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- W2272479310 abstract "The crusting of topsoil, through a variety of physical and physico-chemical mechanisms, results in significant changes to surface structural and hydraulic properties. Although it is widely accepted that ‘structural’ and ‘depositional’ crusts are the two main types of soil crust, comparatively few studies have addressed the evolution of these features through a period of ageing, or weathering. Here, both structural and depositional crusts were produced on a silty soil and a clayey soil using simulated rainfall. Then, following a period of drying, the crusts were subjected to a second simulated rainfall event and a second drying period. Samples of both types of crust from both soil types were subjected to mercury intrusion analysis after both the first and second drying periods. A particle size analysis was also conducted on each of these crusts after both rainfall events. The crusts of two soil types were found to be affected to different extents by the imposed weathering procedure. The silty soil, regarded as the more susceptible to crusting and erosion, quickly yielded structural and thick depositional crusts that did not change markedly with a subsequent wetting and drying cycle. In contrast, the more structurally-stable clayey soil yielded thinner crusts, which were found to undergo more pronounced re-organisation after a second wetting and drying cycle. Both the aggregation of solids and the pore networks of these crusts were altered. These results indicate that crust ageing, through the action of periodic wetting and drying, may be a more important process in relatively structurally stable soils than in readily slaking or dispersing soils." @default.
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- W2272479310 date "2004-01-01" @default.
- W2272479310 modified "2023-09-24" @default.
- W2272479310 title "The Effect Of Soil Crust Ageing, Through Wetting And Drying, On Some Surface Structural Properties" @default.
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