Research article Special Issues

Soil losses in rainfed Mediterranean vineyards under climate change scenarios. The effects of drainage terraces.

  • Received: 15 February 2016 Accepted: 07 April 2016 Published: 25 January 2016
  • Most vines in the Mediterranean are cultivated on bare soils, due to the scarcity of water. In addition, most traditional soil conservation measures have been eliminated to facilitate the movement of machinery in the fields. In such conditions, high erosion rates are recorded. Given the predicted changes in precipitation and an increasing number of extreme events, an increase in erosion processes is expected. In this study, erosion processes under different climate change scenarios were evaluated as well as the effects of implementing drainage terraces in vineyards. Soil losses were simulated using the WEPP model. The results confirmed the relevance of extreme events on annual soil losses. The WEPP model gave satisfactory results in predicting runoff and soil losses, although the soil losses recorded after some extreme events were under-predicted. The model responded to changes in precipitation and because of that a decrease in precipitation gave rise to a decrease in soil losses. For the scenario in 2050, runoff volumes decreased between 19.1 and 50.1%, while erosion rates decreased between 34 and 56%. However, the expected increase in rainfall intensity may contribute to higher erosion rates than at present. The construction of drainage terraces, perpendicular to the maximum slope, 3 m wide and 30 m between terraces, may lead to an average decrease in soil losses of about 45%.

    Citation: María Concepción Ramos. Soil losses in rainfed Mediterranean vineyards under climate change scenarios. The effects of drainage terraces.[J]. AIMS Agriculture and Food, 2016, 1(2): 124-143. doi: 10.3934/agrfood.2016.2.124

    Related Papers:

  • Most vines in the Mediterranean are cultivated on bare soils, due to the scarcity of water. In addition, most traditional soil conservation measures have been eliminated to facilitate the movement of machinery in the fields. In such conditions, high erosion rates are recorded. Given the predicted changes in precipitation and an increasing number of extreme events, an increase in erosion processes is expected. In this study, erosion processes under different climate change scenarios were evaluated as well as the effects of implementing drainage terraces in vineyards. Soil losses were simulated using the WEPP model. The results confirmed the relevance of extreme events on annual soil losses. The WEPP model gave satisfactory results in predicting runoff and soil losses, although the soil losses recorded after some extreme events were under-predicted. The model responded to changes in precipitation and because of that a decrease in precipitation gave rise to a decrease in soil losses. For the scenario in 2050, runoff volumes decreased between 19.1 and 50.1%, while erosion rates decreased between 34 and 56%. However, the expected increase in rainfall intensity may contribute to higher erosion rates than at present. The construction of drainage terraces, perpendicular to the maximum slope, 3 m wide and 30 m between terraces, may lead to an average decrease in soil losses of about 45%.


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    [1] Tropeano D (1984) Rate of soil erosion processes on vineyards in Central Piedmont (NW Italy). Earth Surf Process Landforms 9: 253–266. doi: 10.1002/esp.3290090305
    [2] Wainwright J (1996) Infiltration, runoff and erosion characteristics of agricultural land in extreme storm events, SE France. Catena 26: 27–47. doi: 10.1016/0341-8162(95)00033-X
    [3] Wicherek S (1991) Viticulture and soil erosion in the North of Parisian Basin. Example: The mid Aisne region. Zeitschrift Für Geomorphol 83: 115–126.
