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The soils at Wilton and E<strong>as</strong>t Knoyle were not <strong>as</strong> erosion vulnerable <strong>as</strong> at Pewsey<br />

probably due to the more stable soil structure resulting from their higher clay, organic<br />

matter and/or calcium carbonate contents. The key factors influencing run-off rates<br />

on the chalkland site were timeliness of cultivation and the presence of tramlines<br />

running up-and-down slope, which concentrated the flow. The comparatively low<br />

run-off volumes and export of SS and P at E<strong>as</strong>t Knoyle reflect the beneficial effects<br />

of subsoiling, and drilling across-slope, even though the site w<strong>as</strong> relatively flat. The<br />

consistent beneficial effects of non-inversion cultivation methods in reducing run-off,<br />

and/or SS and P mobilisation under heavy rain at Pewsey and Wilton support earlier<br />

work (Carter, 1998). These benefits reflect both better crop cover and improved<br />

resilience to trafficking after drilling. The lack of any effect of reduced cultivation on<br />

the heavier clay soil at E<strong>as</strong>t Knoyle can be related to the lack of crop residue cover<br />

afforded by maize stubble.<br />

In our study, run-off volumes were incre<strong>as</strong>ed by up to 65% and SS and TP loads<br />

were incre<strong>as</strong>ed up to five- and fourfold, respectively, where tramlines were present.<br />

Earlier initiation of run-off, the lack of any crop cover to protect the soil and the<br />

channelling effect created by the depth and pattern of indentation left by the lugs<br />

of the tractor tyre were key contributory factors. Variation in the impact of tramlines<br />

will depend on the extent to which these key factors are represented. These data<br />

strongly suggest that the timing of tramline establishment in relation to antecedent<br />

soil moisture conditions can have an important influence on the risk of incre<strong>as</strong>ed runoff<br />

and erosion from these soils.<br />

ACKNOWLEDGEMENTS<br />

This work w<strong>as</strong> jointly funded by the European Commission (DESPRAL project EVK1-<br />

CT-1999-00007), Defra and the Environment Agency (EA). The authors also thank<br />

Mr. A. Drake, Mr. T. Goodman and Mr R. Butler for hosting the demonstration plots<br />

on their land, and to Mr. C. Westcott (EA) for organising catchment stakeholder<br />

discussion.<br />

REFERENCES<br />

Carter MR (1998). Conservation tillage practices and diffuse pollution. In: T Petchey,<br />

B D’Arcy and A Frost (eds.) Non-Point Pollution II, pp. 51-60. The Scottish Agricultural<br />

College, Aberdeen, UK.<br />

Chambers BJ, Garwood TWD and Unwin RJ (2000). Controlling soil water erosion and<br />

phosphorus losses from arable land in England and Wales. Journal of Environmental<br />

Quality 29, 145–150.<br />

Edwards AC and Withers PJA (1998). Soil phosphorus management and water<br />

quality: a UK perspective. Soil Use and Management 14, 124–130.<br />

Huggins R (1999). The Landcare project. In: T Petchey, B D’Arcy and A Frost (eds.)<br />

Non-Point Pollution II, pp. 145-152. The Scottish Agricultural College, Aberdeen,<br />

UK.<br />

277

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