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Wind Erosion in Western Queensland Australia

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

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

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Chapter 2 – Land Erodibility Controlsspatial distribution of its controls with<strong>in</strong> a landscape. If a landscape is modified as a result ofhuman activity, or natural disturbance processes such as fire, it may move over somethreshold, result<strong>in</strong>g <strong>in</strong> a non-l<strong>in</strong>ear <strong>in</strong>crease <strong>in</strong> its susceptibility to w<strong>in</strong>d erosion. The way <strong>in</strong>which landscapes are modified by human activities is largely dependent on land use. Landuses commonly associated with w<strong>in</strong>d erosion are cultivation and pastoralism. Themanagement of landscapes under these land uses is quite different, and so the implications ofthese on w<strong>in</strong>d erosion processes also differ.In cultivated lands there are often dist<strong>in</strong>ct boundaries between areas with particular landsurface conditions. The effects of land management on land erodibility <strong>in</strong> cultivatedenvironments are primarily seen through: 1) control of vegetation cover (crops); 2) control offield length (fetch); 3) control of soil aggregation and surface roughness through cultivation;and 4) control of soil moisture conditions through irrigation. While climate variability plays asignificant role <strong>in</strong> driv<strong>in</strong>g the state of these conditions, <strong>in</strong>tensive management will oftenaffect the spatial distribution of erodible land areas (e.g. the location of fallowed fields) andthe tim<strong>in</strong>g of changes <strong>in</strong> controls (Leys, 1999).In rangelands, spatial and temporal changes <strong>in</strong> land erodibility are affected by climaticconditions and graz<strong>in</strong>g pressures. Aga<strong>in</strong>, these affect spatial and temporal patterns <strong>in</strong>vegetation cover, moisture and soil erodibility. Boundaries of management <strong>in</strong> rangelands mayappear to be less structured than <strong>in</strong> cultivated environments. However the effects ofvegetation consumption by graz<strong>in</strong>g animals and trampl<strong>in</strong>g of the soil surface can vary fromcreat<strong>in</strong>g localised patches of highly erodible land to regional scale <strong>in</strong>creases <strong>in</strong> erodibility.Spatial variability <strong>in</strong> graz<strong>in</strong>g pressures may lead to the formation of w<strong>in</strong>d erosion ‘hot spots’that are often significant dust emitters (Gillette, 1999).2.4 Conceptual Model of Land ErodibilityThis section provides a synthesis of the systems analysis presented <strong>in</strong> Section 2.2. Itsummarises the effects of controls on soil and land erodibility and comb<strong>in</strong>es these <strong>in</strong> aconceptual model of the land erodibility cont<strong>in</strong>uum.62

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