    [4] Kosmas C, Danalatos N, Cammeraat LH, et al. (1997) The effect of land use on runoff and soil erosion rates under Mediterranean conditions. Catena 29: 45–59. doi: 10.1016/S0341-8162(96)00062-8
    [5] Ramos MC, Durán B (2014) Assessment of rainfall erosivity and its spatial and temporal variabilities: Case study of the Penedès area (NE Spain). Catena 123: 135–147. doi: 10.1016/j.catena.2014.07.015
    [6] Ramos MC, Martínez-Casasnovas JA (2006) Impact of land levelling on soil moisture and runoff variability in vineyards under different rainfall distributions in a Mediterranean climate and its influence on crop productivity. J Hydrol 321: 131–146. doi: 10.1016/j.jhydrol.2005.07.055
    [7] Ramos MC, Martínez-Casasnovas JA (2010) Soil water balance in rainfed vineyards of the Penedès region (Northeastern Spain) affected by rainfall characteristics and land levelling: influence on grape yield. Plant Soil 333: 375–389. doi: 10.1007/s11104-010-0353-y
    [8] Ramos MC, Martínez-Casasnovas JA (2009) Impacts of annual precipitation extremes on soil and nutrient losses in vineyards of NE Spain. Hydrol Process 23: 224–235. doi: 10.1002/hyp.7130
    [9] Martı́nez-Casasnovas J, Ramos M, Ribes-Dasi M (2002) Soil erosion caused by extreme rainfall events: mapping and quantification in agricultural plots from very detailed digital elevation models. Geoderma 105: 125–140. doi: 10.1016/S0016-7061(01)00096-9
    [10] Ramos MC, Martínez-Casasnovas JA (2006) Nutrient losses by runoff in vineyards of the Mediterranean Alt Penedès region (NE Spain). Agric Ecosyst Environ 113: 356–363. doi: 10.1016/j.agee.2005.10.009
    [11] Martínez-Casasnovas JA, Ramos MC (2006) The cost of soil erosion in vineyard fields in the Penedès–Anoia Region (NE Spain). Catena 68: 194–199. doi: 10.1016/j.catena.2006.04.007
    [12] de Luis M, Brunetti M, Gonzalez-Hidalgo JC, et al. (2010) Changes in seasonal precipitation in the Iberian Peninsula during 1946–2005. Glob Planet Change 74: 27–33. doi: 10.1016/j.gloplacha.2010.06.006
    [13] Ramos MC, Balasch JC, Martínez-Casasnovas JA (2012) Seasonal temperature and precipitation variability during the last 60 years in a Mediterranean climate area of Northeastern Spain: a multivariate analysis. Theor Appl Climatol 110: 35–53. doi: 10.1007/s00704-012-0608-z
    [14] Goubanova K, Li L (2007) Extremes in temperature and precipitation around the Mediterranean basin in an ensemble of future climate scenario simulations. Glob Planet Change 57: 27–42. doi: 10.1016/j.gloplacha.2006.11.012
    [15] Bartolini G, Grifoni D, Torrigiani T, et al. (2014) Precipitation changes from two long-term hourly datasets in Tuscany, Italy. Int J Climatol 34: 3977–3985.
    [16] Nunes AN, Lourenço L (2015) Precipitation variability in Portugal from 1960 to 2011. J Geogr Sci 25: 784–800. doi: 10.1007/s11442-015-1202-y
    [17] Tošić I, Zorn M, Ortar J, et al. (2016) Annual and seasonal variability of precipitation and temperatures in Slovenia from 1961 to 2011. Atmos Res 168: 220–233. doi: 10.1016/j.atmosres.2015.09.014
    [18] Easterling DR, Karl TR, Gallo KP, et al. (2000) Observed climate variability and change of relevance to the biosphere. J Geophys Res Atmos 105: 20101–20114. doi: 10.1029/2000JD900166
    [19] Klein Tank AMG, Können GP (2003) Trends in Indices of Daily Temperature and Precipitation Extremes in Europe, 1946–99. J Clim 16: 3665–3680.
    [20] Kharin VV, Zwiers FW, Zhang X, et al. (2007) Changes in Temperature and Precipitation Extremes in the IPCC Ensemble of Global Coupled Model Simulations. J Clim 20: 1419–1444. doi: 10.1175/JCLI4066.1
    [21] Favis-Mortlock DT, Boardman J (1995) Nonlinear responses of soil erosion to climate change: a modelling study on the UK South Downs. Catena 25: 365-387. doi: 10.1016/0341-8162(95)00018-N
    [22] Nearing MA, Jetten V, Baffaut C, et al. (2005) Modeling response of soil erosion and flow to changes in precipitation and cover. Catena 61: 131-154 doi: 10.1016/j.catena.2005.03.007
    [23] Mullan DJ, Favis-Mortlock DT, Fealy R (2011) Modelling the impacts of climate change on future rates of soil erosion: Addressing key limitations. In: ASABE - International Symposium on Erosion and Landscape Evolution 2011. pp 486–494.
