Wild®res raise concerns over the risk of accelerated erosion as a result of increased overland ¯ow and decreased protection of the soil by litter and ground vegetation cover. We investigated these issues following the 1994 ®res that burnt large areas of native Eucalyptus forest surrounding Sydney, A
Effects of field reorganisation on the spatial variability of runoff and erosion rates in vineyards of Northeastern Spain
✍ Scribed by M. C. Ramos; J. A. Martínez-Casasnovas
- Publisher
- John Wiley and Sons
- Year
- 2010
- Tongue
- English
- Weight
- 348 KB
- Volume
- 21
- Category
- Article
- ISSN
- 1085-3278
- DOI
- 10.1002/ldr.958
No coin nor oath required. For personal study only.
✦ Synopsis
This study analyses the spatial variability of runoff and erosion rates in vineyards due to mechanisation works. Runoff samples were collected at three positions in two plots after 33 erosive events in three years (2001, 2003, 2004) with different rainfall patterns. Three replications were considered at each position. Soil properties were evaluated in order to analyse its relationship with runoff and erosion rates. Runoff and erosion rates were, on average, higher in the levelled plot (HD), ranging between 8Á4 and 34Á3 per cent, than in the non-levelled plot (LD) ranging between 8Á2 and 24Á1 per cent. Mean sediment concentration in runoff ranged between 6 and 8 g L À1 in the HD plot and about 4Á6 g L À1 in the LD plot, but with high differences within the plot. In the HD plot, runoff-rainfall rates were significantly higher (at 95 per cent level) in the upper part of the slope and decreased along the slope, while in the LD plot, differences in runoff rates were not significant and similar to those observed in the less disturbed areas of the HD plot. The higher susceptibility to soil sealing in areas where the original topsoil was removed conditioned runoff rates. In the lower part of the HD plot runoff rates were, on average, 20 per cent lower than in the upper part of the slope. In those positions runoff rates up to 79 per cent were recorded. Organic matter content and water retention capacity at different potentials are the soil characteristics related to the differences on runoff and erosion rates in the resulting soils.
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