基于MMF模型和地理信息的小流域土壤侵蚀评价

K. Kiriwongwattana
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摘要

本研究采用修正的Morgan Morgan and Finney (MMF)模型来评估土壤侵蚀速率。土地利用和土地覆被图来源于2014年Landsat TM数据。土壤组图使用的是国土发展部的土壤组图。坡度图来源于ASTER GDEM数据。利用了位于流域内的泰国气象部门的降雨数据。在MMF模型中,导出了年降雨量、田间容量下土壤含水量、容重、有效水文土壤深度、土壤可脱性指数、坡度、截留能力、冠层盖度、地表盖度、植物高度、作物覆盖管理因子、实际蒸散与潜在蒸散之比等参数,用于土壤侵蚀计算。本研究以泰国西部Ratchaburi省Suanphueng区的淮坂波子流域为研究区。结果表明,平均动能为28.10 J/m2。雨滴的平均可拆卸性为0.0076 kg/m2。径流的平均可拆解性为0.63 kg/m2。年平均土壤可分离性为0.64 kg/m2。径流平均输送能力为2.31 kg/m2。淮班渤子流域年平均土壤流失量为0.64 kg/m2。
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Soil erosion assessment using MMF model and geoinfomations in small watershed
In the present study, Modified Morgan Morgan and Finney (MMF) model is used to assess soil erosion rate. Land use and land cover map was derived from Landsat TM data of 2014. The soil group map from Land Development Department was used. The slope map was from ASTER GDEM data. Rainfall data of Thai Meteorological Department which lies within watershed has been utilized. In MMF model, parameters such as annual rainfall, soil moisture content at field capacity, bulk density, effective hydrological soil depth, soil detachability index, slope, interception capacity, canopy cover, ground cover, plant height, crop cover management factor and ratio of actual and potential evapotranspiration was derived for soil erosion computation. In the present study, Huai Ban Bo sub-watershed which is located in Suanphueng district, Ratchaburi province, Western of Thailand has been taken as study area. The results show that, average kinetic energy is 28.10 J/m2. The average detachability by raindrop is 0.0076 kg/m2. The average detachability by runoff is 0.63 kg/m2. The average annual soil detachability is 0.64 kg/m2. The average transport capacity by runoff is 2.31 kg/m2. Average annual soil loss of 0.64 kg/m2 in Huai Ban Bo sub watershed has been estimated.
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