    [24] Segura C, Sun G, McNulty S, Zhang Y (2014) Potential impacts of climate change on soil erosion vulnerability across the conterminous United States. J Soil Water Conserv 69: 171–181. doi: 10.2489/jswc.69.2.171
    [25] Cilek A, Berberoglu S, Kirkby M, et al. (2015) Erosion Modelling In A Mediterranean Subcatchment Under Climate Change Scenarios Using Pan-European Soil Erosion Risk Assessment (PESERA). ISPRS - Int Arch Photogramm Remote Sens Spat Inf Sci XL-7/W3: 359–365. doi: 10.5194/isprsarchives-XL-7-W3-359-2015
    [26] Haregeweyn N, Poesen J, Verstraeten G, et al. (2013) Assessing the performance of a spatially distributed soil erosion and sediment delivery model (WATEM/SEDEM) in northern Ethiopia. Land Degrad Dev 24: 188–204. doi: 10.1002/ldr.1121
    [27] Kirkby MJ, Jones RJA, Irvine B, et al. (2004) Pan-European soil erosion risk assessment: the PESERA Map, Version 1 October 2003. Explanation of Special Publication Ispra 2004 No.73 (S.P.I.04.73). European Soil Bureau Research Report No.16, EUR 21176, 18pp.
    [28] Morgan RPC, Quinton JN, Smith RE, et al. (1998) The European Soil Erosion Model (EUROSEM): a dynamic approach for predicting sediment transport from fields and small catchments. Earth Surf Process Landforms 23: 527–544.
    [29] Laflen JM, Elliot WJ, Flanagan DC, et al. (1997) WEPP-predicting water erosion using a process-based model. J Soil Water Conserv 52: 96–102.
    [30] Renard KG, Foster GR, Weesies GA, et al. (1997) Predicting soil erosion by water: A guide to conservation planning with the revised universal soil loss equation (RUSLE). Handb. No. 703, Washington, DC US Dep. Agric.
    [31] de Vente J, Poesen J, Verstraeten G (2005) The application of semi-quantitative methods and reservoir sedimentation rates for the prediction of basin sediment yield in Spain. J Hydrol 305: 63–86. doi: 10.1016/j.jhydrol.2004.08.030
    [32] Nerantzaki SD, Giannakis G V, Efstathiou D, et al. (2015) Modeling suspended sediment transport and assessing the impacts of climate change in a karstic Mediterranean watershed. Sci Total Environ 538: 288–297. doi: 10.1016/j.scitotenv.2015.07.092
    [33] Mullan D (2013) Soil erosion under the impacts of future climate change: Assessing the statistical significance of future changes and the potential on-site and off-site problems. Catena 109: 234–246. doi: 10.1016/j.catena.2013.03.007
    [34] Mullan D, Favis-Mortlock D, Fealy R (2012) Addressing key limitations associated with modelling soil erosion under the impacts of future climate change. Agric For Meteorol 156: 18–30. doi: 10.1016/j.agrformet.2011.12.004
    [35] Orwin KH, Stevenson BA, Smaill SJ, et al. (2015) Effects of climate change on the delivery of soil-mediated ecosystem services within the primary sector in temperate ecosystems: a review and New Zealand case study. Glob Chang Biol 21: 2844–2860. doi: 10.1111/gcb.12949
    [36] Simonneaux V, Cheggour A, Deschamps C, et al. (2015) Land use and climate change effects on soil erosion in a semi-arid mountainous watershed (High Atlas, Morocco). J Arid Environ 122: 64–75. doi: 10.1016/j.jaridenv.2015.06.002
    [37] Ramos MC (2001) Rainfall distribution patterns and their change over time in a Mediterranean area. Theor Appl Climatol 69: 163–170. doi: 10.1007/s007040170022
    [38] DAR (2008) Mapa de Sòls (1: 25.000) de l’àmbit geogràfic de la Denominació d’Origen Penedès. Departament d’Agricultura, Alimentació i Acció Rural, Generalitat de Catalunya, Vilafranca del Penedès-Lleida.
    [39] IDESCAT. Anuario estadístico de Cataluña. Agricultura Ganadería y Pesca. 2013. Available from: http: //idescat.cat/pub/aec/es.
