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Wind Erosion in Western Queensland Australia

Modelling Land Susceptibility to Wind Erosion in Western ... - Ninti One

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Chapter 2 – Land Erodibility ControlsTable 2.1 Summary of selected erodibility factors used <strong>in</strong> the <strong>W<strong>in</strong>d</strong> <strong>Erosion</strong> Equation (WEQ) model.Erodibility Index Def<strong>in</strong>ition Spatial Scale Time Scale Measurement ReferenceSoil Erodibility (I) • Potential annual w<strong>in</strong>d erosion for a given soil under agiven set of field conditionsPlot andFieldM<strong>in</strong>utes toMonths<strong>W<strong>in</strong>d</strong> TunnelDust Traps• Expressed as the average annual soil loss <strong>in</strong> tons peracre per year for a field that is isolated, unsheltered,bare, smooth, level, loose, non-crusted, and at alocation where the climatic factor (C) for the WEQ is100Knoll Erodibility (Is) • Accounts for the <strong>in</strong>creased w<strong>in</strong>d erosion potential ontopographic features (i.e. short slopes, knolls)• Varies for slopes with gradient > 3% and < 150 m long• An adjustment to I given the <strong>in</strong>crease <strong>in</strong> w<strong>in</strong>d velocityon the w<strong>in</strong>dward slope<strong>W<strong>in</strong>d</strong> TunnelErodibility (i)• Index of relative erodibility under w<strong>in</strong>d tunnel withconstant conditions of friction velocity of 0.61 ms-1for five m<strong>in</strong>utes over soil <strong>in</strong> trays with dimensions 5 ftlong and 8 <strong>in</strong>ches wide• Expressed <strong>in</strong> tons per acre• Due to fetch and tray length restrictions <strong>in</strong> w<strong>in</strong>d tunnel,i does not account for abrasion experienced under fieldconditionsField Erodibility (E) • Determ<strong>in</strong>ed by application of the <strong>W<strong>in</strong>d</strong> <strong>Erosion</strong>Equation to determ<strong>in</strong>e potential soil loss <strong>in</strong> tons peracre per year• Accounts for soil (I) and knoll (Is) erodibility, localw<strong>in</strong>d erosion climatic factor, soil ridge roughness, fieldlength and vegetation cover.FieldM<strong>in</strong>utes toMonthsFieldChepil and Woodruff(1963)Woodruff and Siddoway(1965)Woodruff and Siddoway(1965)Plot M<strong>in</strong>utes <strong>W<strong>in</strong>d</strong> Tunnel Chepil (1953)Field toRegionAnnual Modelled Woodruff and Siddoway(1965)27

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