (8 mm size) and few (3%) quartz fragments; pH 6.1; abrupt change to:
A23	75-85 cm	Greyish brown (10YR5/2); conspicuously bleached (10YR7/2d); light coarse sandy clay loam; very firm consistence dry; pH 6.6; sharp change to:
Subsoil
B21	85-110 cm	Dark grey brown (10YR4/2) with red (2.5YR4/6) and yellow brown (10YR5/8) mottles; medium-heavy clay; very coarse prismatic structure; strong consistence moist; pH 6.9; gradual change to:
B22	110 + cm	Greyish brown (10YR5/2) with red (2.5YR4/6) and yellow brown (10YR5/8) mottles; medium-heavy clay; strong consistence moist; quartz and gravel present in patches; slickensides present; pH 6.9.

• Very thick subsurface (A2) horizons (to 85 cm depth).
• Strong texture contrast between surface (A) horizons (<20% clay) and subsurface (B21) horizon (46% clay).
• Conspicuously bleached subsurface (A2) horizons.

• Plant available water capacity (PAWC) is estimated to be relatively low (estimated at 65 mm). This is based on available laboratory data and assumes an effective rooting depth of 100 cm. Effective rooting depth will be restricted by the strongly sodic and dispersive subsoil. The low PAWC will limit pasture growth into dry a spring and summer.

• The surface (A) horizons have a much higher level of coarse sand than for the other sites examined. This will contribute to increased infiltration of water and reduced plant available water holding capacity.
• Organic carbon and total nitrogen levels are reasonable for the A1 horizons. Organic matter is important for maintaining surface soil aggregation. The relatively deep A1 horizon is important for plant growth as the deeper A2 horizons have a very low inherent fertility (based on the sum of the exchangeable cations).

• The dense and coarsely structured subsoil is strongly sodic and disperses completely (and has a low calcium:magnesium ratio of 0.3). This is likely to significantly restrict water and root movement through the subsoil. The conspicuously bleached A2 horizon above the sodic subsoil indicates that periodic waterlogging occurs. On sloping country there is likely to be significant lateral flow of water downslope, above the more impermeable clay subsoil.

• Was native pasture until ripped up 12 years ago. Fescue, phalaris and cocksfoot now grown. (Cocksfoot performs better than phalaris).
• More likely to get bogged here than on site LP65

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