    [40] Gee GW, Bauder JW (1986) Particle-size Analysis. P. 383 – 411. In A.L. Page (ed.). Methods of soil analysis, Part1, Physical and mineralogical methods. Second Edition, Agronomy Monograph 9, American Society of Agronomy, Madison, WI.
    [41] Cresswell HP and Hamilton (2002) Particle Size Analysis. In: Soil Physical Measurement and Interpretation For Land Evaluation. (Eds. NJ McKenzie, HP Cresswell and KJ Coughlan) CSIRO Publishing: Collingwood, Victoria, 224-239.
    [42] Allison LE (1965) Organic Carbon. In: Methods of Soil Analysis, Black, C.A. (Ed.). American Society of Agronomy, USA, 1367-1378.
    [43] Pieri L, Bittelli M, Wu JQ, et al. (2007) Using the Water Erosion Prediction Project (WEPP) model to simulate field-observed runoff and erosion in the Apennines mountain range, Italy. J Hydrol 336: 84–97. doi: 10.1016/j.jhydrol.2006.12.014
    [44] Mein RG, Larson CL (1973) Modelling infiltration during a steady rain. Water Resour Res 9: 384-394 doi: 10.1029/WR009i002p00384
    [45] Chu ST (1978) Infiltration during an unsteady rain. Water Resour Res 14: 461–466. doi: 10.1029/WR014i003p00461
    [46] Ritchie JT (1972) Model for predicting evaporation from a row crop with incomplete cover. Water Resour Res 8: 1204–1213. doi: 10.1029/WR008i005p01204
    [47] Allen RG, Pereira LS, Raes D, et al. (1998) FAO Irrigation and Drainage Paper 56. FAO, Rome, Italy.
    [48] Sloan PG, Moore ID (1984) Modeling subsurface storm flow on steeply sloping forested watersheds. Water Resour Res 20: 1915–1822.
    [49] Flanagan D C, Livingston SJ (1995) Water Erosion Prediction Project (WEPP) Version 95.7: User summary. NSERL Report No. 11. West Lafayette, Ind.: USDA-ARS National Soil Erosion Research Laboratory.
    [50] Kliewer WM, Wolpert JA, Benz M (2000) Trellis and vine spacing effects on growth, canopy microclimate, yield and fruit composition of cabernet sauvignon. In: Acta Horticulturae 526: 21–31
    [51] Stevens RM, Nicholas PR (1994) Root length and mass densities of Vitis vinifera L. cultivars “Muscat Gordo Blanco” and “Shiraz”. New Zeal J Crop Hortic Sci 22: 381–385. doi: 10.1080/01140671.1994.9513849
    [52] Alberts EE, Nearing MA, Weltz MA, et al. (1995) Soil component. In USDA Water Erosion Prediction Project: Hillslope Profile and Watershed Model Documentation. NSERL Report No. 2. D. C. Flanagan and M. A. Nearing, eds. West Lafayette, Ind.: USDA-ARS.
    [53] Flanagan DC, Nearing MA, eds (1995) USDA Water Erosion Prediction Project hillslope and watershed model documentation. NSERL Report No. 10. West Lafayette, Ind.: USDA-ARS National Soil Erosion Research Laboratory.
    [54] Moriasi DN, Arnold JG, Van Liew MW, et al. (2007) Model evaluation guidelines for systematic quantification of accuracy in watershed simulations. Trans ASABE 50: 885–900. doi: 10.13031/2013.23153
    [55] Nash JE, Sutcliffe JV (1970) River flow forecasting through conceptual models part I — A discussion of principles. J Hydrol 10: 282–290.
