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| DOAGW15 | ||
Location | Great Western, western Victoria | |||
Landform | Gently undulating plain | |||
Geology | Devonian Granodiorite : adamellite and diorite | |||
Element | Valley flat | |||
Horizon | Depth (cm) | Description | ||
A1 | 0–10 | Brown (10YR4/3) sandy clay loam; massive (structureless) strong consistence (dry), slightly friable (moist); few amounts of fine and medium quartz; pH 6.3; sharp boundary to: | ||
A2 | 10–50 | Very pale brown (10YR7/3) conspicuously bleached (10YR8/2d) sandy loam; massive (structureless); strong consistence (dry), friable (moist), non-plastic and non-sticky (wet); light to moderate amounts of fine and medium quartz; water seepage at about 45-50cm; pH 6.8; sharp boundary to: | ||
B1 | 50-90 | Brownish yellow (10YR6/8) with very pale brown (10YR7/4) and yellowish red (5YR5/6)mottles; sandy clay; moderate medium parting to fine angular blocky structure; smooth ped-fabric; very firm consistence (dry), friable (moist); few to common fine quartz; pH 6.3; clear boundary to: | ||
B2 | 90-120 | Light brownish grey (2.5Y6/2) with red (2.5YR4/6) and strong brown (7.5YR5/6) mottles; heavy clay with some sand; moderate medium parting to fine angular blocky structure; smooth ped-fabric; very firm consistence (dry), moderately friable (moist); few to common fine and medium quartz; some gleying; pH 6.0. | ||
Management considerations | ||||
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Site DOAGW15 | Sample depth cm | pH | EC dS/m | NaCl % | Organic Carbon % | Ex Ca cmol-/kg | Ex Mg cmol-/kg | Ex K cmol-/kg | Ex Na cmol-/kg | Ex acidity cmol-/kg | FC -30okPa | PWP -1500okPa | KS % | FS % | Z % | Ca % | |
Horizon | H2O | CaCl2 | |||||||||||||||
A1 | 0–10 | 6.3 | NA | 0.04 | NA | 2.6 | 1.9 | 1.1 | 0.4 | 0.1 | 9.0 | 20.7 | 8.1 | NA | NA | NA | NA |
A2 | 10–50 | 6.8 | NA | 0.01 | NA | NA | 0.7 | 0.6 | 0.1 | 0.1 | 1.4 | 9.4 | 2.7 | NA | NA | NA | NA |
B1 | 50-90 | 6.3 | NA | 0.03 | NA | NA | 0.4 | 2.0 | 0.2 | 0.2 | 3.2 | 13.7 | 7.9 | NA | NA | NA | NA |
B2 | 90-120 | 6.0 | NA | 0.07 | NA | NA | 0.4 | 3.9 | 0.2 | 0.8 | 10.1 | 26.8 | 18.0 | NA | NA | NA | NA |