Soil water content, runoff and soil loss prediction in a small ungauged agricultural basin in the Mediterranean region using the Soil and Water Assessment Tool

被引:14
作者
Ramos, M. C. [1 ]
Martinez-Casasnovas, J. A. [1 ]
机构
[1] Univ Lleida, Dept Environm & Soil Sci, E-25198 Lleida, Spain
关键词
NONPOINT-SOURCE POLLUTION; SWAT MODEL; SEDIMENT YIELD; EROSION RATES; SPATIAL VARIABILITY; VINEYARDS; TRANSPORT; MOISTURE; PRECIPITATION; SIMULATION;
D O I
10.1017/S0021859614000422
中图分类号
S [农业科学];
学科分类号
09 ;
摘要
The aim of the present work was to evaluate the possibilities of using sub-basin data for calibration of the Soil and Water Assessment Tool (SWAT) model in a small (46 ha) ungauged basin (i.e. where the water flow is not systematically measured) and its response. This small basin was located in the viticultural Anoia-Penedes region (North-east Spain), which suffers severe soil erosion. The data sources were: daily weather data from an observatory located close to the basin; a detailed soil map of Catalonia; a 5-m resolution digital elevation model (DEM); a crop/land use map derived from orthophotos taken in 2010 and an additional detailed soil survey (40 points) within the basin, which included properties such as texture, soil organic carbon, electrical conductivity, bulk density and water retention capacity at -33 and -1500 kPa. A sensitivity analysis was performed to identify and rank the sensitive parameters that affect the hydrological response and sediment yield to changes of model input parameters. A 1-year calibration and 1-year validation were carried out on the basis of soil moisture measured at 0.20-m intervals from depths of 0.10 to 0.90 m in two selected sub-basins, and data related to estimations of runoff and sediment concentrations in runoff collected in the same sub-basins. The present paper shows a methodological approach for calibrating SWAT in small ungauged basins using soil water content measurements and runoff samples collected within the basin. The SWAT satisfactorily predicted the average soil water content, runoff and soil loss for moderate intensity events recorded during the study periods. However, it was not satisfactory for high-intensity events which would require exploring the possibilities of using sub-daily information as an input model parameter.
引用
收藏
页码:481 / 496
页数:16
相关论文
共 73 条
  • [1] Allen R. G., 1998, FAO Irrigation and Drainage Paper
  • [2] Allison L.E., 1965, METHODS SOIL ANAL 2, P1367, DOI DOI 10.2134/AGRONMONOGR9.2.C39
  • [3] [Anonymous], 1985, NAT ENG HDB, p10.1
  • [4] [Anonymous], 2006, WORLD REFERENCE BASE
  • [5] [Anonymous], Z GEOMORPHOLOGIE S
  • [6] Arnold JG, 2010, T ASABE, V53, P1433
  • [7] BED LOAD TRANSPORT BY NATURAL RIVERS
    BAGNOLD, RA
    [J]. WATER RESOURCES RESEARCH, 1977, 13 (02) : 303 - 312
  • [8] Herbaceous crops, vineyards and olive groves. The traditional land management and its impact on water erosion
    Bienes, R.
    Marques, M. J.
    Ruiz-Colmenero, M.
    [J]. CUADERNOS DE INVESTIGACION GEOGRAFICA, 2012, 38 (01): : 49 - 74
  • [9] Analysing and modelling solute and sediment transport in the catchment of the Wahnbach River
    Bogena, H
    Diekkrüger, B
    Klingel, K
    Jantos, K
    Thein, J
    [J]. PHYSICS AND CHEMISTRY OF THE EARTH, 2003, 28 (6-7) : 227 - 237
  • [10] Runoff, erosion, and water quality of agricultural watersheds in central Navarre (Spain)
    Casali, J.
    Gastesi, R.
    Alvarez-Mozos, J.
    De Santisteban, L. M.
    Del Valle de Lersundi, J.
    Gimenez, R.
    Larranaga, A.
    Goni, M.
    Agirre, U.
    Campo, M. A.
    Lopez, J. J.
    Donezar, M.
    [J]. AGRICULTURAL WATER MANAGEMENT, 2008, 95 (10) : 1111 - 1128