    [56] Gupta HV, Sorooshian S, Yapo PO (1999) Status of automatic calibration for hydrologic models: Comparison with multilevel expert calibration. J Hydrolc Eng 4: 135–143. doi: 10.1061/(ASCE)1084-0699(1999)4:2(135)
    [57] Ramos MC, Porta J (1997) Analysis of design criteria for vineyard terraces in the mediterranean area of North East Spain. Soil Technol 10: 155–166. doi: 10.1016/S0933-3630(96)00006-2
    [58] Verheijen FGA, Jones RJA, Rickson RJ, et al. (2009) Tolerable versus actual soil erosion rates in Europe. Earth Sci Rev 94: 23–38 doi: 10.1016/j.earscirev.2009.02.003
    [59] Troeh FR, Hobbs JA, Donahue RL (1999) Soil and Water Conservation: Productivity and Environmental Protection, 3rd Edition. Prentice Hall. Upper Saddle River, New Jersey. 610 p
    [60] Mannering JV. The use of soil loss tolerances as a strategy for soil conservation. In: Editor, RPC Morgan. Soil Conservation Problems and Prospects; 1980 July 21st-25th; Silsoe, Beford, UK. Wiley.
    [61] Licciardello F, Taguas EV, Barbagallo S, et al. (2013) Application of the Water Erosion Prediction Project (WEPP) in Olive Orchards on Vertic Soil with Different Management Conditions. Trans ASABE 56: 951–961. doi: 10.13031/trans.56.9880
    [62] Routschek A, Schmidt J, Kreienkamp F (2014) Impact of climate change on soil erosion—A high-resolution projection on catchment scale until 2100 in Saxony/Germany. Catena 121: 99–109. doi: 10.1016/j.catena.2014.04.019
    [63] Ramos MC, Martínez-Casasnovas JA (2007) Soil loss and soil water content affected by land levelling in Penedès vineyards, NE Spain. Catena 71: 210–217. doi: 10.1016/j.catena.2007.03.001
    [64] Favis-Mortlock DT, Savabi MR (1996) Shifts in rates and spatial distributions of soil erosion and deposition under climate change. Adv Hillslope Process 1: 529-560
    [65] Nearing MA, Pruski FF, O'Neal MR (2004) Expected climate change impacts on soil erosion rates: A review. J Soil Water Conserv 59: 43–50.
    [66] Pruski FF, Nearing MA (2002) Climate-induced changes in erosion during the 21st century for eight U.S. locations. Water Resour Res 38: 341–3411.
    [67] García-Díaz A, Bienes R, Sastre B (2015) Study of Climatic Variations and its Influence on Erosive Processes in Recent Decades in One Location of Central Spain. Engineering Geology for Society and Territory - Volume 1: Climate Change and Engineering Geology, 105-108. doi: 10.1007/978-3-319-09300-0_20
    [68] Shiono T, Ogawa S, Miyamoto T, et al. (2013) Expected impacts of climate change on rainfall erosivity of farmlands in Japan. Ecol Eng 61: 678–689. doi: 10.1016/j.ecoleng.2013.03.002
    [69] Klik A, Konecny F (2013) Rainfall erosivity in northeastern Austria. Trans ASABE 56: 719–725. doi: 10.13031/2013.42677
    [70] Fiener P, Auerswald K, Winter F, et al. (2013) Statistical analysis and modelling of surface runoff from arable fields in central Europe. Hydrol Earth Syst Sci 17: 4121–4132. doi: 10.5194/hess-17-4121-2013
    [71] Ramos MC, Benito C, Martínez-Casasnovas JA (2015) Simulating soil conservation measures to control soil and nutrient losses in a small, vineyard dominated basin. Agric Ecosyst Environ 213: 194-208. doi: 10.1016/j.agee.2015.08.004
    [72] Yang Q, Meng F-R, Zhao Z, et al. (2009) Assessing the impacts of flow diversion terraces on stream water and sediment yields at a watershed level using SWAT model. Agric Ecosyst Environ 132: 23–31. doi: 10.1016/j.agee.2009.02.012
    [73] Mwangi HM. Evaluation of the impacts of soil and water conservation practices on ecosystem services in Sasumua watershed, Kenya, using SWAT model. 2013. Available from: http://ir.jkuat.ac.ke/handle/123456789/994
    [74] Chow TL, Rees HW, Daigle JL (1999) Effectiveness of terraces/grassed waterway systems for soil and water conservation: A field evaluation. J Soil Water Conserv 54: 577–583.
    [75] Dumbrovský M, Sobotková V, Šarapatka B, et al. (2014) Cost-effectiveness evaluation of model design variants of broad-base terrace in soil erosion control. Ecol Eng 68: 260–269. doi: 10.1016/j.ecoleng.2014.03.082
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