Factors affecting runoff and erosion under simulated rainfall in Mediterranean vineyards

  1. Arnaez, J. 1
  2. Lasanta, T. 2
  3. Ruiz-Flaño, P. 3
  4. Ortigosa, L. 1
  1. 1 Universidad de La Rioja
    info

    Universidad de La Rioja

    Logroño, España

    ROR https://ror.org/0553yr311

  2. 2 Instituto Pirenaico de Ecología
    info

    Instituto Pirenaico de Ecología

    Zaragoza, España

    ROR https://ror.org/039ssy097

  3. 3 Universidad de Valladolid
    info

    Universidad de Valladolid

    Valladolid, España

    ROR https://ror.org/01fvbaw18

Revista:
Soil and Tillage Research

ISSN: 0167-1987

Ano de publicación: 2007

Volume: 93

Número: 2

Páxinas: 324-334

Tipo: Artigo

DOI: 10.1016/J.STILL.2006.05.013 SCOPUS: 2-s2.0-33846689795 WoS: WOS:000244850400010 GOOGLE SCHOLAR

Outras publicacións en: Soil and Tillage Research

Obxectivos de Desenvolvemento Sustentable

Resumo

Data on surface runoff and soil loss on gentle slopes with vineyards are analysed. Using a rainfall simulator, 22 rainstorms with varied intensities from 30 to 117.5 mm h-1 and return periods from 2 to 127 years were reproduced. The experimental plots were installed on vineyards planted in straight rows and oriented with the slope direction having a mean gradient of 3.8°. The texture of soils was loamy, with a very heterogeneous surface gravel cover. Values of measured surface runoff varied from 7.2 mm h-1 for low rainfall intensities (30 mm h-1) and short return periods (2 years) to 41.9 mm h-1 with simulation experiments of higher rainfall intensity (104 mm h-1) and long return periods (68 years). Runoff increased linearly with rainfall intensity resulting in soil losses that also increased with rainfall intensity (18.2 g m-2 h-1 with storms of 30 mm h-1, and 93.2 g m-2 h-1 with storms of 104 mm h-1); however, r2 explains only 36% of the variance. It was necessary to add other factors to improve the coefficient of determination (0.74; p = 0.001) and the predictive function of the equation. These variables were rainfall intensity, kinetic energy of the storm, runoff, soil resistance to drop detachment, surface gravel cover, and gradient. The equation obtained was validated with the USLE-M. In comparison with similar experiments in other regions, the results obtained for soil loss were very moderate, especially those caused by rainstorms of intermediate and low intensity. © 2006 Elsevier B.V. All rights reserved.