Exploring some relationships between biological soil crusts, soil aggregation and wind erosion |
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| Authors: | David J Eldridge John F Leys |
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| Institution: | a Department of Land and Water Conservation, Centre for Natural Resources, c/o School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, 2052, NSW, Australia;b Department of Land and Water Conservation, Centre for Natural Resources, 462, Gunnedah, NSW, 2380, Australia |
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| Abstract: | A portable wind tunnel was used to test the contribution of biological and physical elements to overall soil aggregation on a soil dominated by biological soil crusts in south-eastern Australia. After moderate disturbance and simulated wind erosion, 90% of surface aggregates on the loamy soil and 76% on the sandy soil were dominated by biological elements (cryptogams). Lower levels of biological bonding were observed on the severely disturbed treatment. Linear regression indicated a significant positive relationship (r2=0·72) between biological soil crust cover and dry aggregation levels greater than 0·85mm. To maintain sediment transport below an erosion control target of 5gm−1s−1 for a 65kmh−1 wind at 10m height, a crust cover of approximately 20% is required. When a multiple regression model which sequentially fitted biological crust cover and dry aggregation greater than 0·85mm was applied to the data, dry aggregation accounted for more of the variation in sediment transport rate than biological crust cover. These data were used to develop a conceptual model which integrates crust cover and dry aggregation, and provides a useful framework within which to predict the likely impacts of changes in soil crust cover and aggregation. |
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| Keywords: | wind erosion biological soil crust wind erodibility soil aggregation cyanobacteria wind sediment flux cryptogamic crust |
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